Abstract

This paper illustrates a simple yet effective spectroscopic technique for the prediction of soil organic matter (SOM) from moist soil through the synchronous 2D correlation spectroscopy (2D-COS) analysis. In the moist soil system, the strong overlap between the water absorption peaks and the SOM characteristic features in the visible-near infrared (Vis-NIR) spectral region have long been recognised as one of the main factors that causes significant errors in the prediction of the SOM content. The aim of the paper is to illustrate how the tangling effects due to the moisture and the SOM can be unveiled under 2D-COS through a sequential correlogram analysis of the two perturbation variables (i.e., the moisture and the SOM) independently. The main outcome from the 2D-COS analysis is the discovery of SOM-related bands at the 597 nm, 1646 nm and 2138 nm, together with the predominant water absorbance feature at the 1934 nm and the relatively less important ones at 1447 nm and 2210 nm. This information is then utilised to build partial least square regression (PLSR) models for the prediction of the SOM content. The experiment has shown that by discarding noisy bands adjacent to the SOM features, and the removal of the water absorption bands, the determination coefficient of prediction (Rp2) and the ratio of prediction to deviation (RPD) for the prediction of SOM from moist soil have achieved Rp2 = 0.92 and the RPD = 3.19, both of which are about 5% better than that of using all bands for building the PLSR model. The very high RPD (=3.19) obtained in this study may suggest that the 2D-COS technique is effective for the analysis of complex system like the prediction of SOM from moist soil.

Highlights

  • Earth soil consists of complex mixture of substances, including organic carbon (OC), organic matter (OM), minerals, water and air

  • The system chosen in this paper is the assessment of soil organic matter (SOM) from moist soil samples by using spectroscopic technique

  • This makes the assessment of SOM from moist soil using spectroscopic technique very difficult

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Summary

Introduction

Earth soil consists of complex mixture of substances, including organic carbon (OC), organic matter (OM), minerals, water and air. Sensors 2020, 20, 4822 organic matter (SOM) and its content within a unit volume of soil quantifies its fertility for the growth of crops. SOM is mostly the crop residues added to the soil after their decompositions by soil macro-fauna and micro-organisms. As such the SOM consists of carbon, hydrogen, oxygen [1]. The technology for the rapid detection of SOM content in soil has been a hot topic in the soil research community within the past couple decades [2,3,4,5,6,7,8,9,10,11,12,13,14]. Visible-near infrared (Vis-NIR) spectroscopy has been a simple and efficient analytical technique which has been widely deployed for the detection of SOM content [15,16,17,18,19,20,21,22,23]

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