2017
DOI: 10.4172/2469-4134.1000213
|View full text |Cite
|
Sign up to set email alerts
|

Identification of Potential Groundwater Recharge Zones Using Remote Sensing and Geographical Information System in Amaravathy Basin

Abstract: Amaravathy river is one among the main tributaries of the river Cauvery and is surrounded by four districts viz., Coimbatore, Dindigul, Karur and Tirupur in Tamil Nadu. In Karur district 9 out of 15 blocks is over-exploited, 5 is semi-critical and one is under critical category. Coimbatore district has 6 blocks under over exploited category of the 12 blocks, 4 under semi-critical and 2 under safe category. While in Dindigul district out of the 14 blocks 11 is under exploited 2 is semi-critical and only one blo… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

5
18
2

Year Published

2019
2019
2023
2023

Publication Types

Select...
7
2
1

Relationship

0
10

Authors

Journals

citations
Cited by 18 publications
(25 citation statements)
references
References 3 publications
5
18
2
Order By: Relevance
“…Lineaments features (e.g., faults, fractures, cleavages) are usually more concentrated at the plate margins because boundaries between tectonic plates are made up of a system of faults [167]. Lineaments, weak zones in the landscape that facilitate the movement of groundwater, are an important theme for GWPZs mapping since they have considerable control over the movement of groundwater [168,169]. Fractures in rocks enhance their secondary porosity and permeability and thus increase the groundwater movement [76].…”
Section: Lineament Densitymentioning
confidence: 99%
“…Lineaments features (e.g., faults, fractures, cleavages) are usually more concentrated at the plate margins because boundaries between tectonic plates are made up of a system of faults [167]. Lineaments, weak zones in the landscape that facilitate the movement of groundwater, are an important theme for GWPZs mapping since they have considerable control over the movement of groundwater [168,169]. Fractures in rocks enhance their secondary porosity and permeability and thus increase the groundwater movement [76].…”
Section: Lineament Densitymentioning
confidence: 99%
“…Areas with gentle slope are relatively flat with area extent of 129.6 km 2 . These are favorable condition of the occurrence of groundwater potential because they influence high infiltration rate and therefore allowing more percolation of surface water into the subsurface as reported in Raviraj et al (2017).…”
Section: Slopementioning
confidence: 81%
“…MAR suitability studies are available across the globe, e.g. in India (Raviraj et al 2017), Australia (Hostetler 2007), Brazil (Shubo et al 2020), Spain (Escalante et al 2014), United States of America (Russo et al 2015), Jordan (Alraggad et al 2010), Portugal (Rahman et al 2012), and Tunisia (Chenini and Mammou 2010).…”
Section: Inroductionmentioning
confidence: 99%