HS8.3.7 | Soil hydrology and irrigation for sustainable food production in a global climate change context
EDI
Soil hydrology and irrigation for sustainable food production in a global climate change context
Co-organized by SSS6, co-sponsored by ICARDA
Convener: Marco PeliECSECS | Co-conveners: Mira HaddadECSECS, Fatma WassarECSECS, Giulio CastelliECSECS
Orals
| Fri, 19 Apr, 10:45–12:30 (CEST)
 
Room 2.31
Posters on site
| Attendance Fri, 19 Apr, 16:15–18:00 (CEST) | Display Fri, 19 Apr, 14:00–18:00
 
Hall A
Posters virtual
| Attendance Fri, 19 Apr, 14:00–15:45 (CEST) | Display Fri, 19 Apr, 08:30–18:00
 
vHall A
Orals |
Fri, 10:45
Fri, 16:15
Fri, 14:00
The proper management of blue and green water is vital for sustainable livelihoods and agricultural practices around the world. This is especially true in drylands, where any productive activity is deeply related to the understanding of soil hydrological behaviour, and irrigation is both a pillar of agroecosystems and a defence against desertification, but also in temperate or humid lands which can experience variations in the hydrological cycle and be prone to water scarcity due to climate change.
Improper practices, which are not able to cope with climate-induced variability and anomalies, may in fact contribute to soil degradation and depletion of the available water sources. For example, incorrect irrigation techniques may lead to soil and groundwater salinization, with dramatic fallout on agricultural productivity, while overgrazing may lead to exploitation of vegetation cover, soil compaction, and adverse effects on the soil capability of water buffering. On the other hand, the role of irrigation goes beyond the technological aspects: traditional irrigation is a cultural heritage, which is often structurally resilient, and which needs to be faced with an interdisciplinary approach involving humanities.

This session welcomes contributions with a specific focus on:
• The understanding of the soil hydrological behaviour and of the mass fluxes through the soil in drylands and environments under actual or projected stress conditions (e.g. water shortage, compaction, salinization)
• The interaction between irrigation and soil hydrology including deep drainage
• The analysis of the bio-geo-physical and social dynamics related to rainfed and irrigated agriculture in both arid and non-arid areas and oases, including the use of non-conventional waters (e.g. water harvesting), and managed aquifer recharge systems
• The management of rangeland areas, including their restoration

This session is co—sponsored by the International Commission on Irrigation and Drainage (ICID, to be confirmed) and the International Center for Agriculture Research in the Dry Areas (ICARDA, to be confirmed).

Orals: Fri, 19 Apr | Room 2.31

Chairpersons: Marco Peli, Mira Haddad, Giulio Castelli
10:45–10:50
10:50–11:00
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EGU24-692
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ECS
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On-site presentation
Ines Toumi, Mohamed Ghrab, Olfa Zarrouk, and Kamel Nagaz

Irrigation management is the key to improving water productivity in fruit orchards growing under marginal conditions in dry areas where the water for irrigation is significantly decreasing. The aim of this work was to determine the yield response to variable water supply of an early maturing peach orchard and to assess the water productivity in an environment where the water is extremely scarce. Field experiments were carried out on peach trees for a private farm in south of Tunisia for two relevant period (2010/2011 and 2013/2015), in an area with sandy soil, hot summer and mild winter conditions.  Old trees were irrigated with different irrigation strategies 100%, 60%, 50%, 40% and 20% of the estimated ETc. In the first experimental period, Flordasar peach trees were subjected to DI40, DI60 and DI20 and gave a variable yields ranged between 23-30 Kg tree-1. The highest WP values were obtained for DI60 et DI40, respectively 4.26 and 3.63 kg m-3. However, experimental work in peach trees under DI50 with two irrigation strategies, average water productivity varied between 2.21-2.24 and 2.81-3.14 kg m-3 respectively when yields was increased from 25.5 to 34.1 Kg tree-1. The yield reductions under low to severe water defcits accompanied by gains in WP may be justifable in the light of anticipated water restriction.

How to cite: Toumi, I., Ghrab, M., Zarrouk, O., and Nagaz, K.: Field quantification of the water productivity of a peach orchard within an arid climate zone., EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-692, https://doi.org/10.5194/egusphere-egu24-692, 2024.

11:00–11:10
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EGU24-2081
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ECS
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Highlight
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On-site presentation
Malve Heinz, Maria Eliza Turek, Annelie Holzkämper, Bettina Schaefli, and Christoph Raible

In Central Europe, increasing temperatures and declining summer precipitation intensify the water and heat stress on crops and reduce water availability for irrigation from rivers and groundwater. Thus, approaches that reduce the need for irrigation are required. In this study, we quantify the potential of soil and crop management adaptations to reduce irrigation deficits for a mid-sized rainfed catchment in Switzerland. The Broye catchment, comprising 68 % agricultural land with a notable portion dedicated to irrigated agriculture, faces frequent summer irrigation bans. We employ the field-scale agro-hydrological model (SWAP) aiming to 1) quantify irrigation demand at the catchment scale, 2) assess the impacts of temporary irrigation bans on irrigation deficits, and 3) explore the potential of soil and crop management adaptations to reduce these irrigation deficits. SWAP simulates horizontal solute, heat and water flow in the vadose zone and crop growth at a daily timestep. The model calibration process involves a comprehensive global sensitivity analysis and parameter optimization. The optimization aims to maximize the model's fit to reference data on crop yield and seasonal irrigation amounts from the study region. Spatial climate, land use, and soil input data enable the quantification of irrigation water demand on the catchment scale. We simulated the exceptionally hot and dry summer of 2022, revealing a 57 % deficit in water supply and again emphasizing the importance of reducing reliance on irrigation. We further evaluate the effectiveness of measures such as increased soil organic carbon content and planting earlier maturing crop varieties in reducing irrigation demand. Our findings provide valuable insights for sustainable water management in midsized rainfed catchments, particularly in the face of climate change and evolving water use conflicts. As a next step, we plan to couple the field-scale model with a catchment-scale rainfall-runoff model to evaluate the effects of implementing such measures on the catchment's water balance.

How to cite: Heinz, M., Turek, M. E., Holzkämper, A., Schaefli, B., and Raible, C.: Exploring the possibilities to reduce irrigation demands through adaptations in soil and crop management, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-2081, https://doi.org/10.5194/egusphere-egu24-2081, 2024.

11:10–11:20
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EGU24-20070
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On-site presentation
Winter irrigation targeting deep soil water storage for orchards under water shortage
(withdrawn)
Tamir Kamai and Or Sperling
11:20–11:30
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EGU24-2190
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ECS
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On-site presentation
Chenyao Guo, Chenzhi Yao, Jingwei Wu, Shuai Qin, and Haoyu Yang

A reasonable layout of subsurface drainage systems is considered essential for maximizing its drainage and salt control effectiveness. In the saline-alkali farmland of arid regions in Northwest China, clay interlayers are common; however, the influence of clay interlayers on the layout of the subsurface drainage has not been extensively considered in the literature. This study investigated the process of subsurface drainage and salt discharge in salt-affected fields with clay layers using field experiments and numerical simulations. Four field experiments were conducted, considering three different relative positions between the drainage pipes and clay interlayers. The results showed that the clay interlayers hindered water infiltration; however, the distribution of soil salinity in the soil profile varied with the buried depth of drainage pipes at different positions relative to the clay layer. When the buried depth of drainage pipes increased, the amount of water and salt discharged from drainage pipes increased, and the increase rate in salt discharge was greater than water drainage. A numerical model was calibrated and validated using the field experiment data, and 25 orthogonal numerical experiments were conducted to investigate the soil desalination effects of buried depth of drainage pipes, spacing between the pipes, permeability of the interlayer, and position of the clay interlayer. The results showed that the drainage pipe buried depth, spacing, and permeability of the clay layer had significant effects on the desalination rate (P < 0.01), while the position of the clay interlayer had no significant effect (P > 0.05). Therefore, subsurface drainage pipes should be placed below the clay interlayer. The desalination rate linearly increased with the buried depth of drainage pipe and permeability of the interlayer, and it increased exponentially with decreased spacing. An empirical formula for soil desalination rate considering interlayer and subsurface drainage pipe layout parameters was fabricated and used to determine the appropriate layout parameters.

How to cite: Guo, C., Yao, C., Wu, J., Qin, S., and Yang, H.: Field and numerical experiments of subsurface drainage systems in saline and clay interlayered fields in arid regions, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-2190, https://doi.org/10.5194/egusphere-egu24-2190, 2024.

11:30–11:40
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EGU24-12151
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ECS
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On-site presentation
Abdullah Muratoglu and Muhammed Sungur Demir

Agricultural activities account for a significant portion of global water consumption, emphasizing the need to improve water productivity in this sector. This can be achieved through the implementation of effective agricultural management practices, such as optimizing crop patterns, adjusting irrigation methods, and improving fertilization practices. The Water Footprint (WF) concept offers a comprehensive approach to assessing water consumption in agriculture, considering different types of water use. By integrating the WF methodology with hydrological modeling programs, a more detailed analysis of water consumption patterns can be achieved, overcoming previous limitations in understanding agricultural water use. This study aims to assess the water consumption patterns of maize under different spatio-temporal dynamics. The WF of maize, including blue, green, and grey components, was calculated using the Soil and Water Assessment Tool (SWAT) model in the Ceyhan Basin (Turkey) between 2011-2020. The study outputs indicated considerable spatial and temporal variations, with a total WF ranging from 350 to 1320 m3/t. Green WF (61-385 m3/t) is found to be less dominant in maize production across the basin, while blue water emerges as the primary component (25 to 870 m3/t). In this study, the utilization of the SWAT model provided detailed spatio-temporal results, allowing for adjustments in agricultural patterns. We obtained that, optimizing the cultivation regions of maize within the Ceyhan Basin has the potential to reduce the total WF by approximately 26% and the blue WF by 47%. This optimization could result in an annual saving of around 135 million m3 of irrigation water. Furthermore, the study also analyzed temporal water consumption patterns. The findings highlight the significant potential for water conservation in agricultural activities through the spatio-temporal optimization of blue and green water, taking into account hydrological characteristics.

How to cite: Muratoglu, A. and Demir, M. S.: Understanding spatio-temporal variations in crop water consumption: Applying the WF Methodology Integrated with the SWAT Model, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-12151, https://doi.org/10.5194/egusphere-egu24-12151, 2024.

11:40–11:50
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EGU24-9057
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ECS
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On-site presentation
Lin Wang, Tim De Cuypere, Sabien Pollet, Sarah Garré, and Wim Corneils

Hydraulic properties of agricultural soils exhibit dynamic temporal variations influenced by field management practices, such as tillage and irrigation, as well as climatic factors, particularly changes in precipitation and temperature. With the emergence of using treated wastewater (TWW) in irrigation as a solution to alleviate increased pressure on available water resources, but characterized by elevated salt and solute concentrations, understanding its potential impact on soil hydraulic properties is crucial. In this study, we aimed to discern the influences of field management practices and irrigation water sources on the temporal variability of soil hydraulic conductivity.

Mini disk infiltrometers were employed to assess near-saturated hydraulic conductivity Kh and associated soil indicators (including soil’s electrical conductivity ECe, sodium adsorption ratio SAR, water repellency WR, bulk density BD, aggregate stability AS, and air permeability Ka) in the top 20 cm of a Retisol soil in Beitem (50°91′N, 3°12′E), Belgium. A comparative analysis was conducted to evaluate the effects of irrigation using treated wastewater (from households, from vegetable industry and from potato industry) and rainwater, relative to those under rainwater irrigation conditions. All treatments significantly affected ECe and SAR. Across four replicated plots per treatment, Kh was measured at distinct matric potentials on various dates, spanning a wet (2021) and a dry (2022) year, during a crop rotation of cauliflower (Brassica oleracea L.) and spinach (Spinacia oleracea L.). The plots were tilled with a rotary harrow till 30 cm depth to prepare the seedbeds.

Our findings highlighted tillage as the predominant factor influencing Kh . Irrespective of the irrigation type, Kh increased post-tillage and subsequently decreased throughout the growing season. Yearly weather differences also played a significant role, with the dry, warm year resulting in a higher average Kh at each matric potential. Surprisingly, there were no significant differences in Khbetween irrigation treatments over two crop cycles

Despite the elevation of soil salinity (ECe) and sodicity (SAR) with TWW irrigation, it did not detrimentally impact or other soil attributes (WR, BD, AS, and Ka) in this study. Our results underscore the importance of considering the interplay of tillage, weather conditions, the timing/frequency of irrigation/rain events, and matric potential when evaluating the effects of different irrigation sources on soil hydraulic properties.

How to cite: Wang, L., Cuypere, T. D., Pollet, S., Garré, S., and Corneils, W.: Temporal impact of treated wastewater irrigation on field hydraulic conductivity, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-9057, https://doi.org/10.5194/egusphere-egu24-9057, 2024.

11:50–12:00
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EGU24-9563
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ECS
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On-site presentation
Shuai Qin, Chenyao Guo, and Jingwei Wu

The clogging problem of geotextile envelopes in subsurface drainage pipes in arid areas can lead to a reduction of the drainage capacity in the drainage system. The current research on combined clogging is mostly in the stage of phenomenological observations or indoor experiments, and quantitative methods are lacking. In this study, a model for predicting permeability of geotextile envelope was developed using pore distribution theory of geotextile envelope. Then, a stepwise coupled combined clogging model was proposed based on the evolution characteristics of physical and chemical clogging. The coupled model was verified by field sampling, and the measured results of the three sites were within the range of the predicted values. Then, the main factors affecting the combined clogging model of the geotextile envelope were analyzed, and the clogging evolution was predicted. The results showed that the combined clogging model was sensitive to the physical clogging coefficient β1 during the first 30 days and more sensitive to the calcium carbonate saturation index (SI) after 30 days of drainage. When β1 was equal to 0.3, a saturation index greater than 1.0, which corresponds to drainage mineralization exceeding 3.0 g/L, indicated a high risk of clogging in Xinjiang.

How to cite: Qin, S., Guo, C., and Wu, J.: A model for predicting permeability of geotextile envelope after combined clogging in arid areas, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-9563, https://doi.org/10.5194/egusphere-egu24-9563, 2024.

12:00–12:10
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EGU24-11295
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ECS
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On-site presentation
Giulio Gilardi, Darya Tkachenko, Michele Rienzner, and Arianna Facchi

The implementation of adaptation strategies is becoming increasingly important to mitigate climate-related risks and water resource overuse in agriculture. When considering large spatial domains, the assessment of alternative irrigation techniques can be carried out using a modelling approach, useful to take into consideration all the relevant processes in complex agro-ecosystems.

In ‘fully distributed’ models, the domain of interest is divided into simulation units, each characterized by a unique set of parameters and inputs, by using a regular grid. In ‘semi-distributed’ models, simulation units correspond with spatial units of different size and shape but homogeneous in terms of parameters and inputs. Moreover, if the description of processes is based on simplified schematization of the physical system and equations, models are referred as ‘conceptual’, whereas if an accurate physical-mathematical description is adopted, they are considered as ‘physically based’. Because of their complexity and computational requirements, ‘physically based’ models are often applied in a ‘semi-distributed’ manner when describing large territories.

A framework is currently under development to directly link a file-based vector database (GeoPackage), describing the main features of an agricultural area, and ‘physically based’ simulations carried out by the SWAP model (https://www.swap.alterra.nl/). The framework, written in Python, runs within the QGIS environment. It requires the user to define seven basic themes: I) a district domain, II) soil types, III) land uses, IV) irrigation water distribution areas, V) homogeneous groundwater depth polygons or groundwater level measuring stations, VI) homogeneous agro-meteorological polygons or agro-meteorological stations, and VII) a DTM raster layer. From the intersection of the layers considered, a number of polygons are generated. Next, the polygons are post-processed based on of the following options: a) aggregate all polygons characterized by the same value of the input themes, b) maintain all the polygons obtained through the intersection operation, or c) aggregate polygons based on a critical distance (meters). This last option is useful to limit the number of polygons and reduce the computational effort. In the case of multiple groundwater level or agro-meteorological measuring stations, the framework calculates the values of the variables to be assigned to each polygon through the ‘Inverse Distance Weighting’ (IDW) algorithm. Finally, the framework links each unit to its parameter set, transferring the information stored in the database into the SWAP input files. Simulation results are saved in a tabular format that allows them to be analyzed according to different aggregations (by land use, soil type, etc.) and to produce time series graphs or vector maps.

The application of the tool for the estimation of the irrigation requirements and the percolation fluxes of the Lomellina region (northern Italy) under the current and alternative irrigation strategies will be presented and discussed. The study area, located on the left bank of the Po River, covers more than 125,000 hectares mainly cropped with rice. In more recent years, this area is experiencing water shortages and a reduction in aquifer levels.

How to cite: Gilardi, G., Tkachenko, D., Rienzner, M., and Facchi, A.: Development of a new modeling framework for estimating water needs in lowland agricultural areas: linking GIS database and SWAP simulation, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-11295, https://doi.org/10.5194/egusphere-egu24-11295, 2024.

12:10–12:20
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EGU24-6964
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ECS
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Virtual presentation
Xiulu Sun, Henk Ritzema, Jos van Dam, and Petra Hellegers

The North China Plain (NCP) stands as a densely populated region vital for agriculture, sustaining a large population through intensive farming practices. However, the reliance on irrigation and fertilization in the region has led to inefficiencies in water and nutrient use, compromising the sustainability of agriculture and contributing to environmental degradation. To address these challenges, the focus of this study is on optimizing water and fertilizer management, particularly through surface fertigation. This method involves applying fertilizers dissolved in irrigation water to enhance water use efficiency (WUE) and nitrogen use efficiency (NUE). Each section explores different facets of surface fertigation, aiming to improve the uniformity of fertilizer distribution in irrigation water, subsequently enhancing crop yields while reducing water and fertilizer leaching.

A participatory study in the People's Victory Canal Irrigation District revealed farmers' satisfaction with current practices but identified obstacles to adopting more efficient technologies. Challenges included a lack of knowledge about advanced fertigation systems, constraints of small-scale farming, and high implementation costs. Tailored guidelines grounded in empirical evidence and considering socio-economic factors are crucial for overcoming these challenges. An experimental approach in subsequent sections evaluated surface fertigation practices tailored to NCP farmers' fields. Traditional methods showed low field application efficiency and uneven distribution of water and fertilizers. The WinSRFR model aided in understanding these practices, leading to proposed methods for enhancing application efficiency and distribution uniformity. Optimal irrigation depths for wheat and maize were identified to be 95 mm and 80 mm, respectively. Continuing with field experiments and modeling, the study analyzed the impact of irrigation and fertigation practices on crop yield, WUE, NUE, and nitrogen loss. The findings emphasized the need for integrating optimized irrigation and fertigation strategies for sustainable crop production and minimized nitrogen loss. The viability of transitioning smallholder farmers in the NCP to organic fertilizer application through surface fertigation was explored. A 50% organic fertilizer ratio was found to balance maintaining crop yield and minimizing nitrogen leaching. The study advocated for compensation to offset additional costs for farmers adopting organic fertilizers.

In conclusion, the study highlights inefficiencies in current irrigation and fertilization practices in the NCP and suggests surface fertigation as a promising solution. Refining practices, such as adjusting irrigation depth and fertigation scheduling, can significantly enhance WUE, NUE, and mitigate environmental impacts. The research underscores the importance of tailoring solutions to local conditions and farmer preferences, emphasizing the need for government support and incentives to facilitate the adoption of sustainable practices. The research methodology reflects a commitment to evidence-based approaches, utilizing participatory tools, field experiments, and simulation models to assess and refine fertigation strategies. Looking ahead, successful implementation of improved practices relies on understanding and engaging with the local farming community, addressing their concerns, enhancing their knowledge, and providing cost-effective solutions. The research suggests a pathway towards sustainable agriculture in the NCP, emphasizing the need for a comprehensive approach considering both environmental and socio-economic factors.

How to cite: Sun, X., Ritzema, H., van Dam, J., and Hellegers, P.: Surface Fertigation Practices for Smallholder Farmers in the North China Plain, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-6964, https://doi.org/10.5194/egusphere-egu24-6964, 2024.

12:20–12:30
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EGU24-1726
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ECS
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On-site presentation
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Maria Eliza Turek, Annelie Holzkämper, and Attila Nemes

Increasing frequencies and intensities of drought periods are likely to aggravate conflicts between agricultural demands and other human and ecological demands for water resources. Improving the natural soil water retention capacity can help to defuse these conflicts and at the same time strengthen climate mitigation, biodiversity, and food security. Increasing soil organic carbon content (SOC) is seen as a promising negative emission technology for the agricultural sector, with the co-benefit of potentially increasing the soil water retention capacity. We tested how different levels of SOC at varying soil depths influence in the transpiration reduction caused by drought stress (Treddry) in maize under current and future climatic conditions. We used the SWAP (Soil Water Atmosphere Plant) model validated utilizing information from a long-term lysimeter for a typical Swiss soil and applied it at three distinct climatic regions. A pedotransfer function (PTF) was used to indirectly assess the effects of SOC on soil hydraulic properties that affected the drought stress. Study findings revealed that increasing SOC down to 65 cm depth is beneficial to reduce drought limitations in maize. These benefits are minimal if SOC is only increased in the top 25 cm but become considerable if SOC is increased down to 65 or 135 cm depth. With a 2% addition of SOC down to 65 cm depth, a considerable average transpiration gain of 40 mm can be reached. It appears that a greater or deeper SOC addition would not return substantial extra benefits in terms of offsetting more crop drought stress rooting in the changing climate.

How to cite: Turek, M. E., Holzkämper, A., and Nemes, A.: Benefits of increasing soil organic carbon to reduce drought stress in maize under climate change, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-1726, https://doi.org/10.5194/egusphere-egu24-1726, 2024.

Posters on site: Fri, 19 Apr, 16:15–18:00 | Hall A

Display time: Fri, 19 Apr, 14:00–Fri, 19 Apr, 18:00
Chairpersons: Marco Peli, Mira Haddad, Giulio Castelli
A.114
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EGU24-3837
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ECS
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Highlight
Erika Lucía Rodríguez Lache, Guillaume Blanchy, Ali Mehmandoostkotlar, and Sarah Garré

Drainage systems are essential for cultivated fields, ensuring optimal growth conditions for crops by preventing root zone wet stress. However, these conventional drainage systems also lead to a significant loss of water, a valuable resource that could be used to sustain crops during dry (summer) months. To address this, climate adaptive drainage or controlled drainage is employed, raising the water table “when possible given the ongoing agricultural activities”. This approach enhances aquifer recharge and stores excess water for use during the summer. Nevertheless, it remains unclear for farmers and water managers whether climate-adaptive drainage will improve agricultural performance and, if so, how to precisely manage water levels throughout the growing season to optimize performance. 

In this study, we conduct a synthetic experiment using the SWAP model to investigate the complex interaction between drainage types under different meteorological conditions, soil characteristics, and crop types. Our research aims to provide insights into the effect of climate-adaptive drainage for both farmers and water managers.

Our findings highlight that controlled drainage significantly enhances soil water content in sandy and loamy soils, contributing to climate resilience. However, its effectiveness in clay soils is small. It is important to note that climate-adaptive drainage has the potential to raise groundwater levels across all soil types, posing a potential risk of oxygen stress on crops. Regardless of soil type, the implementation of controlled drainage results in increased surface runoff and groundwater recharge, associated with a reduction in drainage flux. While the augmented surface runoff  poses potential issues such as soil erosion and water pollution, the positive aspect lies in the enhanced groundwater recharge, crucial for maintaining water availability and supporting ecological systems.

How to cite: Rodríguez Lache, E. L., Blanchy, G., Mehmandoostkotlar, A., and Garré, S.: Exploring climate-adaptive drainage in water management: Enhancing soil moisture, crop resilience and groundwater recharge., EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-3837, https://doi.org/10.5194/egusphere-egu24-3837, 2024.

A.115
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EGU24-6546
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ECS
Mengqi Wu, Tobias Klauder, Mika Tarkka, Doris Vetterlein, and Steffen Schlüter

Soil moisture, as a key indicator of soil functionality, is significantly influenced by the evolution of soil-plant systems and the hydrologic cycle. Little long-term data is available about how land use and climate change affect the spatial and temporal distribution of soil water. In particular the variations in deeper subsoil layers are poorly documented. Here, the effects of five land use types, including two croplands with conventional and organic farming (CF and OF) and three grasslands with intensive and extensive meadow (IM and EM), as well as extensive pasture (EP) on soil moisture profiles were investigated at the Global Change Experimental Facility (GCEF), at Bad Lauchstädt in the German dryland belt. The facility harbors two climate treatments. The ambient climate and a future climate with increased temperature by ~0.55 C across seasons, and the altered precipitation patterns by ~9 % additional irrigation in spring and autumn, and ~21 % reduction in summer. The soil moisture profiles were bi-weekly monitored with a portable probe (TRIME Pico IPH) down to 110 cm for two continuous years.

Soil moisture content in topsoil and subsoil reflected the presence and size of transpiring plants, i.e. from October to next April, the soil water content was lower in grasslands than in croplands, which planted winter crops. During summer, there was a marked decrease in soil water content in the deeper soil layers of grasslands, while the crop on the cropland was already harvested. As a result, the recovery of soil water storage was faster during winter in croplands than in grasslands. Within croplands, OF had higher moisture than CF below 30 cm during the whole growing season and beyond due to less vigorous growth imposed by nutrient deficits. Within grasslands, differences in soil moisture only emerged in deeper soil (> 70 cm). In general, soil moisture in the shallow soil layers (0 - 20 cm) was very similar across land uses and climate scenarios and these clear differences only emerged in deeper soil. In the deeper soil (< 50 cm), croplands and extensively used grasslands showed an obvious increase of soil moisture in future treatment, especially during wet spring and summer.

Our results clearly indicate long-term differences in soil moisture between the land uses. Climate manipulation at the GCEF only manifests itself in the subsoil (> 50 cm), by contrast, topsoil (< 30 cm) was more controlled by short-term dynamics induced by evaporation and precipitation. These findings stress the importance of deep soil moisture monitoring for a more comprehensive assessment of the water budget. 

How to cite: Wu, M., Klauder, T., Tarkka, M., Vetterlein, D., and Schlüter, S.: The effect of land use types and climate change on soil moisture profile dynamics, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-6546, https://doi.org/10.5194/egusphere-egu24-6546, 2024.

A.116
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EGU24-6804
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ECS
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Highlight
Jorge Preciado, Alexander Fernald, and Richard Heerema

Water balance is important to provide information and to conserve water. The flow of water in the system can be used to help and manage water supply, changes in management can increase water productivity in arid regions. For this study, soil water content was measured from one soil column within the orchards using time-domain reflectometry probes installed at different depths in the root zone of pecan fields. This data was analyzed to compare the irrigation systems. Water that passes the root zone was considered deep percolation. This research compared the amount of water stored on each field and water consumed by the trees for the last four irrigation seasons 2020 - 2023. Quantifying water from irrigation was essential to know how much water would recharge the Mesilla basin. Percolation was higher in the flood section, with 52 % of the total water applied, while in the drip, percolation was less than 5% of the total water applied moving down in the field for the 2021 growing season. In addition, there were differences in crop yield between the irrigation systems. This study estimated recharge and modeled water flow through the soil in drip and flood-irrigated pecan orchards to understand better surface water and groundwater interactions for improved river basin water management strategies and quantifies water stored in the ground lost through evapotranspiration. In addition, this project evaluates which irrigation scenario could best grow sustainable pecans in arid regions, reducing water use while maintaining crop production. It presents a balance of the two irrigation systems to understand the implications of climate change on the water cycle and achieve sustainability in the crops grown in the area.

How to cite: Preciado, J., Fernald, A., and Heerema, R.: Groundwater Recharge in Pecan Orchards Under Different Irrigation Systems to Reduce the Impacts of Climate Change in the Southwest USA, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-6804, https://doi.org/10.5194/egusphere-egu24-6804, 2024.

A.117
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EGU24-7726
Shaoyi Duan and Huimin Lei

Abstract: The Hetao Irrigation District (HID) is located in the arid region along the upper reach of the Yellow River and is an important grain production area in northwest China. Water diverted from the Yellow River is an indispensable water supply of the crop production in this region. Unfortunately, traditional irrigation, drainage and fertilization practices have resulted in severe soil salinization and inefficient of water use, which poses a great challenge to food security and water resources. Therefore, it is important to search a new practice that can achieve water saving, salinity control, and yield increase simultaneously. To this end, this study applied a framework that combined the SWAP model and a multi-criteria decision-making method.

First, we used a total of 21 station-years of experimental data from 12 spring wheat and spring maize sites for parameter calibration by the PEST package. The sensitive parameters of spring wheat and spring maize were obtained, and the evaluation showed that the SWAP model is capable of simulating seasonal variations of leaf area index, evapotranspiration, soil moisture and soil salt content. Specially, we showed that the parameters SALTMAX (threshold salt concentration in soil water) and TSUMEA (temperature sum from emergence to anthesis) were obviously different from the default values of wheat and maize in the SWAP.

Second, we designed simulation scenarios based on the combinations of irrigation, drainage and fertilization practices, constrained by the local customs and water supply from the Yellow River. The simulated crop yield, water use efficiency (i.e., the crop production per irrigation water amount), and soil salt content change were obtained by the SWAP model.

Finally, based on the SWAP-simulated results, optimal practices were obtained with the help of the VIKOR method, a multi-criteria decision-making method which has the advantage of objectively determining the weights of water use efficiency, crop yield, and soil salt content change. Compared with the traditional practices by farmers, the optimal practice can not only increase crop yield by 20 per cent and improve water use efficiency by more than 10 per cent, but also ensure the soil salt content does not increase.

 

Keywords: Irrigation; Drainage; Fertilization; SWAP model; VIKOR method

How to cite: Duan, S. and Lei, H.: Searching for optimal practices for water saving, salinity control and yield increase in an arid and salinity irrigated area of China using the SWAP-based method., EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-7726, https://doi.org/10.5194/egusphere-egu24-7726, 2024.

A.118
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EGU24-8199
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Dario Autovino, Massimo Iovino, and Giorgio Baiamonte

In surface and subsurface drip irrigation systems, predicting the size expansion of the wetting bulb and the irrigation time are mandatory for water saving, and help drive their design and scheduling. At this aim, different hydrological models have been suggested to predict the wetting bulb expansion from buried and surface point sources. In this work, we compare the results obtained by the application of Hydrus-2D/3D and Philip (1984) model.

The Philip (1984) model accounts for the Gardner conductivity function, which is not implemented in Hydrus 2D/3D. Moreover, in the Philip (1984) model, a certain approximation in the choice of the water contents to be used for calculating the average volumetric water content behind the wetting front, θav, is necessary, also considering that definitions do not seem univocal. For example, the water content at the wetting front was assumed as the θav, value when soil hydraulic conductivity, K, was equal to 1 mm/day by Cook et al. (2003) and 1 mm/h by Thorburn et al. (2003).

For the purpose of the comparison, an extended analysis aiming at detecting the parameter ranges of the van Genuchten-Mualem model (van Genuchten 1980), which provide hydraulic conductivity functions matching those of Gardner, was preliminary conducted. Then, for van Genuchten-Mualem parameters falling in such parameters’ ranges, the average volumetric water content that is required in the Philip (1984) model was calculated in Hydrus-2D/3D.

For sandy-loam soil, results showed a quite good agreement between the simplified Philip (1984) model and the more accurate but numerically demanding Hydrus 2D/3D, suggesting that Philip (1984)’s model can be successfully applied to predict the wetting bulb expansion from buried and surface point sources, provided the average volumetric water content in the soil behind the wetting front and the saturated hydraulic conductivity are appropriately considered.

Keywords: wetting bulb, buried sources, surface sources, Philip (1984)’s model, Hydrus 2D/3D.

Acknowledgement: This study was carried out within the RETURN Extended Partnership and received funding from the European Union Next-GenerationEU (National Recovery and Resilience Plan – NRRP, Mission 4, Component 2, Investment 1.3 – D.D. 1243 2/8/2022, PE0000005).

References:

Cook, F.J., P.J., Thorburn, K.L., Bristow, and C.M., Cote, “Infiltration from surface and buried point sources: The Average wetting water content”, Water Resour. Res., 2003, 39(12): 1364, doi:10.1029/2003WR002554.

Philip, J.R., “Travel times from buried and surface infiltration point sources”, Water Resour. Res., 1984, 20(7), 990–994, https://doi.org/10.1029/WR020i007p00990.

Thorburn, P.J., F.J., Cook, and K.L., Bristow, “Soil-dependent wetting from trickle emitters: Implications for system design and management”, Irrig. Sci., 2003, 22: 121–127, doi 10.1007/s00271-003-0077-3.

van Genuchten, M. Th., “A closed form equation for predicting the hydraulic conductivity of unsaturated soils”, Soil Sci. Soc. Am. J., 1980, 44: 892-898.

How to cite: Autovino, D., Iovino, M., and Baiamonte, G.: Comparing Hydrus-2D/3D and Philip (1984)’s model to assess wetting bulb expansion from buried and surface point sources, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-8199, https://doi.org/10.5194/egusphere-egu24-8199, 2024.

A.119
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EGU24-12460
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ECS
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Simran Sekhri, Volker Kleinschmidt, Annette Eschenbach, and Joscha N Becker

In semi-arid and arid regions, prolonged dry spells lead to a significant reduction in topsoil moisture, forming a dry soil layer, where water can only move as vapor. Such conditions hinder young crops with weakly developed root systems to directly reach deep water reservoir. Since there is no indication of gaseous water uptake from soil pores, plants might be able to acquire water from these deep sources when water vapor condensates at night or at a vapor barrier (mulch). To trace potential water vapor uptake by plants, we developed a sand column experiment using deuterium labeled water. The water source column was separated by a glass bead layer and a root barrier (50µm mesh) from the soil to ensure that there was no capillary rise or root uptake of liquid water. Four treatments with three replicates, including planted (Pl), unplanted (Un), mulch variation (Pl+M; Un+M) and an additional unlabeled control column, were installed in a climatic chamber. Vigna radiata a moderately drought resistant plant species was selected for this experiment. Constant day-night cycle with stable temperature and light conditions were maintained for a period of seven days without irrigation. Afterwards, soil samples were collected at 0-5, 5-10 and 10-15 cm depths. Vigna radiata saplings and condensed water samples were collected separately. Cryo-extraction of water from the samples and liquid isotopic water analysis revealed substantial results for the uptake of water vapor by young saplings. Evaporation from the water source into the column was recorded to be 0.7-2.1 ml. The δD/H ratios were analysed using Triple Isotope Water Analyser (Los Gatos Research). The relative potential uptake of water vapor by young saplings was recorded to be as high as 0.56ml for the 'Pl' and 0.35ml for the 'Pl+M' treatment. The utilization of water vapor by young plants in the upper soil layer could prolong plant life during dry spells. Although, it remains uncertain to what extent the prolongation could be maintained.

Keywords: Deuterium Labeled Water, Plant Vitality, Water Conductivity

How to cite: Sekhri, S., Kleinschmidt, V., Eschenbach, A., and Becker, J. N.: Water vapor movement and utilization with condensation in the upper layers of a sandy soil column, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-12460, https://doi.org/10.5194/egusphere-egu24-12460, 2024.

A.120
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EGU24-18026
Davide Canone, Davide Gisolo, Luca Nari, Francesca Pettiti, Alessio Gentile, Stefano Ferraris, Mattia Barezzi, Umberto Garlando, and Danilo Demarchi

The Wappfruit project objective is to optimize the irrigation techniques for water and energy saving in fruit orchards in the Piemonte Region, Northwest Italy. The stakeholders of the project are Politecnico and the University of Torino, Piemonte Region, Agrion Foundation for Research in Agriculture, Astel S.r.l. (for the industrialisation of the experimental hardware developed by Politecnico di Torino), and three farms (“La Marchisa” and “Lorenzo Sacchetto” – apple orchards and “Paolo Vassallo” – actinidia orchard).  In each farm, two areas were identified, an “experimental area” where the new set-up was tested and a control area where the farmers continued the irrigation as usual.

In the year 2023, the Wappfruit project has shown the potentiality of a smart irrigation solution composed of two kinds of IoT (Internet of Things) nodes employing LoRa technology and governed by a 24/7 server script, written in Python, that acquires soil matric potential and decides the opening and closure of the irrigation pumps in real-time. The soil matric potential thresholds, identified in 2022 and early 2023, (-60 kPa and -25 kPa at 20 cm of depth for the activation of the irrigation, respectively in the apple and Actinidia orchards; -50 kPa at 40 and 20 cm of depth and -18 kPa at 20 cm of depth, for the deactivation of the irrigation, again respectively for apple and Actinidia orchards) were verified again after a campaign in which soil parameters (saturated soil water content, infiltration velocity at saturation) were measured. These values were used for new model simulations that included irrigation. The thresholds for the apple orchards were confirmed, whereas new thresholds were identified for the Actinidia: -12 kPa (activation) and -5 kPa (deactivation). Results highlight that these thresholds can activate and deactivate the irrigation appropriately. The 2022 simulations show a matric potential in agreement with the measures collected (R between 0.51 and 0.88). Moreover, the 2023 simulations with modelled irrigation show a good agreement with the measures in the experimental area. Both the simulations and the real optimized irrigation generally show lower values if compared with the irrigation of the farmers (range: 13 – 217.5 mm/ha), with an exception in one apple orchard, where the model suggests more irrigation than expected, likely because of an overestimation of the water infiltration velocity. The hardware/software design and implementation have shown that low-cost low-power electronic devices and artificial intelligence can be reliable and very inexpensive for water and energy savings. The remote control of the system is another important achievement. Moreover, optimized irrigation does not affect the vegetation productivity and increases the fruit quality.

How to cite: Canone, D., Gisolo, D., Nari, L., Pettiti, F., Gentile, A., Ferraris, S., Barezzi, M., Garlando, U., and Demarchi, D.: Wappfruit, a project for the optimization of the irrigation in agriculture: final results, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-18026, https://doi.org/10.5194/egusphere-egu24-18026, 2024.

A.121
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EGU24-19384
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ECS
Haoyu Yang, Chenyao Guo, and Jingwei Wu

Subsurface drainage is widely used in farmland. Entrance resistance occurs when water flows into a perforated drain pipe, reducing the drainage efficiency and resulting in a high water table. Using the real radius will overestimate the drainage discharge. Accurately calculating effective radius is essential for subsurface drainage calculation and simulation. New effective radius formulas for corrugated drains wrapped with a thin geotextile were proposed by dividing the entrance resistance into corrugation and perforation resistance. The accuracy of the formulas was verified by sand tank experiments. Sensitivity analysis was conducted to determine the factors that affected effective radius, indicating that corrugation was the main factor. When the radius and structure of the drain wall were determined, the opening area exhibited high sensitivity with interactivity between it and drainage discharge. The effect of the opening area and position of the perforations on the effective radius was evaluated for different drainage discharges. Putting the perforations on the bottom was better for drainage efficiency. For small drainage discharge of less than 0.1 cm3 s-1 cm-1, the opening area was not significant, and an opening area of 15 cm2 m-1 was sufficient. However, for greater drainage discharge, an opening area of 60 cm2 m-1 with three or more row perforations would be required.

How to cite: Yang, H., Guo, C., and Wu, J.: Effective radius of corrugated drainage pipes wrapped with a thin geotextile envelope, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-19384, https://doi.org/10.5194/egusphere-egu24-19384, 2024.

A.122
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EGU24-20020
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Highlight
Youssouf Belaid, Abeyou Worqlul, Mira Haddad, Aseela Al Moalla, and Fouad Lamghari Ridouane

The emirate of Fujairah, spanning approximately 1,450 km², is characterised by a landscape dominated by rugged mountains, encompassing 77% of its total surface area. Despite its average precipitation of less than 150 mm, Fujairah hosts a thriving ecosystem supported by national tree plantations, including Acacia nilotica, Acacia tortilis, Prosopis cineraria, and Zizyphus spina-christi. These plantations are crucial in providing ecosystem services, notably contributing to honey bee production.

This study attempts to support the increase of vegetation cover in Fujairah through sustainable land management practices of using water harvesting and planting native trees by employing cutting-edge technology. Through the integration of Remote Sensing and Geographic Information System (GIS)-driven Multi-Criteria Evaluation (MCE), the research identifies optimal areas for planting native honey trees. Emphasising sustainability, the methodology incorporates water harvesting techniques that eliminate reliance on traditional irrigation methods for plantation.

Local and international datasets encompassing biophysical parameters such as land use, digital elevation models, slope, topographic wetness index, soil texture, and climate data are combined. Additionally, the study considers optimal ecological conditions for native trees, including temperature and soil pH. The resulting suitability maps, treated as future land cover maps, are employed alongside soil sample data to estimate carbon storage and sequestration potential.

Furthermore, the research investigates indigenous water harvesting knowledge in Fujairah through a comprehensive survey. This survey explores community awareness, historical context, current applications, technical specifics of water harvesting and native tree plantation practices, environmental considerations, and potential obstacles and solutions.

The findings aim to inform a holistic approach to sustainably enhancing Fujairah's vegetation cover, providing valuable insights for environmental conservation and community engagement.

Keywords: Suitability mapping, water harvesting techniques, Sustainable land management, and Ecosystem Services

How to cite: Belaid, Y., Worqlul, A., Haddad, M., Al Moalla, A., and Lamghari Ridouane, F.: Enhancing Vegetation Cover in Fujairah through Sustainable Honey Tree Plantations and Water Harvesting Technique: A Multi-Criteria Suitability Mapping, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-20020, https://doi.org/10.5194/egusphere-egu24-20020, 2024.

A.123
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EGU24-20913
Csilla Farkas, Moritz Shore, Ágota Horel, Gökhan Cüceloglu, Levente Czelnai, Dorota Mirosław-Świątek, Maria Eliza Turek, Natalja Cerkasova, Brigitta Szabó, Antonín Zajiček, Attila Nemes, Sinja Weiland, Petr Fucik, Annelie Holzkaemper, Rasa Idzelyté, and Stepan Marval

Within the EU Horizon project OPTAIN (OPtimal strategies to reTAIN and re-use water and nutrients in small agricultural catchments across different soil-climatic regions in Europe, optain.eu) project, the effects of Natural/Small Water Retention Measures (NSWRMs) on water regime, soil erosion and nutrient transport are evaluated at both, catchment- and field-scales for present and future climate conditions. Our goal is to perform an integrated, model-based assessment of the effectiveness of NSWRMs at field scale and cross-validated these results from those obtained from the catchment-scale modelling. The field-scale assessment is based on the adaptation of the SWAP mathematical model to seven pilot sites across three European biogeographical regions and on combined NSWRM – projected climate scenario analyses. The scenarios are designed to evaluate the efficiency and potential of different natural/small water retention measures in improving soil water retention and reducing flash floods and the loss of soil and nutrients under changing climate conditions. We present the harmonized SWAP modelling workflow and the combined scenario analyses, including the implementation of various in-field measures in the SWAP model. Examples of model calibration, validation and scenario results for selected pilot sites will be given.

How to cite: Farkas, C., Shore, M., Horel, Á., Cüceloglu, G., Czelnai, L., Mirosław-Świątek, D., Turek, M. E., Cerkasova, N., Szabó, B., Zajiček, A., Nemes, A., Weiland, S., Fucik, P., Holzkaemper, A., Idzelyté, R., and Marval, S.: Effectiveness of natural soil water retention measures at field scale under current and future climate – case studies in three European biogeographical regions, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-20913, https://doi.org/10.5194/egusphere-egu24-20913, 2024.

A.124
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EGU24-20983
Stefano Barontini, Martina Greta Caffi, Muhammad Faisal Hanif, Elpida Kolokytha, Dimitrios Malamataris, and Marco Peli

Many agroecosystems are experiencing an increase of agricultural water demand which risks depleting the natural reservoirs, viz lakes and aquifers. The increasing temperature reduces glacier extent and snow accumulation, thus reducing the dry—season water availability, and challenging the agricultural systems and the food security, particularly in arid and semiarid regions.

Aiming at contributing to defining effective strategies that are able to provide robust and parametric parsimonious estimates of the irrigation water demand of the agroecosystems at the planning level, we propose a framework based on the joint use of Melisenda’s aridity index, Benfratello’s water balance and Budyko’s curve to define the crop proneness to the hydrological sustainability.

The strategy is based on Benfratello’s (1961) explicit and conservative method to assess the soil water balance and the irrigation deficit in semiarid Mediterranean climates. The method is parametrized by means of an aridity index (Melisenda, 1964) to assess the soil proneness to water surplus formation, and the results are compared with the natural ecosystem deficit as provided by Budyko’s (1974) curve. Coupling these climatic water balances with a crop based estimate of the maximum required evapotranspiration, as given by the FAO procedure, it is possible to assess the expected crop irrigation deficit.

Our strategy is two—step. The first step is mapping Melisenda’s index, to identify the climatically—wet areas and the potentially climatically—dry areas. In potentially dry areas field capacity may not be refilled during the dry season, if it is greater than a critical value. It is worth noting that the greater is the field capacity, the smaller is the surplus water, and the greater is the crop water availability during the dry season. These maps may be produced both for the actual cultivations, and for some reference crops, viz millet, barley, rice and wheat, which are important for food security, to depict the local hydrological attitude to them.

The second step is the calculation of the monthly and annual irrigation deficit by means of Benfratello’s water balance. The irrigation deficit does not depend only on the annual precipitation and on the annual crop water demand, but also on their annual regime. Benfratello’s irrigation deficit is then compared with the ecosystemic water deficit, provided by Budyko’s curve. The closer is the crop behaviour to Budyko’s curve, the closer is its water demand to the ecosystemic one, considered as a reference natural water demand.

In order to test the sensitivity of the procedure at characterising the water balance also in presence of small climatic differences, we applied it with promising results to two important and comparable Mediterranean agricultural districts, the Bonifica della Capitanata (Southern Italy, 4,410 km2, mainly cultivated with herbaceous crops, olives, fruit and grapevine trees) and the Mygdonia water basin (Northern Greece, 2,100 km2, 1,030 of which are cultivated mainly with cereals). The Köppen—Geiger climate type is mainly Cfa for both areas. De Martonne aridity index depicts a semi—dry to Mediterranean condition for the Capitanata and a mainly Mediterranean condition for the Mygdonia.

How to cite: Barontini, S., Caffi, M. G., Hanif, M. F., Kolokytha, E., Malamataris, D., and Peli, M.: A framework based on Melisenda’s aridity index and on Budyko’s curve to assess the crop proneness to the hydrological sustainability, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-20983, https://doi.org/10.5194/egusphere-egu24-20983, 2024.

Posters virtual: Fri, 19 Apr, 14:00–15:45 | vHall A

Display time: Fri, 19 Apr, 08:30–Fri, 19 Apr, 18:00
Chairpersons: Marco Peli, Mira Haddad, Giulio Castelli
vA.18
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EGU24-18956
Olfa Gharsallah, Arianna Facchi, Gerard Arbat, Sílvia Cufí, Francisco Ramírez de Cartagena, Marco Romani, Michele Rienzner, Darya Tkachenko, Concepcion Mira, Isabel Pedrosa de Lima, José Manuel Gonçalves, Abdrabbo Shehata Aboukheira, Saad Shebl, and Melih Enginsu

Rice is the world's most important food crop, as it is a staple food for more than half of the world's population, and the global demand for rice is expected to increase. More than 1,000,000 hectares in the Mediterranean basin are devoted to rice cultivation. The most important producing countries are Italy (IT) and Spain (SP) in Europe (over 310,000 ha), and Egypt (EG) and Turkey (TR) among non-EU countries (over 600,000 ha). In the Mediterranean region, rice production is of great socio-economic and environmental importance, as rice is often a crucial product for internal consumption and export, especially in Egypt, where it is considered strategic for food security. Despite of this, the peculiar flooding conditions in which rice is traditionally grown lead to the use of huge water volumes, as well as to the potential release of greenhouse gases and pesticides into the environment. For this reason, the introduction of water-saving irrigation strategies could reduce water consumption and decrease the harmful environmental impacts associated with rice flooding, while maintaining yield and rice grain quality.

In the context of the MEDWATERICE project (https://www.medwaterice.org/; PRIMA-2018), alternative irrigation methods to WFL were tested in case studies implemented in five Mediterranean countries (Italy, Spain, Portugal, Turkey, Egypt). Irrigation strategies for each CS were selected with the support of local Stake-Holder groups and applied in experimental fields measuring/estimating all the water balance terms on a daily basis. Wet seeding and alternate wetting and drying (AWD), dry seeding and delayed flooding (DFL), reduction of inlet/outlet discharges (WIR), a better control of ponding water level through automated gates (DFL-aut), hybrid irrigation (HYBRID), sprinkler irrigation (SPRINKLER), surface drip (DRIP) and subsurface drip irrigation (SDI) were implemented for at least two years in the period 2019-2021 alongside the traditional WFL, to investigate their environmental and economic sustainability and social acceptability.

How to cite: Gharsallah, O., Facchi, A., Arbat, G., Cufí, S., Ramírez de Cartagena, F., Romani, M., Rienzner, M., Tkachenko, D., Mira, C., de Lima, I. P., Gonçalves, J. M., Aboukheira, A. S., Shebl, S., and Enginsu, M.: Innovative irrigation strategies for rice in the Mediterranean areas, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-18956, https://doi.org/10.5194/egusphere-egu24-18956, 2024.