globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6369951
论文题名:
冻融循环对五台山典型植被土壤微团聚体的影响
其他题名: Effects of Freeze-thaw Cycles on Soil Micro-aggregates in Typical Vegetations of Wutai Mountain
作者: 李杨波1; 刘楠1; 韩进斌2; 郭勇强2; 李变华2; 申彦科3
刊名: 水土保持通报
ISSN: 1000-288X
出版年: 2018
卷: 38, 期:5, 页码:68-75
语种: 中文
中文关键词: 冻融循环 ; 林线 ; 土壤微团聚体 ; 分形 ; 五台山
英文关键词: freeze-thaw cycles ; timberline ; soil micro-aggregates ; fractal ; Wutai Mountain
WOS学科分类: FORESTRY
WOS研究方向: Forestry
中文摘要: [目的]研究气候变化背景下季节性冻融对土壤微团聚体的作用,为影响林线附近土壤地球生物化学过程的相关研究提供参考。[方法]选择五台山林线附近3种典型植被:草甸、华北落叶松(Larix principis-rupprechtii)和云杉(Picea meyeri)覆盖下的土壤,通过土柱野外原位培养,测定不同时期土壤各粒径微团聚体含量以及土壤分形维数(D)。[结果]在培养期内,3个样地的2~0.25 mm和0.25~0.05 mm团聚体含量变化趋势各不相同;0.05~0.02 mm(先降后增再降),0.02~0.002 mm(先降后增,华北落叶松样地除外),<0.002 mm(先增后降)团聚体含量变化趋势基本一致。在初冻期和融化期,季节性冻融导致3个样地土壤微团聚体含量发生显著变化(p<0.05),深冻期无显著变化(p>0.05)。生长季同样发生了土壤微团聚体含量的显著变化(p<0.05)。不同样地植被组成的差别造成了土壤微团聚体含量差异显著(p<0.05),体现在初冻期和融化期。季节性冻融期间,土壤微团聚体分形维数逐渐增加,而此时云杉样地土壤微团聚体分形维数最低;生长季期间,微团聚体分形维数逐渐降低,草甸样地土壤微团聚体分形维数最低,但在生长季末期,则是华北落叶松样地最低;但3个样地土壤微团聚体分形维数仅在生长季末期存在显著差异(p<0.05),且培养期结束时的土壤分形维数与开始时无显著差异(p>0.05)。[结论]季节性冻融对3个样地土壤微团聚体含量都具有显著影响,且3种植被下土壤结构对季节性冻融的响应也明显不同,主要发生在初冻期和融化期;在培养期内,虽在冻融作用下土壤微团聚体分形维数增加,但进入生长季后都逐渐减少至培养前水平,3个样地土壤结构性和团聚能力均呈周期性变化,具有一定的自我恢复能力。
英文摘要: [Objective]The effect of seasonal freeze-thaw on soil micro-aggregates in the context of climate change was studied in order to provide references for the reserch of soil biochemical processes near the timberline.[Methods]Soil samples from three typical vegetation types(meadow,Larix principis-rupprechtii and Picea meyeri)near the timberline of Wutai Mountain were collected for soil column in situ experiment. Soil micro-aggregates contents and fractal dimensions(D)were measured.[Results]The variations of 2~0.25 mm and 0.25~0.05 mm aggregate contents were different among the three plots.The content of 0.05~0.02 mm aggregate reduced initially,then increased and finally reduced.The content of 0.02~0.002 mm aggregate reduced initially and then increased(except in Larix principis-rupprechtii plot),and the content of<0.002 mm micro-aggregates increased firstly and then reduced.The content of micro-aggregates changed significantly(p<0.05)due to seasonal freeze-thaw events in initial freezing and thawing periods,while there was no significant change in deep freezing period(p>0.05).Soil micro-aggregate contents also changed significantly (p< 0.05)in the growing season.Different vegetation compositions caused significant differences(p<0.05) among micro-aggregate contents in three plots,especially,in initial freezing and thawing periods.During the freezing-thawing period,Dvalues were increased,and that of Picea meyeri plots was the lowest.In growing season,Dvalues were decreased,and that of meadou plots was the lowest.Significant differences(p<0.05) of Dvalues among three researched plots were only observed in the late growing season,and the least D value is obtained in H.principis-rupprechtii.[Conclusion]Freeze-thaw cycles have great impacts on soil micro-aggregate contents.The responses of soil structures to seasonal freeze-thaw events are significantly different, and mainly occur in initial freezing period and thawing period.The D values of all plots are increased by freeze-thaw cycles.Although the D value of soil microaggregates increased during the incubation period,it gradually decreased to the pre-incubation level after entering the growing season.Soil aggregations and structures of all three plots vary periodically and have certain self-recovery capabilities.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/154874
Appears in Collections:气候变化事实与影响

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作者单位: 1.太原理工大学水利科学与工程学院, 太原, 山西 030024, 中国
2.山西省林业厅,山西省五台山树木园, 忻州, 山西 035500, 中国
3.中水北方勘测设计研究有限责任公司, 天津 300220, 中国

Recommended Citation:
李杨波,刘楠,韩进斌,等. 冻融循环对五台山典型植被土壤微团聚体的影响[J]. 水土保持通报,2018-01-01,38(5):68-75
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