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Extraction of groundwater is through open dug wells (<10 m depth), filter point wells (10 25 m depth) and tube wells (30 60 m depth).
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Two hundred liters of seawater was collected from the South Adriatic Sea (41°36'N; 17°22'E) at 1,000 m depth (200 m from the bottom) and sequentially filtered through Millipore 20, 5, and 0.22 µm-pore-size filters (fig. 1).
We estimated there were 9.7 × 1012 mussels (mean = 3402.9/m2) in the Lake Ontario nearshore totalling 1.2 × 105 mT of mussel tissue which could filter the entire Lake Ontario nearshore volume (0 20 m depth = 30.9 km3) in roughly 1 to 7 days.
Field data included >5500 Chl- a observations, which were reduced to 1947 after filtering for surface samples (0 to 2 m depth) and satellite overpass time (±3 h).
The correspondent Karous Hjelt pseudosection filtering confirms the moderately high conductivity which extends below 50 m depth.
In the Karous Hjelt filtering pseudo-section, the extent of the fractured identified is below 40 m depth, this can either be a localized zone of fracture or thick clayey materials in the region.
Cenozoic sediment extends to 2800 3000 m depth.
(E) Height (m) Depth of borehole (m) Static Disp.
Table 3 Depth of tubewell in As-contaminated areas in the Ghaghara Basin, Uttar Pradesh Study areas Depth 10 20 m Depth 21 45 m Depth 46 60 m Max.
The temperature rises from 34.1 °C at 30 m depth to 37.5 at 255 m depth.
Different areas between 300 and 1200 m depth were surveyed.
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