亚表层有机培肥调控盐渍土孔隙结构与水盐运移机制
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国家自然科学基金项目(31871584)、国家重点研发计划项目(2016YFC0501302)和中央级公益性科研院所基本科研业务费专项(1610132020011)


Effects of Pore Structure and Water-Salt Movement for Saline Soil under Subsurface Organic Amendment
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    摘要:

    为探明亚表层有机培肥结合地膜覆盖对土壤孔隙结构及其水盐运移的调控机制,以内蒙古河套灌区典型盐渍土为研究对象,设置了地表不覆膜(CK)、地膜每年覆盖(PM)和亚表层单次有机培肥+地膜每年覆盖(OMP)3个处理,3年后采用X射线CT扫描和图像处理技术获取了部分亚表层(15~21cm)与深层(35~41cm)土壤孔隙结构信息,同时测定了土壤剖面水盐含量,分析了土壤孔隙结构与水盐分布特征的关系。结果表明,PM处理与CK相比,亚表层大孔隙度(>30μm)无明显差异(P>0.05),但深土层降低了0.48个百分点(P<0.05)。OMP处理与CK相比,亚表层及深土层大孔隙度分别提高了11.95、0.75个百分点(P<0.05),其中不同当量直径孔隙度和孔隙连通度均差异显著(P<0.05)。与CK和PM处理相比,OMP处理春灌后0~40cm土层含水率分别提高12.02%和6.33%(P<0.05),全盐含量分别降低了16.22%和13.21%(P<0.05);收获后0~40cm土壤含水率分别降低40.69%和35.77%(P<0.05),返盐率分别降低了12.22、11.56个百分点(P<0.05)。大孔隙度、土壤孔隙连通度与水盐含量显著相关(P<0.05),增加当量直径小于1.500μm孔隙度可以显著提高春灌后土壤保水效果,而增加当量直径小于500μm孔隙度可以促进春灌后盐分淋洗。通过在亚表层施用有机肥结合地膜覆盖可以优化土壤物理结构,增强盐渍土水盐调控能力。

    Abstract:

    Plastic film mulching is one of the widely adopted agronomic measures in the northwest of China, and subsurface (10~30cm) organic amendment is an important soil improvement and fertilization technique to quickly realize the efficient use of salinized farmland. However, it is still not clear of the effects of combinations of plastic film mulching and subsurface organic amendment on the soil pore structure and water-salt movement. The field experiment with three treatments was conducted: with (PM) and without (CK) plastic film mulching yearly, as well as the combination of subsurface organic amendment once with plastic film mulching yearly (OMP), in a typical saline soil in the Hetao Irrigation District of Inner Mongolia. Pore structures of subsurface (15~21cm) and deep (35~41cm) soil layers were measured by X-ray computed tomography and image processing, water and salt contents within soil profiles were measured in three years after the applications simultaneously, and then the effects of soil pore structure on water-salt movement were analyzed. The results showed that there was no significant difference (P>0.05) in macroporosity (greater than 30μm) between PM and CK in subsurface soil layer. However, the macroporosity in deep soil layer of PM was decreased by 0.48 percentage points than that of CK(P<0.05). Compared with CK, the macroporosity of OMP was boosted by 11.95 percentage points and 0.75 percentage points in subsurface and deep soil layers (P<0.05), respectively. The porosity of each equivalent pore size and the pore connectivity were also improved significantly with OMP than that with CK. Compared with CK and PM, the water contents in 0~40cm soil layers with OMP were significantly increased by 12.02% and 6.33%, and its total salt contents were significantly reduced by 16.22% and 13.21% (P<0.05) after spring irrigation, respectively. In addition, the water contents in 0~40cm soil layers with OMP were decreased by 40.69% and 35.77% after harvest, and its salt accumulation rate was reduced by 12.22 percentage points and 11.56 percentage points respectively (P<0.05), compared with CK and PM. It was worth noting that the macroporosity, soil pore connectivity, and water-salt content were significantly related (P<0.05). Increasing the porosity of equivalent diameter (less than 1.500μm) significantly improved the soil water retention ability, and fortifying the porosity of equivalent diameter (less than 500μm) promoted the salt leaching after spring irrigation. Therefore, subsurface organic amendment combined with plastic film mulching could optimize the soil physical structure and enhance the regulation ability to regulate water and salt contents in saline soil.

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张宏媛,逄焕成,宋佳珅,王国丽,常芳弟,李玉义.亚表层有机培肥调控盐渍土孔隙结构与水盐运移机制[J].农业机械学报,2022,53(2):355-364. ZHANG Hongyuan, PANG Huancheng, SONG Jiashen, WANG Guoli, CHANG Fangdi, LI Yuyi. Effects of Pore Structure and Water-Salt Movement for Saline Soil under Subsurface Organic Amendment[J]. Transactions of the Chinese Society for Agricultural Machinery,2022,53(2):355-364.

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  • 收稿日期:2021-02-23
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  • 在线发布日期: 2021-04-06
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