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Mud sediments (depth 5 cm; salinity 260 ‰ & pH 10.5) was collected from the condenser pond of the solar salt works of Kovalam, Kanyakumari, Tamilnadu, India (8°05′04.35″N 77°31′17.07″E) during the summer season of May 2013.
However, anomalies can be observed in this trend due to geological formations, groundwater extraction amount, size and type of sediments, depth of groundwater and, interactions between aquifer systems in the area.
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The Late Cretaceous sediments depths of the Dorado North, Dorado and Barracuda exploration wells are 3010 3622, 2850 3288 and 3440 4741 m, respectively (Fig. 2).
The Paleogene sediments depths of the Dorado North, Dorado and Barracuda exploration wells are 2200 3010, 2150 2850 and 2340 3440 m, respectively (Fig. 2).
The density function describes the joint probabilities of the following parameters: the anaerobic dechlorination rate constant, the volatilization rate constant, the aerobic biodegradation rate constant, the sedimentation rate, and the contaminated sediment depth.
We found that N2 fixation was widespread, yet heterogeneously distributed with sediment depth at all sites.
The importance of the higher frequencies decreases with increasing sediment depth.
Sediment depth and particle size had significant effects on a variety of water parameter measures throughout the experiment.
The effects of incubation temperature (10, 20, 30 and 50 °C) and sediment depth (0 2, 4 6 and 8 10 cm) were investigated.
At −10 cm sediment depth, pore water salinity ranged from 6 to 24 in less than 1 m horizontally.
TIFs can be used for remediation of acid mine drainage (AMD), however, as sediment depth increases, Fe(inI)-reduction in anoxic subsurface areas may compromise treatment effectiveness.
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