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Spatial Variability Analysis of Soil Physical …(土壤空间变异性分析物理u2026)
Spatial Variability Analysis of Soil Physical Properties of Alluvial Soils
Javed Iqbal,* John A. Thomasson, Johnie N. Jenkins, Phillip R. Owens, and Frank D. Whisler
.
d ABSTRACT ited on sandy or on loamy sediments. Therefore, it is
e
v
r Analysis and interpretation of spatial variability of soils is a key- important to study not only the extent of surface spatial
e
s stone in site-specific farming. Soil survey maps may have up to 0.41- variability, but also the distribution of subsurface and
e
r
s ha inclusions of dissimilar soils within a mapping unit. The objectives deep soil horizons.
t of this study were to determine the degree of spatial variability of soil Among the various soil physical properties, Ks and
h
g physical properties and variance structure, and to model the sampling
i related measures are reported to have the highest statis-
r
y interval of alluvial floodplain soils. Soil profiles (n 209) from 18 tical variability (Biggar and Nielsen, 1976). Bouma
p
o parallel transects were sampled with a mean separation distance of (1973) stressed the need for more studies on field vari-
c
l 79.4 m. Each profile was classified into surface, subsurface, and deep
l ability of Ks and soil water retention curves. Stockton
A horizons. Structural analysis of soil bulk density ( ), sand, clay, satu-
b
a. rated hydraulic conductivity (K ), volumetric water content ( ) at and Warrick (1971) indicated that var
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