Estimating soil fertility status in physically degraded land using GIS and remote sensing techniques in Chamarajanagar district, Karnataka, India

• Main Authors: Mohamed A.E. AbdelRahman, A. Natarajan, C.A. Srinivasamurthy, Rajendra Hegde
• Format: Article
• Language: English
• Published: Elsevier 2016-06-01
• Series: Egyptian Journal of Remote Sensing and Space Sciences
• Subjects: Bulk density; Physical degradation; Remote sensing; Soil erosion
• Online Access: http://www.sciencedirect.com/science/article/pii/S1110982315000721

Soil physical degradation is a major environmental problem throughout the world due to its negative impact on biomass and economic production. This study presented new ways of combining rapid soil analysis using GIS and remote sensing imagery to provide a precision mapping of soil physical condition indicators in the study area and producing fertility status using Geostatistical approach. Study has been carried out to map the areas with physical degradation using remotely sensed data from Indian Remote Sensing LISS III sensor. It was observed that the data enabled better delineation of small units of eroded areas. Satellite data have been used for qualitative assessment of areas, being subject to soil erosion. Soil erosion was found to be none or slight to very sever using visual interpretation of IRS data along with field survey method where soil erosion was found to be moderate to high using the RUSLE method. The eroded areas of degraded lands will be used as an input for planning reclamation and conservation programs in Chamarajanagar district of Karnataka. Soil compaction is a form of physical degradation resulting in densification and distortion of the soil where biological activity, porosity and permeability are reduced, strength is increased and soil structure partly destroyed. Compaction can reduce water infiltration capacity and increase erosion risk by accelerating run-off. The compaction process can be initiated by wheels, tracks, rollers or by the passage of animals. Some soils are naturally compacted, strongly cemented or have a thin topsoil layer on rock subsoil. Soils can vary from being sufficiently strong to resist all likely applied loads to being so weak that they are compacted by even light loads.