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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 />

57

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