首页|辽西地区玉米农田土壤水分消退特征及其预测模型研究

辽西地区玉米农田土壤水分消退特征及其预测模型研究

Research on characteristics of soil moisture recession and the development of predictive models for corn fields in western Liaoning province

扫码查看
选用2021 年辽宁西部地区玉米农田3 种质地土壤(中壤土、沙壤土和粘土)的不同降水量级(小雨、中雨、大雨)连续7d、7d后隔日0~50cm土壤相对湿度资料,分析该地区玉米生长期不同降水量级、不同质地土壤水分消退特性和不同土层深度土壤水分消退系数(K)的变化特征,构建土壤水分预报模型.结果表明:辽宁西部地区玉米农田土壤水分消退过程可分为快速消退、缓慢消退、滞缓消退3 个阶段,3 种质地土壤快速消退阶段的平均消退速率为 7.21 mm·d-1,其中,粘土的快速消退速率较其他土质高9%~12%,各土质缓慢消退速率及滞缓消退速率差异不明显.浅层(10~20 cm)K值明显小于其他土层,且离散程度最大,强降雨量级的50 cm土层K值波动幅度明显增大.K值与降水量为显著的负相关关系(R=-0.92).相同降雨量级条件下,粘土的K值小于中壤土和沙壤土,偏小 12%~20%.K值月变化为 3 月最大、8 月最小,11 月末回升至较大值.基于土壤水分平衡方程构建的土壤水分消退模型,小雨量级的模拟精度最好,浅层土壤的模拟结果好于深层.
Three types of soil textures(loam,sandy loam,and clay)from corn fields in western Liaoning province in 2021 were selected,along with different precipitation levels(light rain,moderate rain,and heavy rain)for con-tinuous 7 days and every other day for 7 days after that.The relative soil moisture data for 0~50 cm depth was collected.The characteristics of soil moisture recession for different precipitation levels,soil textures,and soil depth recession coefficients(K)during the corn growing season in this region were analyzed,and a soil moisture predic-tion model was constructed.The results show that the soil moisture recession process in corn fields of western Lia-oning can be divided into three stages:rapid recession,slow recession,and stagnant recession.The average reces-sion rate during the rapid recession stage for the three soil textures was 7.21 mm·d-1,with clay soil having a 9%-12%higher rapid recession rate than other soil textures.There were no significant differences in the slow recession and stagnant recession rates among different soil textures.The K value of the shallow layer(10~20 cm)was sig-nificantly smaller than other soil layers and had the largest dispersion.The fluctuation range of K values in the 50 cm soil layer increased significantly under heavy rainfall conditions.There was a significant negative correlation between K values and precipitation(R=-0.92).Under the same rainfall level,the K value of clay soil was12%-20%lower than that of loam and sandy loam.The monthly variation of K values showed the highest in March,lowest in late August,and rebounded to a relatively high value in late November.Based on the soil moisture bal-ance equation,a soil moisture recession model was constructed.The simulation accuracy was best for light rain lev-els,and the simulation results for shallow soil layers were better than those for deep layers.

Precipitation levelsSoil textureRecession rateSoil moisture balance equation

张兵兵、吕晓、高莉莉、高全、吴航、梁涛、鲁宇超、张方敏、蔡福

展开 >

中国气象局沈阳大气环境研究所,辽宁 沈阳,110166

锦州市生态与农业气象中心,辽宁 锦州 121000

广东省东江流域管理局,广东 广州 516000

南京信息工程大学气象灾害预报预警与评估协同创新中心,江苏 南京 210044

展开 >

降水量级 土壤质地 消退速率 土壤水分平衡方程

2024

气象与环境学报
中国气象局沈阳大气环境研究所

气象与环境学报

CSTPCD
影响因子:1.433
ISSN:1673-503X
年,卷(期):2024.40(6)