河南农业科学 ›› 2019, Vol. 48 ›› Issue (11): 84-91.DOI: 10.15933/j.cnki.1004-3268.2019.11.012

• 农业资源与环境 • 上一篇    下一篇

黔西南不同程度石漠化土壤的养分、酶活性特征

杨丹,石菊,李冕,杜润来,管庆丽   

  1. (贵阳学院生物与环境工程学院,贵州 贵阳 550005)
  • 收稿日期:2019-05-06 出版日期:2019-11-15 发布日期:2019-11-15
  • 作者简介:杨丹(1982-),女,贵州兴义人,副教授,博士,主要从事土壤环境质量评价与污染防治研究。E-mail:yangdansky@163.com
  • 基金资助:
    国家自然科学基金项目(31600442);贵州省教育厅科技拔尖人才支持计划项目(黔教合KY字[2018]063);贵阳学院引进人才科研启动项目(2017);贵州省高等学校大学生创新创业训练计划项目(2018520806);贵州省教育厅青年科技人才成长项目(黔教合KY字[2018]295)

Characteristics of Nutrients and Enzyme Activity in Different Grades of Rocky Desertification Soils in Southwest Guizhou

YANG Dan,SHI Ju,LI Mian,DU Runlai,GUAN Qingli   

  1.  ( School of Biological and Environmental Engineering,Guiyang University,Guiyang 550005,China)
  • Received:2019-05-06 Published:2019-11-15 Online:2019-11-15

摘要: 为了解石漠化土壤质量状况,以贵州典型喀斯特地区不同程度石漠化土壤为研究对象,运用野外定点采样和实验室测定的方法,分析不同程度石漠化土壤养分及酶活性特征,探讨不同程度石漠化土壤质量变化规律,为石漠化生态环境修复过程中土壤质量的改善提供依据。结果表明,石漠化使土壤pH值显著增加,增加了4.49%~5.80%;石漠化土壤有机质、全氮含量反而高于无石漠化土壤,分别高1.02~2.99倍、3.65%~24.82%,但全磷全钾含量在中度和重度石漠化土壤中显著降低。随着石漠化程度加重,土壤蔗糖酶、脲酶、脱氢酶、纤维素酶活性降低。从轻度到重度石漠化土壤,蔗糖酶活性降低了22.33%~71.46%,脲酶活性降低了31.25%~80.14%。中度、重度石漠化土壤脱氢酶活性分别降低了70.83%、83.33%,纤维素酶活性分别下降了55.0%、80.0%。碱性磷酸酶活性在重度石漠化土壤中仅为无石漠化土壤的24.78%。因此,土壤养分含量和酶活性可作为反映不同程度石漠化土壤质量的重要指标。

关键词: 喀斯特, 石漠化土壤, 土壤养分, 酶活性, 土壤质量

Abstract:  In order to reveal the qualitative status of soils in rocky desertification region,different degrees of rocky desertification soils were collected from a typical karst region in Guizhou Province as research ob ject.The nutrients content and enzymatic activity were analyzed,based on field sampling and laboratory determination,and the changes of soil quality with different degrees of rocky desertification were explored,to provide the foundation for possible soil improvement and ecological restoration in rocky desertification areas.The results showed that soil pH significantly increased by 4.49%—5.80% in rocky desertification soils.Organic matter and total nitrogen content in rocky desertification soils were higher than those in no rocky desertification soil.Soil organic matter content was 1.02—2.99 times more,and total nitrogen con tent was 3.65%—24.82% more in rocky desertification soils.However,total phosphorus content and to tal potassium content significantly decreased in moderate and severe rocky desertification soils.Activities of soil ivertase,urease,dehydrogenase,cellulose showed obvious decrease as the rocky desertification ag gravated.From light to severe rocky desertification,soil ivertase activity declined by 22.33% —71.46%,soil urease activity decreased by 31.25%—80.14%.Soil dehydrogenase activity was 70.83% and 83.33% down,and soil cellulose activity declined by 55.0% and 80.0% respectively in moderate and severe rocky desertification soils. Alkaline phosphatase activity was only 24.78% of the no rocky desertifi cation soil in severe desertification soil.Therefore,the nutrients content and enzyme activities could be ap plied as critical indicators for evaluating the soil quality in various degrees of rocky desertification soils.

Key words:  Karst, Rocky desertification soils, Soil nutrient, Enzyme activity, Soil quality

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