Improved 3D characterization of in-situ soil desiccation cracking by multi-source data integration

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE Geoderma Pub Date : 2024-09-01 DOI:10.1016/j.geoderma.2024.117033
Jun-Zheng Zhang, Chao-Sheng Tang, Wen Mu, Jin-Jian Xu, Qi-You Zhou, Bin Shi
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Abstract

Desiccation cracking is a common and natural phenomenon under a drought climate. The geometric and morphologic characteristics of the crack pattern are critical to understanding the response of soil mechanical and hydraulic properties to drought climate. It is always a big challenge to obtain the refined geometric structure of the in-situ soil desiccation crack network. This study proposes an integrated method named ERT+ for determining the three-dimensional geometry of in-situ soil desiccation crack networks by integrating multi-source data from electrical resistivity tomography (ERT), surface image analysis, and depth investigation. The proposed method was applied to three in-situ expansive soil sites with different crack geometries and soil properties. The results showed that the joint application of ERT with other investigations reduced the ambiguity of interpreting each technique independently. The crack network model characterized the three-dimensional geometric structure of the desiccation crack accurately and quantitatively, verifying the effectiveness and feasibility of the ERT+ method. Field and laboratory experiments showed that heterogeneity in soil properties resulted in different cracking morphologies (width, depth, and width-depth ratio). The crack geometric data suggested that the width-depth ratio of the crack network was related to the cracking modes and the soil properties, indicating the non-homology of different crack networks. In addition, the correction gradients calculated from the ERT+ method also varied with the cracking modes and soil properties, further suggesting the reliability and prospect of the proposed method.

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通过多源数据整合改进原位土壤干燥开裂的三维特征描述
干燥开裂是干旱气候下一种常见的自然现象。裂纹模式的几何和形态特征对于了解土壤力学和水力特性对干旱气候的响应至关重要。如何获得原位土壤干燥裂缝网络的精细几何结构一直是一个巨大的挑战。本研究提出了一种名为 ERT+ 的综合方法,通过整合电阻率层析成像(ERT)、表面图像分析和深度调查等多源数据,确定原位土壤干燥裂缝网络的三维几何结构。所提出的方法被应用于三个具有不同裂缝几何形状和土壤性质的原位膨胀性土壤场地。结果表明,将电阻率层析成像技术与其他勘测技术联合应用,减少了独立解释每种技术的模糊性。裂缝网络模型准确定量地描述了干燥裂缝的三维几何结构,验证了 ERT+ 方法的有效性和可行性。现场和实验室实验表明,土壤性质的异质性导致了不同的裂缝形态(宽度、深度和宽深比)。裂缝几何数据表明,裂缝网络的宽深比与开裂模式和土壤性质有关,表明不同裂缝网络的非同源性。此外,ERT+ 方法计算出的校正梯度也随开裂模式和土壤性质的不同而变化,这进一步表明了所提方法的可靠性和前景。
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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