Spectral Unmixing Applied to Desert Soils for the - Naval ...

Spectral Unmixing Applied to Desert Soils for the - Naval ... Spectral Unmixing Applied to Desert Soils for the - Naval ...

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Figure 9. The above figure is a map of world soil types and their distribution adapted from the http://www.cals.uidaho.edu/soilorders/i/worldorders.jpg (2012). Notice that the primary soil types associated with the arid regions in Figure 7 are Aridisols (orange), and Entisols (pink) to some extent. B. CHEMICAL AND BIOLOGICAL SOIL COMPONENTS 1. Soils Aridisols are the predominant soil type associated with the desert environment (Whitford, 2002). Figure 9 illustrates different soils throughout the world along with their respective regions, and Figure 10 shows the percentage distribution of aridosols in the United States. Aridosols are CaCO3 containing soils generally found in arid regions that experience some subsurface horizon development. Characteristically, these soils are dry through most of the year with limited leaching (Balba, 1995; Whitford, 2002). Subsurface horizons have accumulations of clays, calcium carbonate, silica salts, and gypsum in some cases, though gypsum and calcium carbonate tend to leach from soils in most climate types (Balba, 1995). The properties of the subsurface soil horizons are important to know because variability in soil materials is detectable through Imaging Spectrometry (Clark, 1999; Kruse et al., 2000) and their presence may tell something about activities in the area (Webb et al., 2009). Other soil types also found 20

in desert regions include argids, orthids, mollisols, entisols, and shrink swell soils also known as cracking clays (Whitford, 2002). The structure and processes that occur within desert regions can be directly linked to soil properties and therefore make it possible to link changes in those properties to alterations in ecosystem functions (Prose, 1985; Whitford, 2002). Because soils are a product of geology, geomorphology, and climate it is possible to make inferences as to what types of soil components may be present based on local geologic, geomorphologic and climatologic information (Whitford, 2002; Lammers, 1991). These similarities should also allow for use of endmembers from a geographically different yet geologically similar area to be used to study surface disturbances in different arid regions of the world (Whitford, 2002; Lammers, 1991). Soils also play a key role in nutrient availability and nutrient cycling critical to survival of biologic soil components such as cryptobiotic soil crusts (BSCs) (Whitford, 2002; Bowker et al., 2005). It is a reasonable assumption that biological soil components exhibiting signs of stress can yield information (Smith et al., 2004) on anthropogenic activities causing surface disturbances; because these impacts change ecosystem functions and nutrient delivery systems (Bowker et al., 2005; Evans et al., 1999; Prose, 1985) within and around an area (Webb et al., 2009). 21

Figure 9. The above figure is a map of world soil types and <strong>the</strong>ir distribution adapted<br />

from <strong>the</strong> http://www.cals.uidaho.edu/soilorders/i/worldorders.jpg (2012).<br />

Notice that <strong>the</strong> primary soil types associated with <strong>the</strong> arid regions in Figure<br />

7 are Aridisols (orange), and Entisols (pink) <strong>to</strong> some extent.<br />

B. CHEMICAL AND BIOLOGICAL SOIL COMPONENTS<br />

1. <strong>Soils</strong><br />

Aridisols are <strong>the</strong> predominant soil type associated with <strong>the</strong> desert environment<br />

(Whit<strong>for</strong>d, 2002). Figure 9 illustrates different soils throughout <strong>the</strong> world along with <strong>the</strong>ir<br />

respective regions, and Figure 10 shows <strong>the</strong> percentage distribution of aridosols in <strong>the</strong><br />

United States. Aridosols are CaCO3 containing soils generally found in arid regions that<br />

experience some subsurface horizon development. Characteristically, <strong>the</strong>se soils are dry<br />

through most of <strong>the</strong> year with limited leaching (Balba, 1995; Whit<strong>for</strong>d, 2002).<br />

Subsurface horizons have accumulations of clays, calcium carbonate, silica salts,<br />

and gypsum in some cases, though gypsum and calcium carbonate tend <strong>to</strong> leach from<br />

soils in most climate types (Balba, 1995). The properties of <strong>the</strong> subsurface soil horizons<br />

are important <strong>to</strong> know because variability in soil materials is detectable through Imaging<br />

Spectrometry (Clark, 1999; Kruse et al., 2000) and <strong>the</strong>ir presence may<br />

tell something about activities in <strong>the</strong> area (Webb et al., 2009). O<strong>the</strong>r soil types also found<br />

20

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