EGU21-8125
https://doi.org/10.5194/egusphere-egu21-8125
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Mapping of tank silt application using Sentinel-2 images over the Berambadi catchment (India).

Cécile Gomez1,2, Dharumarajan Subramanian3, Philippe Lagacherie1, Jean Riotte2,4, Sylvain Ferrant5, Muddu Sekhar2,6, and Laurent Ruiz2,4,7
Cécile Gomez et al.
  • 1LISAH, Univ. Montpellier, IRD, INRAE, Institut Agro, Montpellier, France.
  • 2Indo-French Cell for Water Sciences, IRD, Indian Institute of Science, Bangalore, India.
  • 3ICAR‐National Bureau of Soil Survey and Land Use Planning, Hebbal, Bangalore, India.
  • 4GET, Université Paul-Sabatier, IRD, CNRS, Toulouse, France
  • 5CESBIO, Université Paul-Sabatier, CNRS, CNES, IRD, INRAE, Toulouse, France.
  • 6Indian Institute of Science, Civil Engineering Department, Bangalore, India.
  • 7SAS, INRAE, Institut Agro, Rennes, France.

Mapping soil properties is becoming more and more challenging due to the increase in anthropogenic modification of the landscape, calling for new methods to identify these changes. A striking example of anthropogenic modifications of soil properties is the widespread practice in South India of applying large quantities of silt from dry river dams (or “tanks”) to agricultural fields. Whereas several studies have demonstrated the interest of tank silt for soil fertility, no assessment of the actual extent of this age-old traditional practice exists. Over pedological contexts characterized by Vertisol, Ferralsols and Chromic Luvisols in sub-humid and semi-arid Tropical climate, this practice is characterized by an application of black-colored tank silt providing from Vertisol, to red-colored soils such as Ferralsols. The objective of this work was to evaluate the usefulness of Sentinel-2 images for mapping tank silt applications, hypothesizing that observed changes in soil surface color can be a proxy for tank silt application.

We used data collected in a cultivated watershed (Berambadi, Karnataka state, South India) including 217 soil surface samples characterized in terms of Munsell color. We used two Sentinel-2 images acquired on February 2017 and April 2017. The surface soil color over each Sentinel-2 image was classified into two-class (“Black” and “Red” soils). A change of soil color from “Red” in February 2017 to “Black” in April 2017 was attributed to tank silt application. Soil color changes were analyzed accounting for possible surface soil moisture changes. The proposed methodology was based on a well-balanced Calibration data created from the initial imbalanced Calibration dataset thanks to the Synthetic Minority Over-sampling Technique (SMOTE) methodology, coupled to the Cost-Sensitive Classification And Regression Trees (Cost-Sensitive CART) algorithm. To estimate the uncertainties of i) the two-class classification at each date and ii) the change of soil color from “Red” to “Black”, a bootstrap procedure was used providing fifty two-class classifications for each Sentinel-2 image.

The results showed that 1) the CART method allowed to classify the “Red” and “Black” soil with overall accuracy around 0.81 and 0.76 from the Sentinel-2 image acquired on February and April 2017, respectively, 2) a tank silt application was identified over 97 fields with high confidence and over 107 fields with medium confidence, based on the bootstrap results and 3) the identified soil color changes are not related to a surface soil moisture change between both dates. With the actual availability of the Sentinel-2 and the past availability of the LANDSAT satellite imageries, this study may open a way toward a simple and accurate method for delivering tank silt application mapping and so to study and possibly quantify retroactively this farmer practice.

How to cite: Gomez, C., Subramanian, D., Lagacherie, P., Riotte, J., Ferrant, S., Sekhar, M., and Ruiz, L.: Mapping of tank silt application using Sentinel-2 images over the Berambadi catchment (India)., EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-8125, https://doi.org/10.5194/egusphere-egu21-8125, 2021.