Rav. Rossel et Ab. Mcbratney, LABORATORY EVALUATION OF A PROXIMAL SENSING TECHNIQUE FOR SIMULTANEOUS MEASUREMENT OF SOIL CLAY AND WATER-CONTENT, Geoderma, 85(1), 1998, pp. 19-39
Precision agriculture, largely the application of information and comm
unications' technologies to in-field data gathering and management, ma
y be regarded as 'best practice' far crop growth in the future because
of its twin goals of maximising economic returns whilst concurrently
minimising environmental impact. The practice of precision agriculture
, whether it be to differentially apply fertiliser, seed, pesticide, i
rrigation or tillage requires detailed knowledge of the spatial and te
mporal variation of crop yield components, weeds, soil-borne pests and
attributes of physical, chemical and biological soil fertility. Howev
er, a detailed description of fine or even coarse scale variation in s
oil properties has always been difficult and costly to perform. Sensin
g and scanning technologies are currently being developed to more effi
ciently and economically describe and obtain precise information on th
e extent and variability of soil attributes which affect crop growth a
nd yield. Combining these technologies with vastly improved ground pos
itioning systems allows detailed mapping of soil resource and crop yie
ld variability which may therefore be an important input for site-spec
ific decision making. Experiments were conducted to design an invasive
sensor for real-time, simultaneous measurements of clay, organic matt
er and soil water content from reflectance of a suitable wavelength or
combination of wavelengths in the near infra-red (NIR) portion of the
electromagnetic spectrum. Soil materials were prepared with varying a
mounts of clay, soil water and organic matter according to a response-
surface design, and the reflectance spectra measured at 2-nm intervals
from 1300 nm to 2500 nm. Response-surface models were fitted to the r
eflectance data at specified wavelengths. Reflectance showed significa
nt response to clay content and soil water but not to organic matter.
A thorough selection procedure using non-linear modelling and root-mea
n-square-error of prediction was used to derive the four most suitable
wavelengths (1600, 1800, 2000 and 2100 nm) for simultaneously measuri
ng clay and soil water content. In a simulation experiment clay conten
t was more accurately predicted than water content. (C) 1998 Elsevier
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