Jg. White et al., SOIL ZINC MAP OF THE USA USING GEOSTATISTICS AND GEOGRAPHIC INFORMATION-SYSTEMS, Soil Science Society of America journal, 61(1), 1997, pp. 185-194
The geographic distribution of soil Zn is important to agriculture, nu
trition, and health. A map illustrating the total Zn content of soils
of the conterminous USA was developed using geostatistics and geograph
ic information systems. Data were combined from a U.S. Geological Surv
ey study targeting nonagricultural soils in 47 states, and a U.S. Depa
rtment of Agriculture-U.S. Environmental Protection Agency-U.S. Food a
nd Drug Administration study targeting agricultural soils in 33 states
. Semivariograms indicated spatial correlation at distances up to 470
km. A significant quadratic trend was modeled, but detrending had litt
le effect on the semivariogram or on interpolation via kriging. The da
ta exhibited some anisotropy, but it had little effect on kriging. An
exponential semivariogram model was fit using least squares and used t
o krige a grid covering the conterminous USA. The resultant map depict
ed soils north of about 37 degrees N latitude or west of about 109 deg
rees W longitude as generally having more Zn than the average of 55 mg
kg(-1). Soils southeast of this boundary tended to contain less Zn th
an average, with exceptions of soils developed on Mississippi alluvium
and in Piedmont valleys and ridges. High estimate standard deviations
occurred where data were sparse. The map will be useful in future res
earch to determine the geographic distribution of plant-available soil
Zn, regional patterns of plant, animal, and human Zn deficiencies, th
e relationship of Zn to soil parent material, genesis, and surficial g
eology, and in considering the consequences of land disposal of Zn-lad
en wastes.