干旱绿洲长期微咸地下水灌溉对棉田土壤微生物量影响

    Effects of long-term irrigation with brackish groundwater on soil microbial biomass in cotton field in arid oasis

    • 摘要: 由于淡水资源的缺乏,利用微咸地下水灌溉是干旱绿洲普遍采用的一种灌溉措施。该文对北疆棉区长期利用微咸地下水灌溉的土壤微生物和酶活性进行了研究。结果表明,长期微咸地下水灌溉土壤的含盐量比渠水灌溉上升61.5%,显著增加了棉田耕层土壤盐分(P<0.05),土壤可交换性钠百分率(ESP)升高3.2倍,并造成土壤碱化。微咸地下水灌溉纤维素酶、脲酶等、转化酶及过氧化氢酶4种酶活性分别降低了21.3%、50.9%、50.0%和10.5%,但在微咸地下水灌溉条件下多酚氧化酶和碱性磷酸酶的活性显著升高。微咸地下水灌溉对土壤微生物有明显抑制作用,长期微咸水灌溉使土壤微生物量碳、氮分别降低24.4%和42.4%,但对微生物量磷影响不显著。微生物量和酶活性与棉田土壤肥力密切相关,长期微咸地下水灌溉导致有机质、全氮分别降低26.8%和28.0%。长期微咸地下水灌溉影响了土壤生物质量,不利于绿洲农田土壤的持续利用。

       

      Abstract: Due to the shortage of fresh water, groundwater is the main resource for irrigation in arid oasia. In the present study, the impacts of ten-year irrigation with brackish ground water on soil microbial biomass and enzyme activity were compared to those of fresh water in a cotton farming system. The results showed that total salt content changes were significantly greater in soil receiving long-term saline groundwater irrigation (P<0.05), compared with fresh water irrigation, total soil salt content and exchangeable sodium percentage(ESP) increased by 61.5% and 3.2 times, respectively. In the salt affected soil, total enzyme activities of cellulose, urease, invertase and catalase decreased by 21.3%, 50.9%, 50% and 10.5%, respectively. By contrast, soil alkaline phosphatase and polyphenol oxidase activities increased significantly (P<0.05) with increasing salinity and sodicity. Long time brackish groundwater irrigation caused deleterious effects on soil microbial biomass, with biomass carbon and biomass nitrogen decreasing by 24.4% and 42.4%, respectively. However, no obvious detrimental effect of salinity on soil microbial biomass phosphorus was observed. Microbial biomass and enzyme activities were closely related to soil fertility in cotton fields. Organic matter and total nitrogen with the long-term brackish ground water irrigation decreased by 26.8% and 28.0%, respectively. These results reveal that long-term saline groundwater irrigation not only influences the chemical and physical characteristics of soils, but also directly affects soil biological properties and, therefore, has important implications for soils health and sustainability in arid agricultural areas.

       

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