2008
DOI: 10.1007/s11119-008-9077-x
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Soil heterogeneity at the field scale: a challenge for precision crop protection

Abstract: Crop protection seldom takes into account soil heterogeneity at the field scale. Yet, variable site characteristics affect the incidence of pests as well as the efficacy and fate of pesticides in soil. This article reviews crucial starting points for incorporating soil information into precision crop protection (PCP). At present, the lack of adequate field maps is a major drawback. Conventional soil analyses are too expensive to capture soil heterogeneity at the field scale with the required spatial resolution… Show more

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Cited by 82 publications
(61 citation statements)
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“…Moreover, clay has the lowest share of the three texture compartments in our study area, such that it may have been less distinct within spectral reflectance. The SOC model provided results comparable to those achieved by Patzold et al [24] and Stevens et al [28]; indeed, it even slightly exceeded their quality.…”
Section: Discussionsupporting
confidence: 75%
See 1 more Smart Citation
“…Moreover, clay has the lowest share of the three texture compartments in our study area, such that it may have been less distinct within spectral reflectance. The SOC model provided results comparable to those achieved by Patzold et al [24] and Stevens et al [28]; indeed, it even slightly exceeded their quality.…”
Section: Discussionsupporting
confidence: 75%
“…Under laboratory conditions, Patzold et al [24] were able to predict SOC with PLSR and achieved an R 2 value of 0.93. They concluded that SOC estimations using laboratory spectroscopy lead to promising results.…”
Section: Introductionmentioning
confidence: 99%
“…SOC content, in particular, has been often related to reflectance data acquired by airborne spectrometers. with the HyMap sensor (420-2480 nm) while Patzold et al (2008) obtained a R 2 of 0.74 with the same sensor and a very limited set of composite soil samples. Less satisfactory prediction models of SOM were obtained by Bajwa and Tian (2005) with the RDACS/H-3 sensor (471-828 nm; R 2 = 0.66) and De Tar et al (2008) with the AVNIR sensor (429-1010 nm; R 2 = 0.48).…”
Section: Introductionmentioning
confidence: 93%
“…Mid-infrared spectra cover a larger range of frequencies and are more efficient to reflect the chemical properties of soil organic matter . They are preferentially used to predict organic components and exchangeable elements in litter and soil (Patzold et al 2008), especially soil carbon, nitrate, metals, and microelements (Kuang et al 2012), whereas near-infrared analyses associated with MIR reveal the physical properties of soil (Soriano-Disla et al 2014). Near-infrared spectra are a good predictor of clay content, exchangeable K (Viscarra Rossel et al 2006), and moisture content (Kuang et al 2012).…”
Section: Validation Of the Repeated Random Drawingmentioning
confidence: 99%