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The range is extremely wide; the seepage rate through clean gravel is 10,000 times that through sand, 10,000,000 times that through silt, and 100,000,000 times that through dense clay.
Seepage measurements were conducted at 17 sites (mean seepage rate = 0.8 cm/day).
Lower seepage rate was observed in seepage meter 3 fixed close to the coast and higher seepage rate was observed in seepage meter 1 fixed at distance from the coast.
Open image in new window Fig. 5 Comparison of seepage rate and physicochemical parameters for the seepage meter 1.
In this paper, an innovative Distributed Temperature System for measuring seepage rate, called S-DTS, is introduced.
A test is designed and carried out to validate the feasibility of this technology in measuring the seepage rate quantitatively.
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The measured seepage rates are noted in the table.
Measurements of groundwater seepage rates are often made using manual seepage meters.
These seepage rates are comparable with the seepage rates for the aquaculture ponds (Teichert-Coddington et al. 1989; Weisburd and Laws 1998).
These seepage rates are at the low end of the range of seepage rates from recent performance assessment (PA) calculations, confirming the conservative nature of the performance assessment.
Significant temporal and (particularly) spatial variabilities were observed in both measured infiltration and seepage rates.
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