SCHRIFTENREIHE Institut für Pflanzenernährung und Bodenkunde ...
SCHRIFTENREIHE Institut für Pflanzenernährung und Bodenkunde ...
SCHRIFTENREIHE Institut für Pflanzenernährung und Bodenkunde ...
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Chapter 3 Factors controlling spatio-temporal variability of soil moisture using multivariate geostatistics<br />
water redistribution are scale-dependent. Therefore, it is critical to define the<br />
spatial scale of a simulation model when devising a sampling scheme.<br />
Table 3.6. Structural variation contributions of each component to the total variation (%) at<br />
different spatial scales for different grazing intensities<br />
Treat- Scale Soil Plant<br />
ment<br />
Moisture<br />
Sand SOC BD VC AGB<br />
UG79 Nugget 73% 0% 62% 62% 93% 56%<br />
Short 7% 100% 0% 0% 0% 44%<br />
Long 20% 0% 38% 38% 7% 0%<br />
UG99<br />
WG<br />
CG<br />
HG<br />
Nugget 31% 0% 20% 31% 69% 72%<br />
Short 69% 3% 80% 69% 0% 0%<br />
Long 0% 97% 0% 0% 31% 28%<br />
Nugget 82% 0% 21% 14% 33% 0%<br />
Short 18% 0% 0% 0% 67% 0%<br />
Long 0% 100% 79% 86% 0% 100%<br />
Nugget 39% 0% 65% 44% 0% 22%<br />
Short 0% 0% 6% 56% 0% 0%<br />
Long 61% 100% 29% 0% 100% 78%<br />
Nugget 30% 8% 51% 84% 67% 61%<br />
Short 34% 39% 49% 16% 33% 39%<br />
Long 37% 53% 0% 0% 0% 0%<br />
Sand: sand content (%); SOC: soil organic carbon (g kg -1 ); BD: bulk density (g cm -3 ); VC:<br />
vegetation coverage (%); AGB: above gro<strong>und</strong> biomass (g m -2 ).<br />
The structural variation contributions of each component to the total variation<br />
are shown in Table 6. The variation of soil moisture was dominated by nugget<br />
effects in UG 79 and WG, the short-range scale component in UG 99, long-range<br />
scale component in CG, and averaged random, short- and long-range scale<br />
components in HG. As fo<strong>und</strong> for the structural correlation coefficients, the<br />
variations of soil and plant variables were basically consistent with that of SWC<br />
at different spatial scales. The weak correlations between soil moisture and plant<br />
properties in the two ungrazed sites may be further explained by the high nugget<br />
variations of plant properties. This difference could be due to grazing intensity as<br />
the regionalized variables had a more heterogeneous spatial distribution in the<br />
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