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西部采煤沉陷区长期微生物复垦紫穗槐水分利用策略研究

Long term microbial reclamation optimization of water use strategy for purple locust in western coal mining subsidence areas

  • 摘要: 探明半干旱区采煤沉陷地长期微生物复垦下植物水分利用策略及其对土壤水分的响应特征,是矿山生态复垦可持续发展的重要依据。以长期进行微生物复垦的陕北大柳塔采煤沉陷地为研究区,采用同位素示踪、直接相关法、贝叶斯混合模型(Mixing Model with Stable Isotope Analysis in R,MixSiAR)等方法,分析了微生物复垦(丛枝菌根真菌(Arbuscular Mycorrhizal Fungi,AM))和植被复垦10、9、8 a的紫穗槐样地土壤水分、根系分布、水分利用比例及效率等指标。结果表明:长期复垦下浅层土层水分没有表现出显著差异,而在深层土壤(1.5 m下),微生物复垦具有显著的保水作用,其复垦10、9、8 a处理分别增加16.5%、33.6%、51.0%。基于土壤纵剖面水分变化率,所有复垦处理在深度1 m内土壤含水率均处于亏缺状态,相较于CK处理,植被复垦土壤水分平均变化率为−33.9%,而微生物复垦处理平均增加了39.7%。紫穗槐木质部水与土壤水的氢氧同位素的重合度均大于95%,表明紫穗槐木质部水的分馏程度较小,深层土壤水的同位素组成则趋于稳定。相较于植被复垦,微生物复垦下水的δD和δ18O表现出相似的变化趋势,所有处理紫穗槐木质部水与土壤水的交点普遍下移,表明接菌处理后紫穗槐的用水层位有所加深。所有处理紫穗槐对土壤水分的绝对利用量表现为以表层土壤水为主,在累计土壤剖面水分利用率表现为微生物复垦以浅深层土壤水分为主,对深层土壤水分的利用比例和效率平均增加11.2%和9.1%。综上,长期微生物复垦优化了复垦植被的水分利用策略,有利于采煤沉陷地水分保蓄,促进了矿区生态持续正向演替。

     

    Abstract: Clarifying the plant water use strategy and its response characteristics to soil moisture under long-term mycorrhizal reclamation in coal mining subsidence areas in semi-arid regions is an important basis for the sustainable development of mining ecological reclamation. This study focuses on the long-term mycorrhizal reclamation of the Daliuta coal mining subsidence area in northern Shaanxi. Isotope tracing, direct correlation method, Bayesian mixed model (Mixing Model with Stable Isotope Analysis in R, MixSiAR), and other methods were used to analyze soil moisture, root distribution, water use ratio, and efficiency indicators of purple locust sample plots after mycorrhizal reclamation (Arbuscular Mycorrhizal Fungi, AM) and vegetation reclamation for 10, 9, and 8 a. The results showed that there was no significant difference in water content in the shallow soil layer under long-term reclamation, while mycorrhizal reclamation had a significant water retention effect in the deep soil layer (below 1.5m) , with an increase of 16.5%, 33.6%, and 51.0% after 10, 9, and 8 a of reclamation, respectively. Based on the rate of soil moisture change in the longitudinal profile, all reclamation treatments showed a deficit in soil moisture content within a depth of 1 meter. Compared with the CK treatment, the average rate of soil moisture change in vegetation reclamation was −33.9%, while the mycorrhizal reclamation treatment increased by an average of 39.7%. The coincidence degree of hydrogen and oxygen isotopes between the water in the xylem of sophora japonica and soil water is greater than 95%, indicating that the degree of fractionation of water in the xylem of sophora japonica is relatively small, while the isotopic composition of deep soil water tends to be stable. Compared with vegetation reclamation, the δD and δ18O of water in mycorrhizal reclamation showed similar trends, and the intersection of xylem water and soil water in all treatments of sophora japonica generally shifted downwards, indicating that the water use layer of sophora japonica was deepened after inoculation treatment. The absolute utilization of soil water by all treatments of sophora japonica showed that surface soil water was the main source, and the cumulative soil profile water use efficiency showed that mycorrhizal reclamation was mainly based on shallow and deep soil water, with an average increase of 11.2% and 9.1% in the utilization ratio and efficiency of deep soil water. In summary, long-term mycorrhizal reclamation has optimized the water use strategy of reclaimed vegetation, which is beneficial for water retention in coal mining subsidence areas and promotes sustainable positive ecological succession in mining areas.

     

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