Sentence examples for groundwater profile from inspiring English sources

Trace fossils also relate information about soil formation and development, the type of biologic activity, topography of the landscape and its relationship to groundwater profile, and duration of time that a body of sediment has been stable at the surface with respect to sedimentation rate.

The groundwater profile at NS21 indicates a rapid increase in As concentrations to a maximum of 920 μg/L at 6 m depth.

The general shape of such groundwater profiles shows some similarity to rainwater, indicating that such groundwater is of meteoric origin and affected by continental processes.

Thus, trace fossils in the continental realm are proxies for: (1) biodiversity in terrestrial and aquatic palaeoenvironments not recorded by body fossils; (2) above- and below-ground palaeoecological associations; (3) palaeosol formation; (4) palaeohydrology and palaeo-groundwater profiles; and (5) seasonal and annual palaeoclimate indicators and climate change.

Based upon groundwater physicochemical profile, three clusters have been identified and characterised by source type (borehole or hand-dug well) and local geological setting.

To overcome the influence of specific warm or cold years we introduced the computation of an annual averaged groundwater temperature profile.

The highest dissolved As concentration of 27 μg/L was measured in groundwater from profile NS19 collected beneath an 18-m-thick layer of fine silt and clay.

Landfill leachate, surface water, groundwater and soil profile samples were collected from a MSW landfill area in Wuhan, China.

An infiltration coefficient is introduced in the network architecture apart from antecedent rainfall, slope profile, groundwater level and shear strength of soil.

There was no significant difference in nitrate concentrations in the groundwater or soil profile with and without a cover crop in either no-tillage or conventional tillage.

Because of their small size (i.e., 25 90 nm), low attachment to particles at typical soil pH (Gupta et al. 2009), and large numbers shed in the stool of infected individuals, viruses have great potential to travel downward through the soil profile, reach groundwater, and move with groundwater flow to drinking water wells.