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Surface correlation functions capture information about the spatial distribution of interfaces in the material and are based upon the surface indicator function ( {chi}_{alpha}left({overrightarrow{r}}_1right) ), which is nonzero only at the interface of phase α (Torquato 2002; Fullwood et al. 2010).
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Landscape Function Analysis (LFA) is a monitoring procedure that assesses the degradation of landscapes, as brought about by human, animal and natural activities, through rapidly assessing certain soil surface indicators which indicate the biophysical functionality of the system.
The goal of RS is to locate surface indicators, which may indicate suitable traps at depth, lineament mapping, thrust zone mapping, micro-seepage maps of hydrocarbons, and stain maps of hydrocarbons.
The LFA soil surface indicators, and the related NC (Nutrient Cycling) and IR (Infiltration/Runoff) indices were assessed in the observed ecological patches and inter-patches, for a total number of 157 microsites.
The landscape function analysis (LFA), developed in Australia by David Tongway (CSIRO), uses soil surface indicators to assess the condition of a given ecosystem by producing three numerical indices (stability, infiltration and nutrient cycling) reflecting the status of basic soil functions.
LFA uses soil surface indicators to assess the condition of a given ecosystem by producing three numerical indices (stability, infiltration and nutrient cycling) reflecting the status of basic soil functions.
LFA assesses fine-scale landscape patchiness (entailing resource conserving potential and erosion resistance) and 11 soil surface indicators to produce three main LFA parameters (stability, infiltration, and nutrient cycling), which indicates how well a system is functioning in terms of fine-scale biophysical soil processes and characteristics.
Hence, the surficial features can be used as surface indicators to the sub-surface fracturing and weathering which are essential for high yielding productive aquifers in hard rocks.
We use remote sensing data from a variety of satellite and airborne instruments to characterize mineral and thermal properties as surface indicators of geothermal resources in Nevada.
In order to detect disturbances in these areas we developed an automated processing chain for the calculation and analysis of robust trends of key land surface indicators based on the full record of available Landsat TM, ETM +, and OLI data.
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