Soil surface evaporation processes under mulches of different sized gravel

被引:109
作者
Yuan, Cuiping [1 ]
Lei, Tingwu [1 ,2 ]
Mao, Lili [1 ]
Liu, Han [1 ]
Wu, Yang [1 ]
机构
[1] China Agr Univ, Coll Water Conservancy & Civil Engn, Beijing 100083, Peoples R China
[2] Chinese Acad Sci, State Key Lab Soil Eros & Dryland Farming Loess P, Inst Soil & Water Conservat, Yangling 712100, Peoples R China
关键词
Gravel mulch; Soil surface evaporation; Gravel size; WATER;
D O I
10.1016/j.catena.2009.03.002
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
To reduce water loss from soil surface evaporation is important in agricultural and environmental practices, especially in arid and semi-arid regions. Gravel mulch has long been practiced to reduce soil surface evaporation. In this study, a series of simulation experiments were conducted to study the effects of gravel mulches of different sizes on evaporation process from soil surface. Four mulch treatment levels were used: diameter 0.5 cm (A), diameter 2.5 cm (B), diameter 4.5 cm (C), and bare soil (CK), with three replicates. It was found that the gravel mulches dramatically reduced the evaporation from bare soil surface, particularly when soil water contents were at high levels. Under the same soil water content, the evaporation reduction rates under gravel mulches were negatively correlated with gravel sizes. The evaporation processes under gravel mulches were much more stable as compared with that from bare soil surface. The ratio of the soil surface evaporation to the atmospheric evaporation (E-ss/E-sa) and soil water contents with no mulch decreased rapidly with time. Soil water contents decreased slowly with time under mulches while the E-ss/E-sa values maintained at the more or less stable levels. During the successive evaporation process of 41 days, the cumulative soil surface evaporation under mulches was linearly correlated with time but that from bare soil surface was logarithmically correlated with time. (C) 2009 Published by Elsevier B. V.
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页码:117 / 121
页数:5
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