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Stream/Area:
-
Subject:
-
Paper ID:
IJSREM67125
Volume:
10 |
9 |
Sep 2026
Pages:
1-5
Publication Frequency:
Monthly (12 issues per year)
License:International Journal of Scientific Research in Engineering and Management follows the Creative Commons Attribution 4.0 (CC BY 4.0) License, allowing free use and distribution with proper attribution.

Department of Industries and Earth sciences
Tamil University
Professor and Head, Department of Industries and Earth sciences,
Tamil University.
The irrigation canal network systems have contributed to the availability of water not only for agriculture but also for domestic use by urban and rural households. Irrigation canal seepage and infiltration provide an important contribution to groundwater recharge. This saves a substantial amount of water that can be used to extend the irrigation area so more people can benefit from the available irrigation water. However, in the currently irrigated areas lining will have impacts by lowering groundwater levels due to a reduction in percolation from canals. This percolation contributes to the recharge of underground water in both shallow and deep bore well used by the people to obtain water for drinking and agriculture purpose during alternate season of six months in a year. In this study, the positive effects of subsurface conditions on recharge zones by infiltration from Grand Anicut canals are evaluated. The soil, geomorphology and geological data along with slope of the canal command Area in Thanjavur and Pudukottai districts are used to identify the infiltration zones influenced by Grand Anicut canal and branch canals. The analysis thus carried out has revealed that the areal extent of zones in the canal irrigated area with poor, moderate, good and excellent infiltration process zones are 30.99 sq.km, 1191.16 sq.km, 2325.87 sq.km and 327.50 sq.km respectively.
KEYWORDS
In order to understand the active infiltration zone in the study area, thematic layers such as soil, geology, slope, geomorphology and canal density which improve the ground water storages are considered. All the above said layers were overlaid and analysed using ArcGIS software. For each of the above parameters suitable weightage values were assigned based on their ability to store water. As soil is concerned sand, loamy sand was assigned the maximum weightage value followed by sandy loam, Sandy clay loam, clay loam and clay in the decreasing order. Areas with less than 4% slope were assigned higher weightage and progressively lower weightages were assigned to the slope classes of 4-8%, 8-12%, 12-16% and over 16%. Among the various landforms of the study area maximum weightage value was assigned for alluvial plains, flood plain, coastal plain followed by Deltaic plain, Pediment, Lateritic and hill in the decreasing order. After assigning weightage values for various classes of each of these parameters, these thematic layers were integrated and the resultant map was re-classed showing zones of infiltration progressive area. The analysis thus carried out has revealed that the areal extent of zones in the canal irrigated area with poor, moderate, good and excellent infiltration process zones are 30.99 sq.km, 1191.16 sq.km, 2325.87 sq.km and 327.50 sq.km respectively. In general, it is found that in the study area, areas with low, moderate, high and very high infiltration areas are spread towards the southern and north eastern parts, covering about 51.01 per cent and 4.89 per cent of Thanjavur and Pudukkottai District respectively.
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Publication Date
9/5/2026
Peer Review Type
Double-Blind Peer Review
Review Rounds: 2
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