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 ...

26.03.2013 Views

Inset C of Figure 35 is the same data set (f110512t01p00r07) utilized with the imagery derived BSC endmembers in Figure 35, inset A and B. Inset D of Figure 35 is the f110512t01p00r08 data set result using the same endmember as in inset C for a repeatability test. While the healthy BSC result using the imagery derived endmember (Figure 35, inset A) was not repeatable using any of the ASD collected BSC endmembers, the disturbed BSC endmember results did appear to be replicable to the imagery derived ones with 7–11% providing the best result range in the f110512t01p00r07 data set. Similar results for the f110512t01p00r08 data set of 5–9% yielding the best range for the disturbed BSC endmember were obtained. Slightly different results are expected as the resolution of the two images is close but not exact. Figure 35, inset D shows the result for the f110512t01p00r08 data set. BSC results are, however, somewhat inconclusive as they appear in high concentrations in areas that other endmembers have also been detected, particularly the adjacent to tread endmember. The distribution of the BSC pixels did look slightly different, and there is no reason they could not occur in the same location, as BSCs tend to also cause soil to become more consolidated via their growth method and are known to be a stabilizing mechanism of slope material (Johnston, 1997). 68

A B C D Figure 35. A shows results using BSC endmember 2 derived from the imagery. B and C show areas suspected to contain BSCs using endmember 3 and the Mazourka Canyon disturbed BSCs in green. While B and C show similar results, the results of A were not repeatable with the collected BSC endmembers. D shows the results from the repeatability test using the same endmember as in C. In all cases, the range was between 9–11% for target material, with higher values of 15–30% associated with possible bare to nearly bare soil. 69

Inset C of Figure 35 is <strong>the</strong> same data set (f110512t01p00r07) utilized with <strong>the</strong> imagery<br />

derived BSC endmembers in Figure 35, inset A and B. Inset D of Figure 35 is <strong>the</strong><br />

f110512t01p00r08 data set result using <strong>the</strong> same endmember as in inset C <strong>for</strong> a<br />

repeatability test. While <strong>the</strong> healthy BSC result using <strong>the</strong> imagery derived endmember<br />

(Figure 35, inset A) was not repeatable using any of <strong>the</strong> ASD collected BSC<br />

endmembers, <strong>the</strong> disturbed BSC endmember results did appear <strong>to</strong> be replicable <strong>to</strong> <strong>the</strong><br />

imagery derived ones with 7–11% providing <strong>the</strong> best result range in <strong>the</strong><br />

f110512t01p00r07 data set. Similar results <strong>for</strong> <strong>the</strong> f110512t01p00r08 data set of 5–9%<br />

yielding <strong>the</strong> best range <strong>for</strong> <strong>the</strong> disturbed BSC endmember were obtained.<br />

Slightly different results are expected as <strong>the</strong> resolution of <strong>the</strong> two images is close<br />

but not exact. Figure 35, inset D shows <strong>the</strong> result <strong>for</strong> <strong>the</strong> f110512t01p00r08 data set.<br />

BSC results are, however, somewhat inconclusive as <strong>the</strong>y appear in high concentrations<br />

in areas that o<strong>the</strong>r endmembers have also been detected, particularly <strong>the</strong> adjacent <strong>to</strong> tread<br />

endmember. The distribution of <strong>the</strong> BSC pixels did look slightly different, and <strong>the</strong>re is<br />

no reason <strong>the</strong>y could not occur in <strong>the</strong> same location, as BSCs tend <strong>to</strong> also cause soil <strong>to</strong><br />

become more consolidated via <strong>the</strong>ir growth method and are known <strong>to</strong> be a stabilizing<br />

mechanism of slope material (Johns<strong>to</strong>n, 1997).<br />

68

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