Percolation near Hingana
pt-3 · 21.4065, 79.7094 · Tumsar taluka · PIN 441912
Contributing catchment 8.07 km² · at a 3 m bund it impounds 158 thousand m³ over 17 ha · design monsoon yield 2,996 thousand m³ · soil HSG-C (clay 40%).
In plain words
A percolation-tank site near Hingana (Tumsar) on lighter HSG-C soil, where the sensors track the seasonal fill well (correlation 0.74). The blocker is land: six buildings fall inside the 3 m footprint, the nearest only about 59 m away.
What to build
Survey the six structures — and test whether a lower bund clears them — before committing; the recharge case is otherwise sound.
Why here
HSG-C soil makes this a genuine recharge site (around a third of storage percolates) and the flow is well witnessed; the only real question is whether the six nearby structures can be avoided or the bund lowered.
How
Cadastral + ground check of the six structures; an area-capacity trade-off for a lower bund that keeps useful storage while clearing the buildings.
The delta — now vs after
Clear the land and Hingana gains a recharge tank; if the structures cannot be avoided, a lower design or a drop.
What it delivers · indicative
Indicative benefit at a 3 m bund (DEM area-capacity at 3 m bund) under standard norms (irrigation ~5 TCM/ha; drinking 150 lpcd). Recharge is limited on HSG-D clay (35% of storage). Actual yield varies with monsoon reliability, seepage and siltation.
Incremental over today · the net-new gain, from the 4-year record
≈ 158 thousand m³ of net-new water · 32 ha irrigable · 2,873 drinking person-years.
full design storage — no structure holds water here today.
Why this site
Sited where soil is lighter (HSG-C) or fractures raise infiltration — a percolation tank turns runoff into recharge rather than surface storage.
Seasonal water extent · dual-sensor
Radar (S1, 48 passes) fills the monsoon gap that cloud hides from optical (S2, 38 scenes). Radar peak vs summer low: 1.7 → 0 ha, a 1.6 ha annual draw-down — the storage renovation recovers.
Area-capacity (DEM, 30 m) · gross storage by bund height
Cross-witness & confidence — independent corroboration
Two sensors track together
Optical (S2) and radar (S1) rise and fall together with correlation r = 0.74 across 38 paired months. Absolute extents match 0% — they differ by sensor physics on a flowing nala, so the shared rhythm is the witness, not the magnitude.
Nala flow (new-build site)
No existing lake here — expected for a new structure. Sensors confirm a monsoon flow pulse in the nala; nearest mapped lake is 4,784 m away.
Land acquisition (submergence)
A 3 m bund would submerge 17 ha — the land to be acquired. Cost & consent scale with this.
Displacement witness — real building footprints
Several structures — survey neededIn the submergence footprint
6
buildings within the 231 m design-submergence radius (17 ha pond at 3 m).
Nearest structure
59 m
to the closest mapped building.
Within 500 m
33
buildings in the influence ring.
Overture Maps buildings 2026-05-20.0 (union of OSM / Google Open Buildings / Microsoft / Esri), Bhandara admin_code=506. A desktop displacement screen — precedes, not replaces, cadastral (7/12) verification.
Reconnaissance context & access — Ola + Google Places
Nearest habitation
Hingana
153 m away · Tumsar taluka · PIN 441912
Nearest landmark
Mitewani.P.H Railway Station
Schools within 2 km
3
nearest 696 m
Health within 2 km
0
Google Places (New) searchNearby + Ola Maps Places nearbysearch · reconnaissance-grade. Independent witness to the buildings displacement layer — dense amenities near a site corroborate high displacement. Does not replace cadastral 7/12 records, geotechnical bores or a level survey.
Human pressure — land-cover change (2022 → 2026)
Stable land coverVegetation (NDVI) change
+0.032
34 ha lost · 116 ha gained over 1,856 ha land
Built-up (NDBI) change
15.9 ha
new built-up / bare (construction proxy)
Window
2022-11..2023-02 (8 scenes)
→ 2025-11..2026-02 (8 scenes)
Sentinel-2 L2A dry-season MEDIAN composites (2022-23 vs 2025-26), water-masked; NDVI+NDBI change screen — not cadastral or DEM cut/fill
DPR-grade desktop hydrology from Copernicus GLO-30 (30 m) + ISRIC SoilGrids + ESA WorldCover; water extent from Sentinel-2 L2A MNDWI (optical) and Sentinel-1 GRD VV radiometrically calibrated to σ⁰ (DN²/sigmaNought² from the product calibration LUT, GCP thin-plate-spline geocoded, open water at σ⁰ < −17 dB; thermal-noise floor not subtracted). A desktop assessment that precedes — not replaces — the statutory ground & geotechnical survey.