ISWC OpenIR  > 水保所知识产出(1956---)
黄土区不同生长期大豆坡耕地的入渗特征
王林华1; 马波2; 吴发启3
2015
发表期刊中国水土保持科学
卷号13期号:4页码:15-24
摘要

坡耕地水土流失是土壤侵蚀最为突出的问题。为了研究坡耕地在作物不同生长期内降水土壤水分入渗性
能,选取大豆( Glycine max L. ) 的初花期( R1
) 、末花期( R2
) 、结荚期( R4
) 、始粒期( R5
) 的坡耕地为研究对象,并以裸
坡为对照( CK) ,通过人工模拟降雨实验方法,分析其入渗过程及特征,并用Horton 和Kostiakov 入渗模型对入渗过
程模拟。结果表明: 不同降雨强度和坡度条件下,大豆各生长期的坡地与裸坡的初始入渗率、稳定入渗率、累计入
渗量和入渗补给系数总体呈现出R5 > R4 > R2 > R1 > CK 的变化趋势; 采用的Horton 和Kostiakov 2 个入渗模型拟合
效果较好,且能反映大豆坡耕地在不同生长期的降水入渗过程及其特征,二者的拟合优度都比较高,其中Horton 模
型的拟合效果优于Kostiakov 模型。

其他摘要

Soil erosion in sloping farmland is a key ecological and environmental issue that threats the
sustainable agricultural development on the Loess Plateau of China. Knowledge of infiltration process is
crucial for understanding and managing hydrological processes and soil erosion in sloping farmland. The
objective of this study was to clarify the infiltration characteristics in sloping farmland at different stages of
crop growth. The soybean ( Glycine max L. ) was selected as our research object and its growth was
divided into four stages: initial flowering stage ( R1
) ,late flowering stage ( R2
) ,pod bearing stage
( R4
) ,and maturity starting stage ( R5
) . The bare sloping farmland was set as control ( CK) . Runoff
from experimental plots was collected under the simulated rainfall condition,the infiltration processes and
characteristics were analyzed,and the infiltration processes were simulated with the Horton and Kostiakov
infiltration models. The following results were obtained. For the four growth stages of soybean,
parameters such as initial infiltration rate,stable infiltration rate,cumulative infiltration amount and
infiltration recharge coefficient presented generally the order as R5 > R4 > R2 > R1 > CK at different
rainfall intensities and slope gradients. The recharge coefficient increased with growth stages butdecreased with slope gradient. The crop coverage was the important factor for determining the recharge
coefficient. Simulated infiltration processes with Horton and Kostiakov models showed that two models fit
well with the infiltration and could reflect the infiltration characteristics while the fitting effect of Horton
was better than Kostiakov. The results of our study are helpful for better understanding of the infiltration
processes and characteristics in sloping farmland during the crop growth stages.

关键词生长期 黄土高原 入渗特征 坡耕地
收录类别中文核心期刊要目总览
语种中文
文献类型期刊论文
条目标识符sbir.nwafu.edu.cn/handle/361005/9705
专题水保所知识产出(1956---)
作者单位1.西北农林科技大学水土保持研究所
2.中国科学院水利部水土保持研究所
3.西北农林科技大学资源环境学院
推荐引用方式
GB/T 7714
王林华,马波,吴发启. 黄土区不同生长期大豆坡耕地的入渗特征[J]. 中国水土保持科学,2015,13(4):15-24.
APA 王林华,马波,&吴发启.(2015).黄土区不同生长期大豆坡耕地的入渗特征.中国水土保持科学,13(4),15-24.
MLA 王林华,et al."黄土区不同生长期大豆坡耕地的入渗特征".中国水土保持科学 13.4(2015):15-24.
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