Abstract

Soil surveys are critical for maintaining sustainable use of natural resources while minimizing harmful impacts to the ecosystem. A key soil attribute for many environmental factors, such as CO2 budget, soil fertility and sustainability, is soil organic matter (SOM), as well as its sequestration. Soil spectroscopy is a popular method to assess SOM content rapidly in both field and laboratory domains. However, SOM source composition differs from soil to soil, and the use of spectral-based models for quantifying SOM may present limited accuracy when applying a generic approach to SOM assessment. We therefore examined the extent to which the generic approach can assess SOM contents of different origin using spectral-based models. We created an artificial big dataset composed of pure dune sand as a SOM-free background, which was artificially mixed with increasing amounts of different organic matter (OM) sources obtained from commercial compost of different origins. Dune sand has high albedo and yields optimal conditions for SOM detection. This study combined two methods: partial least squares regression for the prediction of SOM content from reflectance values across the 400–2500 nm region and a soil spectral detection limit (SSDL) to judge the prediction accuracy. Spectral-based models to assess SOM content were evaluated with each OM source as well as with a merged dataset that contained all of the generated samples (generic approach). The latter was concluded to have limitations for assessing low amounts of SOM (<0.6%), even under controlled conditions. Moreover, some of the OM sources were more difficult to monitor than others; accordingly, caution is advised when different SOM sources are present in the examined population.

Highlights

  • Accepted: 13 April 2021Soil organic matter (SOM) is the product of the onsite biochemical decomposition of dead tissues of flora and fauna

  • The soil spectral detection limit (SSDL) method was examined, and it was concluded that the detection of a given class of OM is not necessarily affected only by its OM content and by the non-organic components of the OM source, which change the signals

  • This observation coincides with the results of the spectral angle mapper (SAM) analysis that was applied to the spectral signatures of the composts after the loss on ignition (LOI)

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Summary

Introduction

Soil organic matter (SOM) is the product of the onsite biochemical decomposition of dead tissues of flora and fauna. It controls the chemical and physical properties of the soil and is responsible for its overall health [1,2]. The stage of SOM decomposition is determined by the activity of soil microorganisms, which use fresh organic matter (OM) as an available energy source for reproduction. The young stage in the OM decomposition process refers to the initial phase of the microorganisms’ activity, in which the C:N ratio should be over 26 [4]. The C:N ratio allows one to evaluate the decomposition stage of OM in both natural soil and compost substances

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