The influence of field survey principles on the quality of approximation of the relationship between the content of soil organic matter and multi-temporal spectral characteristics

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Abstract

Five field surveys of the same territory were conducted to establish functional relationships between the content of soil organic matter (SOM) and multi-temporal spectral characteristics of the bare soil surface (BSS). The surveys differ in five methods for planning soil sampling sites. Three methods used traditional approaches using regular and irregular networks, and two methods used the coefficient C map of the multi-temporal (empirical) soil line (MSL). It is shown that it is difficult to obtain a stable relationship between the values of the spectral characteristics of remote sensing data and the SOM content using traditional methods. The determination coefficients of such dependencies are below 0.60, which does not allow to recommend the obtained dependencies for the purposes of SOM mapping. Organization of field work based on a pre-built map of the coefficient C of the MSL showed the possibility of establishing functional relationships between the SOM content and multi-temporal spectral characteristics of the BSS with a determination coefficient of 0.81. The reason for the different quality of regression models is the omission of a number of soil objects during traditional organization of field work and problems in positioning the sampling. Correction of traditional field surveys based on multi-temporal spectral characteristics of the BSS allows improving the quality of research and developing new methods for SOM mapping.

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About the authors

D. I. Rukhovich

Dokuchaev Soil Institute

Email: soilmap@yandex.ru
ORCID iD: 0000-0002-8002-0698
Russian Federation, Moscow

D. G. Borshchev

Dokuchaev Soil Institute

Email: soilmap@yandex.ru
Russian Federation, Moscow

P. V. Koroleva

Dokuchaev Soil Institute

Author for correspondence.
Email: soilmap@yandex.ru
ORCID iD: 0009-0000-0689-4621
Russian Federation, Moscow

A. D. Rukhovich

Dokuchaev Soil Institute

Email: soilmap@yandex.ru
ORCID iD: 0000-0002-5701-1785
Russian Federation, Moscow

References

Supplementary files

Supplementary Files
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1. JATS XML
2. Fig. 1. Block diagram of operation.

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3. Fig. 2. Ground survey maps and SOM content: (a) – agrochemical survey by fields (survey 1), (b) – agrochemical survey by elementary plots (survey 2), (c) – soil survey based on the map of the coefficient of the SML (survey 4) on the map of the coefficient of the SML, (d) – agrochemical survey by points based on the map of the coefficient of the SML (survey 5) on the map of the coefficient of the SML.

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4. Fig. 3. Dependence of the SOM content on multi-temporal spectral characteristics of the soil (the coefficient of the SML): (a) – agrochemical survey by fields (survey 1), (b) – agrochemical survey by elementary plots (survey 2), (c) – soil survey based on the map of the coefficient of the SML (survey 4), (d) – agrochemical survey by points based on the map of the coefficient of the SML (survey 5).

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5. Fig. 4. Combined graphs of the dependence of the SOM content on multi-temporal spectral characteristics of the soil (the coefficient of the SML): (a) – 1 – agrochemical survey by points based on the map of the coefficient of the SML (survey 5), 2 – agrochemical survey by elementary plots (survey 2), 3 – traditional soil survey (survey 3); (b) – 1 – SOM content obtained by intersecting the coordinates of the points of agrochemical survey 5 and the map of the traditional agrochemical survey by elementary plots (survey 2), 2 – agrochemical survey 5.

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6. Additional materials: The influence of field survey principles on the quality of approximation of the relationship between the content of soil organic matter and multi-temporal spectral characteristics.
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