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东北黑土区农田土壤风蚀的影响因素及其数量关系
引用本文:林 艺,李和平,肖 波.东北黑土区农田土壤风蚀的影响因素及其数量关系[J].水土保持学报,2017,31(4):44-50.
作者姓名:林 艺  李和平  肖 波
作者单位:1. 中国农业大学资源与环境学院,北京100193;农业部华北耕地保育重点实验室,北京100193;2. 中国农业大学资源与环境学院,北京100193;农业部华北耕地保育重点实验室,北京100193;黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西杨凌712100
基金项目:中央高校基本科研业务费专项(2017QC048)
摘    要:为明确东北黑土区农田土壤风蚀的主要影响因素,通过室内模拟试验,对比分析了黑土在不同风速(5~14m/s)、土壤含水量(2%~11%)以及秸秆覆盖率(0~80%)下的风蚀速率差异,进而分析了风蚀速率与各因素之间的数量关系。结果表明,黑土起沙风速略大于5m/s,其风蚀速率随风速增大呈指数增加,风速14m/s(含水量2%)时的风蚀速率比8m/s时增加了11.6~42.7倍。黑土风蚀速率随土壤含水量升高呈先增加后降低趋势;在土壤含水量小于5%时随含水量升高而逐渐增加,至含水量5%时达到峰值并逐渐降低,至含水量11%时接近零。秸秆覆盖显著降低了黑土风蚀速率,二者成近似指数函数关系;秸秆覆盖率20%(含水量2%)时的风蚀速率比无覆盖减少了72.6%~92.3%,但秸秆覆盖率由20%增加至80%(含水量2%)后风蚀速率仅降低了0.02~1.20g/(m2·s),幅度有限。研究表明,风速、土壤含水量以及秸秆覆盖率均可显著影响东北黑土区农田土壤风蚀速率,其权重依次为风速土壤含水量秸秆覆盖率。

关 键 词:黑土地退化  黑土风蚀  风速  土壤含水量  秸秆覆盖率

Influencing Factors of Wind Erosion and Their Quantitative Relationships with Erosion Rate in Black Soil Area of Northeast China
LIN Yi,LI Heping,XIAO Bo.Influencing Factors of Wind Erosion and Their Quantitative Relationships with Erosion Rate in Black Soil Area of Northeast China[J].Journal of Soil and Water Conservation,2017,31(4):44-50.
Authors:LIN Yi  LI Heping  XIAO Bo
Institution:1.College of Resources and Environmental Sciences, China Agricultural University, Beijing 100193;2.Key Laboratory of Arable Land Conservation in North China, Ministry of Agriculture, Beijing 100193;3.State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Yangling, Shaanxi 712100
Abstract:In order to identify the influencing factors of wind erosion in black soil area of Northeast China,the wind erosion rates of black soil under different wind speeds (5~14 m/s),soil water contents (2%~11%),and straw coverage rates (0 ~ 80%) were measured through a series of simulated wind experiments.Subsequently,the relationships between the wind erosion rate of black soil and the factors were quantitatively analyzed.The results showed that the black soil began to be eroded when the wind speed was slightly greater than 5 m/s,and wind erosion rate of black soil increased exponentially with increasing wind speed.The wind erosion rate under 14 m/s of wind speed (at 2% of soil water content) was 11.6~42.7 times higher than that under 8 m/ s of wind speed.Moreover,the wind erosion rate of black soil increased with the increasing of soil water content when the soil water content was less than 5 %,while it decreased with the increasing of soil water content when the soil water content was between 5 % and 11%.Especially,the wind erosion rate of black soil was close to zero when the soil water content exceeded 11%.In addition,the wind erosion rate of black soil was significantly reduced by straw cover and an exponential relationship was found between them.For instance,the wind erosion rate of black soil with 20% of straw coverage (at 2% of soil water content) was 72.6%~92.3% lower than that of bare land.However,wind erosion rate was only decreased by 0.02~1.20 g/(m2 · s) when the straw coverage increased from 20% to 80% (at 2% of soil water content).In conclusion,wind erosion rate of black soil was significantly affected by wind speed,soil water content,and straw coverage rate in Northeast of China in this study,and their importance in decreasing wind erosion listed in the order of wind speed>soil water content>straw coverage rate.
Keywords:black soil degradation  wind erosion of black soil  wind speed  soil water content  straw coverage rate
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