Open Access

Mapping Soil Salinity Across Raised Mounds and Inter-Row Areas to Delineate Precision Irrigation Zones in a Salt-Affected Pomegranate Orchard

1 Agricultural University of Tirana, Faculty of Agriculture and Environment, Department of Horticulture and Landscape Architecture, Tirana, Albania
2 Agricultural University of Tirana, Faculty of Agriculture and Environment, Department of Environment and Natural Resource Management, Tirana, Albania
3 The University of Texas at Arlington, College of Science, Department of Mathematics, Arlington, Texas, United States
4 Texas A&M AgriLife Research, Temple Research and Extension Center, Temple, Texas, United States

Abstract

Raised mounds, drip irrigation, and plastic mulch are commonly used to improve the root zone conditions in orchards affected by salt. However, their success depends on how salt spreads between mounds, and inter-mounds, as well deeper soil layers. This study focuses on a 50-hectare section of a 100-hectare pomegranate (Punica granatum L.) orchard in the Karavasta coastal lowland of Albania. Proximal/remote sensing and digital elevation models were used to derive salinity indices and terrain attributes for initial stratification. A DualEM-1S electromagnetic induction mapping, Delta-T W.E.T. field measurements, and laboratory electrical-conductivity tests of 1:5 soil-water extracts were conducted. DualEM readings were calibrated separately for raised mounds and inter-mounds and a spatial detailed maps was developed using Empirical Bayesian Kriging and regression-kriging at depths of 0–30 and 0–100 cm. W.E.T. sensor measurements revealed a clear contrast between managed and native (structural) salinity areas. The median electrical conductivity (EC) was 237.5 mS m-1 on mounds and 862.0 mS m-1 in inter-rows (P=0.002). Soil moisture and temperature did not show significant differences. The cross-validation of EBK maps was high (R2=0.93-0.99; RMSE=22.6–73.1 mS m-1). For the inter-mounds areas 42 and 45% of the area were saline or extremely saline at both 0-30 and 0–100 cm depths. In contrast, for the mounds 100% were non-saline at 0–30 cm and 89% non-saline at 0–100 cm. These results show that raised mounds can reduce salt levels in the active root zone, but they do not eliminate deeper and lateral salt. The results indicate that a combination of depth-specific monitoring, different leaching strategies and spatially detailed maps are needed for precision management of the salinity in pomegranate orchards in the study area.

Keywords

How to Cite

KULLAJ, E., SEMA , X., MICI , E., HUQI, F., KRISTO , I., WINZELER , E., & ADHIKARI, K. (2026). Mapping Soil Salinity Across Raised Mounds and Inter-Row Areas to Delineate Precision Irrigation Zones in a Salt-Affected Pomegranate Orchard. MAS Journal of Applied Sciences, 11(3), 508–523. https://doi.org/10.5281/zenodo.21418501

References

πŸ“„ Allbed, A., Kumar, L., 2013. Soil salinity mapping and monitoring in arid and semi-arid regions using remote sensing technology: a review. Advances in Remote Sensing, 2(4): 373-385.
πŸ“„ Allen, R.G., Pereira, L.S., Raes, D., Smith, M., 1998. Crop evapotranspiration: Guidelines for computing crop water requirements (FAO Irrigation and Drainage Paper No. 56). Food and Agriculture Organization of the United Nations.
πŸ“„ Ayers, R.S., Westcot, D.W., 1985. Water quality for agriculture (FAO Irrigation and Drainage Paper No. 29, Rev. 1). Food and Agriculture Organization of the United Nations.
πŸ“„ Bhantana, P., Lazarovitch, N., 2010. Evapotranspiration, crop coefficient and growth of two young pomegranate (Punica granatum L.) varieties under salt stress. Agricultural Water Management, 97(5): 715-722.
πŸ“„ Corwin, D.L., Lesch, S.M., 2005. Apparent soil electrical conductivity measurements in agriculture. Computers and Electronics in Agriculture, 46(1-3): 11-43.