基于CT扫描技术探究滩涂围垦区土壤孔隙特征

Soil Pore Characteristics of Coastal Reclamation Zones Based on CT Scanning Technology

  • 摘要:
    目的 研究滩涂围垦区不同土地利用方式下土壤孔隙分布特征,为滩涂围垦区盐渍化土壤改良和开发利用提供依据。
    方法 试验选取上海崇明滩涂围垦区水稻田和撂荒地为研究对象,采用原状土柱计算机断层扫描(CT)技术和图像分析软件,定量研究滩涂围垦区两种不同土地利用方式下土柱(0 ~ 35 cm)孔隙分布特征;同时测定剖面5 ~ 10 cm、15 ~ 20 cm、20 ~ 25 cm、30 ~ 35 cm深度土壤容重、总孔隙度、通气孔隙度、毛管孔隙度、饱和持水量、毛管持水量和田间持水量等参数;并原位测定土壤紧实度和体积含水量。
    结果 水稻田土柱孔隙分布存在异质性,上层土壤孔隙分布多且孔隙大,而下层土壤孔隙分布少且孔隙小;撂荒地土柱孔隙分布则相对较为均质化。水稻田土柱大孔隙的连通性相对较差,上层土壤大孔隙多以大块状堆积形式存在;撂荒地土柱大孔隙连通性较好,具有明显的竖向管状结构;水稻田和撂荒地土柱大孔隙分布特征与土壤体积含水量具有相关性。相关性分析表明,CT扫描得出的土壤总孔隙(> 0.05 mm)占比和大孔隙(> 1 mm)占比与容重均呈显著负相关(P < 0.05),与总孔隙度、饱和持水量、毛管持水量和田间持水量均呈显著正相关(P < 0.05)。
    结论 土柱CT扫描技术获得的土壤孔隙特征参数可为滩涂围垦区土壤改良提供参考。

     

    Abstract:
    Objective To provide basis for the improvement of saline soil and utilization of coastal reclamation zones, the pore distribution characteristics of soil column under different land use types of coastal reclamation zones were analyzed.
    Methods Paddy field and abandoned land of coastal reclamation zones were selected in Chongming, Shanghai, and the pore distribution characteristics of soil column (0 - 35 cm) were quantitatively studied under two different use land types of coastal reclamation zones, by using the soil column computed tomography (CT) technology and image analysis software. At the same time, soil bulk density, total soil porosity, soil aerated porosity, soil capillary porosity, soil saturated water holding capacity, soil capillary holding water capacity and soil field water holding capacity of 5 - 10 cm, 15 - 20 cm, 20 - 25 cm and 30 - 35 cm on the soil profile were measured. Soil compaction and volumetric water content were measured in situ by soil compaction meter and soil sensor.
    Results The results showed that there was a heterogeneity for the pore distribution of soil column in paddy field. The more and larger pore distribution was found in the upper soil layer, the less the subsoil layer had pore distribution. The pore distribution of soil column in abandoned land was relatively homogeneous. The connectivity of soil macro-pores in paddy field was relatively poorer, and the macro-pores of the upper soil mostly existed in the form of massive accumulation. The soil macro-pore connectivity in the abandoned land was relatively better, and the vertical tubular structure was obvious. The distribution characteristics of soil macro-pore in paddy field and abandoned land were relevant to soil volumetric water content. Correlation analysis showed that the ratio of total porosity and macro-porosity obtain by CT were negatively correlated with soil bulk density (P < 0.05), and significantly positively correlated with total porosity, soil saturated water holding capacity, soil capillary water holding capacity and soil field water holding capacity (P < 0.05).
    Conclusion The soil pore characteristic parameters obtained by soil column CT scanning technology would provide reference for soil improvement in coastal reclamation zones.

     

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