CAJ | 학술논문

为研究不同根系含量和盐分含量土壤表面干缩裂缝的发育规律，该文提出了一套基于数字图像处理的裂缝几何参数提取方法，分析裂缝形态随含水率的变化规律。结果表明：随着含水率的降低，不同根系含量条件下裂缝面积密度和长度密度的差异显著（P＜0.05），裂缝发育稳定时根系含量越大，面积密度越小，长度密度越大。盐分质量分数为2.0%的土壤试样在整个干燥过程中裂缝面积密度明显比其他低盐分含量的试样高。当含水率＜27%时，盐分含量对土壤裂缝面积密度的影响差异明显，不同盐分含量的土壤裂缝面积密度和长度密度均差异显著（P＜0.05），说明盐分含量越大，稳定时土壤裂缝面积密度越大，长度密度越小。该成果对指导开裂土壤的农田灌溉具有重要的实践意义。
위연구불동근계함량화염분함량토양표면간축렬봉적발육규률，해문제출료일투기우수자도상처리적렬봉궤하삼수제취방법，분석렬봉형태수함수솔적변화규률。결과표명：수착함수솔적강저，불동근계함량조건하렬봉면적밀도화장도밀도적차이현저（P＜0.05），렬봉발육은정시근계함량월대，면적밀도월소，장도밀도월대。염분질량분수위2.0%적토양시양재정개간조과정중렬봉면적밀도명현비기타저염분함량적시양고。당함수솔＜27%시，염분함량대토양렬봉면적밀도적영향차이명현，불동염분함량적토양렬봉면적밀도화장도밀도균차이현저（P＜0.05），설명염분함량월대，은정시토양렬봉면적밀도월대，장도밀도월소。해성과대지도개렬토양적농전관개구유중요적실천의의。
Soil shrinkage cracks which come into being with consumption and evaporation of water, cause changes in soil infiltration capacity and lead to the preferential migration of soil water and solute. To investigate the development law of desiccation cracks on the soil surface under the condition of different roots and salt contents, a set of method, based on digital image processing, was proposed to extract the crack geometry parameter, which greatly improved the efficiency and accuracy of image processing, and then researched the crack morphology variation with water content. In this paper, a laboratory dry test was carried out in the view of root content and soil content of soil samples. It was concluded that when the mass water content >30%, there was little difference among the crack area density of the soil samples with different root length densities. As the mass water content continued to reduce, the crack area density increased gradually, and reached the maximum and kept stable when the mass water content reduced to 10% or so. The influences of different root length densities on the crack area density were quite different (P<0.05), the greater the root length density was, the more obvious the role of root to anchor the soil was, and the smaller the soil crack area density was. When the mass water content >30%, the crack length densities of soil samples with different root length densities all grew fast with the reduction of mass water content, but with little difference. As the moisture content continued to reduce, the greater the root length density was, the greater the crack length density was, and significantly different (P<0.05). And the crack network connectivity index gradually dwindled with the root length density increased. The soil crack area density of the soil sample with a salt content of 2.0% was obviously greater than the soil crack density of the soil samples with other salt content in the whole drying process. When the moisture content was between 27% and 34%, there were little difference among the crack area density with a salt content of 0.5%, 1.0%, 1.5%, respectively, but were all greater than the crack area density of the control group, namely the soil sample with a salt content of 0. As the moisture content continued to reduce, the influences of different salt contents on the soil crack area density became more and more obvious. Soil crack area density and length densities of different salt contents were all significantly different (P<0.05), and it indicated that the greater the salt content was, the larger the soil crack area density was, when the crack network got stable, and the smaller the length density was. Also, the greater the salt content was, the greater the network connectivity index was, and when the salt content got 2.0%, the network connectivity index was 1, which is the maximum value in theory, namely, there was no single-linkage crack. The research results have important practical significance for guiding cracked soil irrigation.