EGU26-8713, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-8713
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 05 May, 09:05–09:15 (CEST)
 
Room B
Nitrate transport process driven by groundwater-surface water interactions in the Langat River Basin, Malaysia
Mayu Ogiya1, Koichi Sakakibara2, Yusra Shabir3, Noorain Mohd Isa3, Takashi Nakamura4, Maki Tsujimura5, and Siti Nurhidayu3
Mayu Ogiya et al.
  • 1Graduate School of Science and Technology, Shinshu University, Matsumoto, Japan
  • 2Faculty of Science, Shinshu University, Matsumoto, Japan
  • 3Faculty of Forestry and Environment, Universiti Putra Malaysia, Serdang, Malaysia
  • 4Interdisciplinary Center for River Basin Environment, University of Yamanashi, Kofu, Japan
  • 5Institute of Life and Environmental Science, University of Tsukuba, Tsukuba, Japan

Rapid population growth and agricultural expansion have increased nitrogen input in tropical regions, increasing the risk of nitrate contamination of water resources in tropical catchments. Most catchment-scale studies of nitrate contamination have focused on either surface water or groundwater. However, because nitrate is highly soluble and mobile, investigating interactions between groundwater and surface water systems is essential for tracking nitrate contamination. In this study, a multi-isotope tracer approach (δ2H-H2O, δ18O-H2O, δ15N-NO3-, and δ18O-NO3-) was applied to investigate three-dimensional nitrate transport processes through groundwater–surface water interactions. The study area is the Langat River Basin (2350 km2), in Selangor, Malaysia, which includes diverse land uses such as tropical rainforest, urban areas, peatlands, and oil palm plantations. Water sampling was carried out in wet and dry seasons at a spatial network of 44 groundwater, 17 river water, and 4 irrigation drainage channel sites. Results in the dry season showed that the mean nitrate concentration in river water was 13.4 mg/L (range 1.38 to 96.2 mg/L), while much lower concentrations were observed in groundwater (0.69 mg/L) and irrigation drainage (0.80 mg/L). Spatial stable water isotope compositions showed that groundwater near the river had similar signatures to river water, whereas groundwater farther from the river was more depleted, indicating river water recharge into the aquifer is important in floodplain areas. Nitrate isotope data revealed that sewage and manure were the dominant nitrate sources in the floodplain, affecting both river water and groundwater. In contrast, downstream areas dominated by oil palm plantations showed nitrate sources derived from fertilizer were dominant. These results demonstrate that land use and groundwater–surface water interactions control nitrate sources and transport pathways, emphasizing the importance of integrated water flow for assessing nitrate pollution in tropical catchments.

How to cite: Ogiya, M., Sakakibara, K., Shabir, Y., Mohd Isa, N., Nakamura, T., Tsujimura, M., and Nurhidayu, S.: Nitrate transport process driven by groundwater-surface water interactions in the Langat River Basin, Malaysia, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-8713, https://doi.org/10.5194/egusphere-egu26-8713, 2026.