{"title":"Effect of soil crust on the prediction of soil organic matter based on soil colour","authors":"Caiwu Wu , Zhiyong Wu , Ye Wang , Yue Yang","doi":"10.1016/j.catena.2025.108818","DOIUrl":null,"url":null,"abstract":"<div><div>Soil organic matter (SOM) plays a pivotal role in enhancing soil quality and structure. Given the darkening effect of SOM on soil colour, rapid SOM prediction can be achieved by quantifying soil surface colour. However, owing to heterogeneity in soil surfaces and differences in colour acquisition between laboratory and field environments for various sensors, understanding the transferability of laboratory findings to field applications is essential. Therefore, this study aimed to uniquely evaluate the effects of soil crusts formed in field environments and soil moisture on SOM prediction using different sensors. 125 soil samples were collected from the 0–20 cm topsoil layer on the Bashang Plateau, North China. Dispersed and crusted soil samples were prepared in the laboratory to simulate controlled and natural conditions, and colour data were obtained using digital cameras and Nix colour sensors. The study results showed that crusted soil samples exhibited a better correlation with SOM than did dispersed samples, while slight soil moisture enhanced this correlation. Among the red, green and blue bands, the red band exhibited the highest correlation with SOM. Mathematical transformations, particularly the excess red index (ExR), further improved this relationship, achieving a correlation coefficient of 0.87. Comparing the digital camera and Nix sensor prediction results revealed that integrating soil surface variation information facilitated significant model accuracy improvement. Among the modeling results, the digital camera provided the best prediction for the crusted soil samples, with a coefficient of determination (R<sup>2</sup>) of 0.80 and a root-mean-square error (RMSE) of 0.50 %, while R<sup>2</sup><sub>val</sub> = 0.80 and RMSE<sub>val</sub> = 0.61 % were obtained for the validation results. Due to the unevenness of the soil surface and the importance of the sampling area size for stable predictions, the non-contact digital camera is more suitable for the acquiring soil surface colour information and predicting SOM content than the Nix sensor.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"251 ","pages":"Article 108818"},"PeriodicalIF":5.4000,"publicationDate":"2025-02-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0341816225001201","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
Soil organic matter (SOM) plays a pivotal role in enhancing soil quality and structure. Given the darkening effect of SOM on soil colour, rapid SOM prediction can be achieved by quantifying soil surface colour. However, owing to heterogeneity in soil surfaces and differences in colour acquisition between laboratory and field environments for various sensors, understanding the transferability of laboratory findings to field applications is essential. Therefore, this study aimed to uniquely evaluate the effects of soil crusts formed in field environments and soil moisture on SOM prediction using different sensors. 125 soil samples were collected from the 0–20 cm topsoil layer on the Bashang Plateau, North China. Dispersed and crusted soil samples were prepared in the laboratory to simulate controlled and natural conditions, and colour data were obtained using digital cameras and Nix colour sensors. The study results showed that crusted soil samples exhibited a better correlation with SOM than did dispersed samples, while slight soil moisture enhanced this correlation. Among the red, green and blue bands, the red band exhibited the highest correlation with SOM. Mathematical transformations, particularly the excess red index (ExR), further improved this relationship, achieving a correlation coefficient of 0.87. Comparing the digital camera and Nix sensor prediction results revealed that integrating soil surface variation information facilitated significant model accuracy improvement. Among the modeling results, the digital camera provided the best prediction for the crusted soil samples, with a coefficient of determination (R2) of 0.80 and a root-mean-square error (RMSE) of 0.50 %, while R2val = 0.80 and RMSEval = 0.61 % were obtained for the validation results. Due to the unevenness of the soil surface and the importance of the sampling area size for stable predictions, the non-contact digital camera is more suitable for the acquiring soil surface colour information and predicting SOM content than the Nix sensor.
期刊介绍:
Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment.
Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.