Sinnar Taluka Overview
and preparation for field trip
Pooja Prasad (Ph D scholar) 22/8/2017
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Sinnar Taluka Overview and preparation for field trip Pooja Prasad - - PowerPoint PPT Presentation
Sinnar Taluka Overview and preparation for field trip Pooja Prasad (Ph D scholar) 22/8/2017 1 Topics Overview of Sinnar taluka Geo-morphology, cropping patterns Diversion based irrigation (DBI) system on Devnadi Konambe dam
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Devnadi Jam nadi Mahalunge Godavari
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9 Crop type Hectares under cultivation (2014-15) % of cultivable land Kharif pulses 1,182 1% Kharif cereal 30,617 31% Kharif onion 4,558 5% Rabi cereal 8,330 8% Rabi harbhara 4,650 5% Rabi onion 5,607 6% Sugarcane 532 1% Cotton 1,583 2% Oilseeds 15,990 16% Other Vegetables 7,084 7% Fruits 4,906 5% Gross sown area 85,038 87% Total Cultivable land 98,226 100%
Source: Sinnar block Agriculture dept
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Year Cultivable area (Ha) Orchards and sugarcane area (Ha) Kharif cropped area ha Rabi cropped area ha Sugarcan e, fruits TCM Kharif CWR TCM Rabi CWR TCM Total crop water requirement (TCM) Total rain TCM Crop water requirement as fraction of rainfall 2014-15 98,226 5,438 61,823 18,587 70,573 246,807 86,803 404,182 523,679 0.77 2015-16 98,226 4,906 58,443 22,449 58,872 236,040 102,482 397,393 552,444 0.72 2016-17 98,226 5,378 66,692 29,224 69,256 303,501 136,079 508,836 882,784 0.58
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gains offset the losses in the region?
across the region?
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Source: Anish Holla MTP Direct command area
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Structural decomposition
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Domain Decomposition-By surface flows
p1 p2 p3 p5 p4 surface water A1 A2 A3 A4 A5 salinity ingress water table q W(q) W(p2)
The watershed W (x) of a point x is W (x) = {all points y from where surface water flows to x}. For any two points x, y either W (x) ⊆ W (y) or W (x) ∩ W (y) is a thin set. Decomposition of Domain into disjoint union of watersheds.
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The Watershed
source:albanywater.org
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Thane Watersheds
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Ridgelines, flowlines, drainlines
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How does water flow on a slope?
flow of water surface normal iso−height gravity water drop
Elevation e(x, y), then flow direction is ∇e = (− ∂e
∂x , − ∂e ∂y ) and
normal is [− ∂e
∂x , − ∂e ∂y , 1]. Direction of steepest descent.
Enough to check when e(x, y) = ax + by + c
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The Siddhagad Area
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Its Contour Map
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Contours and contour-flows
100 95 gentle plain ridge slope valley narrow convergence divergence 90 85
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A sample Topo-sheet
Gudwanwadi reservoir.
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A close-up
Notice (i) the point data which is used to build the curves, and (ii) the drainage lines.
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Decomposition
watershed(p)=all points from where water flows to p. Either watershed(p) is disjoint with watershed (q) Or watershed(p) ⊆ watershed (q) This may be used to decompose a terrain into disjoint watersheds of appropriate sizes.
p1 p2 W1 W2 W3 W3 W3 p3 W3 ridges p4 W4
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