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The mobility was determined as a function of hydrologic conditions and solution chemistry using column breakthrough curves and numerical modeling.
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The term "groundwater productivity (potentiality)" denotes the amount of groundwater available in an area and it is a function of several hydrologic and hydrogeological factors (Jha et al. 2010).
Potential infiltration sites are assessed as a function of two primary topics: hydrologic and soil conditions.
The accrual (colonization plus growth) of benthic algal biomass is a function of nutrients, light, and temperature, whereas hydrologic stability and grazing control the process of biomass loss (Biggs 1996a).
However, major efforts focused on developing complex equations to describe hydrologic processes as a function of vegetation structure at the plot level have not been accompanied by corresponding attempts to adequately extrapolate these metrics over the wider landscape in order to parameterize fully-distributed models.
Understanding how these variables change as a function of solar radiation, rainfall, and biotic and hydrologic factors will advance our ability to develop mechanistic models for watershed management and set pollutant discharge limits.
Change in total sediment load is not only a function of the area conserved but also a function of the hydrologic responses of the watershed.
Increased marginal attenuation of the hydrologic response of a watershed is primarily a function of the marginal change in conserved area of a watershed.
The independent calibration of the assembled hydrologic models revealed (i) important variations of model predictions; and (ii) from average to important variations of effective parameter values, as a function of the different DEMs.
At the Calhoun CZO, interfluve order and corresponding erosion and intra-critical zone regimes inform us about the evolution and functioning of hydrologic, geomorphologic, biogeochemical, and biotic systems; CZ response to historic land use change; and the contemporary functioning and management of the CZ.
The distribution of stable isotopes of water within the soil plant atmosphere continuum is indicative of a range of hydrologic processes and plant functions.
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