荒漠开垦与施肥对土壤有机碳储量与微生物群落特征的影响

Effects of desert reclamation and fertilization on soil organic carbon storage and microbial community characteristics

  • 摘要:目的 】研究开垦与长期不同施肥对荒漠土壤有机碳(SOC)储量与微生物群落特征(微生物丰度和群落结构)的影响。【 方法 】以中国科学院阜康荒漠生态站长期定位试验为平台,选择11种管理模式:不施肥(CK a)、单施化肥(PK b、NK c、NP d、NPK e、N2P2 f、N2P2K g),化肥配施秸秆(NPKR h,NPKR2 i,N2P2R3 j)和化肥配施厩肥(NPKM k),采集其0~20 cm土层样品,与同一毗邻原生荒漠土壤进行比较,分析荒漠开垦过程中土壤有机碳储量和微生物群落特征及两者的联系。【 结果 】与毗邻荒漠相比,开垦与长期施肥显著增加了土壤有机碳储量;同时,土壤细菌、真菌、古菌及固氮菌的丰度显著增加,真菌>细菌>古菌;其中,处理g、处理j与处理k中土壤有机碳储量及微生物丰度均具有较高增幅。【 结论 】荒漠开垦与施肥通过降低土壤pH值与盐分,增加外源有机质与养分输入,提高了土壤有机碳储量和微生物丰度,改变了微生物群落结构。植被对干旱区土壤有机碳汇的形成有正向促进作用,化肥(尤其是N、P)配施有机肥增加了干旱区土壤有机碳储量和微生物群落丰度。

     

    Abstract:Objective 】To study the effects of reclamation and long-term fertilization on soil organic carbon (SOC) storage and microbial community characteristics (microbial abundance and community structure) in desert soils. 【 Methods 】Taking the long-term positioning experiment of Fukang Desert Ecological Station of Chinese Academy of Sciences as the platform, 11 management modes were selected: no fertilization (CK a), single application of chemical fertilizer (PK b, NK c, NP d, NPK e, N2P2 f, N2P2K g), chemical fertilizer with straw (NPKR h, NPKR2 i, N2P2R3 j) and chemical fertilizer with manure (NPKM k). They were compared with the adjacent native desert soil by collecting 0-20 cm soil layer samples, and then the characteristics of soil organic carbon storage and microbial community in the process of desert reclamation and the relationship between them were analyzed. 【 Results 】When reclaimed and long-term fertilized soils to adjacent desert soils were compared, reclamation and fertilization significantly increased soil organic carbon storage. In addition, the abundance of soil bacteria, fungi, archaea, and nitrogen-fixing microorganisms was substantially increased, with the following order of enhancement: fungi > bacteria > archaea. Specifically, treatments g, j, and k showed higher increases in both soil organic carbon storage and microbial abundance. 【 Conclusion 】Desert reclamation and fertilization, through reducing soil pH and salinity, increasing the input of exogenous organic matter and nutrients, have increased the storage of soil organic carbon and the abundance of microorganisms, and changed the structure of the microbial community. The positive effect of vegetation on the formation of soil organic carbon sinks in arid areas, and the importance of chemical fertilizers (especially N and P) combined with organic fertilizers for soil organic carbon storage and microbial abundance in arid regions.

     

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