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冻融过程对土壤物理化学及生物学性质的影响研究及展望
引用本文:高敏,李艳霞,张雪莲,张丰松,刘蓓,高诗颖,陈兴财.冻融过程对土壤物理化学及生物学性质的影响研究及展望[J].农业环境科学学报,2016,35(12):2269-2274.
作者姓名:高敏  李艳霞  张雪莲  张丰松  刘蓓  高诗颖  陈兴财
作者单位:1. 北京师范大学环境学院水环境模拟国家重点实验室,北京,100875;2. 北京市土肥工作站,北京,100029;3. 中国科学院地理科学与资源研究所,北京,100101
基金项目:国家自然科学基金项目(21577007,21277013);“十三五”国家重点研发计划重点专项(2016YFD0800204)
摘    要:冻融是我国北方地区常见的气候现象,其水热条件的反复变化会影响土壤等环境介质的物理化学及生物学性质。冻融过程产生的交替收缩与膨胀可改变土壤结构、水分分布特征,尤其会降低土壤团聚体的稳定性;由于温度、水分、氧化还原等条件的不断变化,冻融过程会促进土壤硝化作用和溶解性有机酸的释放,使土壤微生物量及其活性受到影响,导致土壤pH值、CEC和Ca CO_3含量等随之降低。在冻融过程中,土壤有机质的变化最为明显,反复冻融使有机碳不同程度地暴露和释放,加快了土壤有机碳矿化速率,使土壤可溶性有机碳量增加,最终加剧可溶性有机碳的流失。以往对冻融作用的研究主要集中在自然土壤介质,缺乏对其他环境介质如畜禽粪便等有机固体废弃物的相关报道。在综述冻融过程对土壤物理、化学及生物学性质影响的基础上,提出了未来在一定区域尺度上开展冻融过程对土壤理化性质影响研究,并结合探讨畜禽粪便等有机固体废弃物和土壤污染物的响应机制,为冻融气候条件下土壤污染控制和科学土地利用管理提供科学依据。

关 键 词:冻融过程  土壤  理化性质  生物学性质
收稿时间:2016/8/22 0:00:00

Influence of freeze-thaw process on soil physical, chemical and biological properties: A review
GAO Min,LI Yan-xi,ZHANG Xue-lian,ZHANG Feng-song,LIU Bei,GAO Shi-ying and CHEN Xing-cai.Influence of freeze-thaw process on soil physical, chemical and biological properties: A review[J].Journal of Agro-Environment Science( J. Agro-Environ. Sci.),2016,35(12):2269-2274.
Authors:GAO Min  LI Yan-xi  ZHANG Xue-lian  ZHANG Feng-song  LIU Bei  GAO Shi-ying and CHEN Xing-cai
Institution:State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China,State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China,Beijing Soil and Fertilizer Extension Service Station, Beijing 100029, China,Institute of Geographic Sciences and Natural Resource Research, Beijing 100101, China,State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China,State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China and State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China
Abstract:Freeze-thaw process is a natural phenomenon in Northern China. The fluctuation of hydrothermal conditions may strongly influence soil physiochemical properties, microbial enzymatic activities and total microbial community abundance. The alternating contraction and expansion caused by freeze-thaw process may alter soil structure and water distribution, which especially reduce soil aggregates water stability and bulk density. Because of the fluctuations in soil temperature, water distribution and redox conditions, as a consequence of the freezing-thaw process will accelerate the soil nitrification and release of soluble organic acids. Accordingly, soil pH value, CEC and CaCO3 content will be reduced. The organic matter composition is typically affected during freeze-thaw process. In this process, various forms of organic carbon in soil aggregates will be exposed, dissolved organic matter(DOM) will be released into the aqueous phase and as a result, the soil components absorbed by soil aggregate and organic matter become more mobilized. However, previous studies mainly focused on the effects of freeze-thaw process on natural soils while other types of environmental matrixes have always been neglected. On the basis of previous studies, investigations into the effects of soil pollutants are recommended due to their deep connection with the soil organic components. Furthermore, large amounts of organic solid wastes like animal manure and farm waste have to be used in farmland. The organic wastes change the bulk density, enhance the microbial activity and carbon stock in the soil, protect soil from water erosion should be considered in freeze-thaw process.
Keywords:freeze-thaw process  soil  physicochemical property  biological property
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