28.02.2018 Views

Revitalization of Rivers in India Draft Policy - Isha Guru Jaggi Vasudev

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

<strong>Revitalization</strong> <strong>of</strong> <strong>Rivers</strong> In <strong>India</strong><br />

<strong>Draft</strong> <strong>Policy</strong> Recommendation<br />

stream network, slope/contour, forest legal boundaries, settlement<br />

locations and village boundaries. The ma<strong>in</strong> criterion that will be used to<br />

differentiate the various land uses <strong>in</strong> the study area <strong>in</strong> these type groups is<br />

their similarity, such as <strong>in</strong> the height and extent <strong>of</strong> forest canopy <strong>in</strong> the case<br />

<strong>of</strong> vegetative covers, and the predom<strong>in</strong>ance <strong>of</strong> a paved, impervious surface<br />

devoid <strong>of</strong> vegetation <strong>in</strong> the case <strong>of</strong> commercial and rural residential zones.<br />

The percentage <strong>of</strong> land use with<strong>in</strong> the proposed area will be calculated and<br />

grouped <strong>in</strong> each bas<strong>in</strong> which can be determ<strong>in</strong>ed from the prepared data set<br />

(Map layers). F<strong>in</strong>ally, field validation will be conducted with processed data<br />

base.<br />

3.2. Geology – To understand the geology <strong>of</strong> the area <strong>in</strong>clud<strong>in</strong>g rock formations<br />

and types <strong>of</strong> rock, structural aspects will be studied through field<br />

exam<strong>in</strong>ations.<br />

3.3. Soil Study – Physical and chemical characteristics, types <strong>of</strong> soil, and<br />

depth pr<strong>of</strong>ile data will be collected from the exist<strong>in</strong>g source for further<br />

understand<strong>in</strong>g and analysis.<br />

3.4. Ra<strong>in</strong>fall – Ra<strong>in</strong>fall data will be collected from the exist<strong>in</strong>g data source for the<br />

proposed region to understand the ra<strong>in</strong> pattern.<br />

3.5. Streamflow – Flow rate data will be collected for the past few decades to<br />

understand the exist<strong>in</strong>g scenario.<br />

3.6. Evapotranspiration (ET) – If the ET data is not available then it will be<br />

calculated from collected ra<strong>in</strong>fall and streamflow, etc. The mass-balance<br />

approach <strong>of</strong> Giusti (1978) will be used to estimate evapotranspiration<br />

(ET) with<strong>in</strong> the study area. In this approach, ET can be considered to be<br />

the difference between ra<strong>in</strong>fall and run<strong>of</strong>f (ET = P–RO) where P is the<br />

bas<strong>in</strong> average precipitation and RO is run<strong>of</strong>f. Accord<strong>in</strong>g to Giusti (1978),<br />

ET <strong>in</strong>creases until a threshold <strong>in</strong> ra<strong>in</strong>fall is reached, beyond which it<br />

progressively decreases with further <strong>in</strong>creases <strong>in</strong> ra<strong>in</strong>fall. The ra<strong>in</strong>fall and<br />

streamflow data will be used to estimate evapotranspiration.<br />

3.7. Groundwater – Available groundwater data will be used to understand the<br />

current condition <strong>of</strong> the bas<strong>in</strong>.<br />

Annexures<br />

291

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!