冻融对沼泽湿地土壤水稳性大团聚体的影响
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福建省青年人才项目(2008F3019);国家自然科学基金(30900280);中国科学院知识创新工程重要方向项目(KZCX22YW2309)


Effects of Freezing2tha wing on Soil Water2stable Aggregates in Fresh Marsh
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    摘要:

    水稳性大团聚体(>0. 25 mm)是土壤侵蚀和质量的重要表征指标。通过室内培养,在不同含水量、冻融次数和压实处理条件下,研究冻融过程对三江平原沼泽湿地土壤水稳性大团聚体的影响。结果表明,冻融过程影响土壤水稳性大团聚体含量,但压实和土壤起始含水量对湿地土壤的水稳性大团聚体影响较小,而冻融次数影响显著。4次冻融前,随着冻融次数的增加,不同处理的土壤水稳性大团聚体含量呈增加趋势;4次冻融后,高含水量处理的土壤水稳性大团聚体变化不明显,而低含水量处理的土壤水稳性大团聚含量有微弱增加。

    Abstract:

    Soil water-stable macro-aggregates (>0.25mm) are an important characteristic index of soil ero-sion and soil quality. The effects of freezing-thawing on the content of soil water-stable macro-aggregates in Sanjiang Plain wetlands were studied under different soil water contents,numbers of freezing2thaw cycles,and compaction treatments by indoor incubation experiment. Results showed that the content of soil water-stable macro-aggregate was influenced by the freezing2thawing. The effects of freezing-thawing frequency were more significant compared with compaction and initial soil water content. Before the 4th freezing-thaw cycle,the content of soil water-stable macro-aggregates under different treatments increased with the increas-ing of freezing2thawing frequency. After the 4th freezing-thaw cycle,however,the content at high soil water content did not change obviously and increased slightly.

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秦胜金,刘景双,丁洪,张玉树.冻融对沼泽湿地土壤水稳性大团聚体的影响[J].水土保持通报,2009,(6):115-118

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  • 收稿日期:2009-04-08
  • 最后修改日期:2009-05-25
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  • 在线发布日期: 2014-11-26
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