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冻融对典型黑土团聚体输移破碎特征的影响

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融雪期的侵蚀外营力主要以冻融和融雪径流为主,该营力可能会影响土壤结构和团聚体稳定性,从而对融雪侵蚀过程产生影响。在融雪期,融雪径流过程会导致团聚体输移破碎,但是关于冻融对团聚体输移破碎的影响研究鲜有报道。本研究以东北典型黑土区5~7和3~5 mm团聚体为对象,分析了不同冻融次数(0、1、5、10、15和20次)下水稳性团聚体组成、平均重量直径(MWD)、标准化平均重量直径(NMWD)和不同冻融次数、不同输移距离(5、10、15、20、25和30 m)下团聚体输移破碎率(BR)及冻融和输移共同作用对BR的贡献度(CT),研究融雪期典型黑土团聚体输移破碎特征。结果表明:5~7和3~5 mm团聚体冻融循环后主要以0。5-1 mm粒径为主,随着冻融次数增加其MWD值总体呈下降趋势,并且在相同冻融次数下3~5 mm团聚体NMWD大于5~7 mm。5~7和3~5mm团聚体随着输移距离的增加BR逐渐增加,尤其是在1次冻融条件下,与未冻融组相比输移距离为5、10、15、20、25和30 m时BR分别显著增加59。7%、32。2%、13。7%、6。2%、13。4%、7。5%和 60。0%、39。0%、18。4%、13。0%、6。3%、6。1%;但随着冻融次数的增加,BR 增加相对缓慢。团聚体输移破碎主要受输移距离(CT=54。6%)和冻融循环(CT=26。2%)的影响,并且冻融循环主要改变团聚体稳定性,进而影响团聚体输移破碎率。可见,在融雪期,冻融循环降低了土壤团聚体稳定性,致使融雪径流过程中团聚体输移破碎严重,土壤更易随水流迁移引发水土流失,因此,应重视该时期的土壤侵蚀及其防治。
Effect of freeze-thaw cycles on aggregate breakdown of typical black soil during transportation
During the snowmelt period,the external erosive forces are dominated by freeze-thaw cycles and snowmelt runoff.These forces may affect soil structure and aggregate stability,thereby influencing snowmelt erosion.The process of snowmelt runoff can lead to the breakdown of aggregates during their transportation.However,few studies examined the effects of freeze-thaw cycles on the breakdown of aggregates during transportation.Focusing on 5-7 and 3-5 mm soil aggregates of typical black soil region in Northeast China,we analyzed the composition of water-stable aggregates,mean weight diameter(MWD),normalized mean weight diameter(NMWD),as well as breakdown rate of soil aggregates(BR)under different freeze-thaw cycles(0,1,5,10,15 and 20 times)and dif-ferent transport distances(5,10,15,20,25 and 30 m).We further investigated the contribution(CT)of both freeze-thaw cycles and transport distances to BR.The results showed that:1)After freeze-thaw cycles,the 5-7 and 3-5 mm aggregates were mainly composed of particles with a diameter of 0.5-1 mm.With increasing frequency of freeze-thaw cycles,the MWD generally showed a downward trend.Moreover,under the same number of freeze-thaw cycles,the NMWD of 3-5 mm aggregates was higher than that of 5-7 mm aggregates.2)As the transport distance increased,the BR of 5-7and 3-5 mm aggregates gradually increased.Compared that under control group,the BR under one freeze-thaw cycle increased by 59.7%,32.2%,13.7%,6.2%,13.4%,7.5%,and 60.0%,39.0%,18.4%,13.0%,6.3%,6.1%at the condition of 5,10,15,20,25 and 30 m transport distances,respectively.However,with increasing frequency of freeze-thaw cycles,the BR increased slowly.3)The breakdown of soil aggregates was mainly influenced by the transport distance(CT=54.6%)and freeze-thaw cycles(CT=26.2%).Freeze-thaw cycles primarily altered the stability of soil aggregates,which in turn affected the BR.Therefore,during the snowmelt period,freeze-thaw cycles reduced the stability of soil aggregates,leading to severe breakdown of soil aggregates during snowmelt runoff process.This made the soil more susceptible to migration with snowmelt runoff,which triggered soil erosion.Therefore,more attention should be paid on the prevention of soil erosion during snowmelt period.

snowmeltfreeze-thaw cycletransportaggregate breakdownblack soil

张茜、马仁明、贾燕锋、范昊明、楚智婷

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沈阳农业大学水利学院,沈阳 110866

辽宁省水土流失防控与生态修复重点实验室,沈阳 110866

融雪期 冻融循环 输移 团聚体破碎 黑土

国家重点研发计划项目

2021YFD1500700

2024

应用生态学报
中国生态学学会 中国科学院沈阳应用生态研究所

应用生态学报

CSTPCD北大核心
影响因子:2.114
ISSN:1001-9332
年,卷(期):2024.35(5)