The Influence of Rock Fragment Cover on Soil Infiltration Properties

FANG Kai ,ZHENG Jia-xing,ZHANG Li ,LI Zi-chun ,ZHAO Yu

PDF(671 KB)
China Rural Water and Hydropower ›› 2020 ›› (2) : 100-104.

The Influence of Rock Fragment Cover on Soil Infiltration Properties

  • FANG Kai 1 ,ZHENG Jia-xing2 ,ZHANG Li 3 ,LI Zi-chun3 ,ZHAO Yu3
Author information +
History +

Abstract

Soil infiltration is a complicated process, and the rock fragment cover will affect soil infiltration properties. In this paper, the related parameters of soil infiltration properties are analyzed through gravel covering experiment and soil-gravel mixing experiment. The results show that the stable infiltration rate, sorptivety, hydraulic conductivity and soil effective porosity decrease with the increase in gravel coverage soil-gravel mixing degree. In the infiltration of different gravel coverage soil-gravel mixing degree, the variation of relative parameters is significant (P< 0.05). This shows that the effective porosity of the soil decreases with the increase in the gravels, and the water movement channel is so complicated as to limit the infiltration of water. In the soil-gravel mixing experiment, sorptivety, hydraulic conductivity and soil effective porosity decreases sharply with the increase in gravel coverage soil-gravel mixing degree, which is higher than those in the gravel covering experiment. The gravels in the soil can change the soil infiltration properties. Studying the effect of gravel on soil infiltration characteristics further is of practical significance. It is significant to study the possibility of using the rock fragment cover to maintain soil and water for engineering slopes.

Key words

rock fragment cover / soil infiltration properties / soil-gravel mixing / slope protection / soil infiltration rate ;soil hydraulic conductvity / soil infiltration test / soil porosity

Cite this article

Download Citations
FANG Kai ,ZHENG Jia-xing,ZHANG Li ,LI Zi-chun ,ZHAO Yu. The Influence of Rock Fragment Cover on Soil Infiltration Properties. China Rural Water and Hydropower. 2020, 0(2): 100-104

References

[1]李阳兵, 谢德体. 西南岩溶山地生态脆弱性研究[J]. 中国岩溶, 2002,21(1):25-29.
[2]LI X Y. Gravel-sand mulch for soil and water conservation in the semiarid loess region of North West China[J]. Catena, 2003,52(2):105-127.
[3]陈士辉, 谢忠奎, 王亚军, 等. 砂田西瓜不同粒径砂砾石覆盖的水分效应研究[J]. 中国沙漠, 2005,25(3):433-436.
[4]SAUER T J, LOGSDON D. Hydraulic and physical properties of stony soils in a small watershed[J]. Soil science society of america journal, 2002,147(19):889-892.
[5]VERBIST K, BAETENS J, CORNELIS W M, et al. Hydraulic conductivity as influenced by stoniness in degraded drylands of Chile[J]. Soil Science society of america journal, 2009,73(2):471-484.
[6]时忠杰, 王彦辉, 于澎涛, 等. 六盘山森林土壤中的砾石对渗透性和蒸发的影响[J]. 生态学报, 2008,28(12):6 090-6 098.
[7]LIU D D, SHE D L. Can rock fragment cover maintain soil and water for saline-sodic soil slopes under coastal reclamation[J]. Catena, 2017,151:213-224.
[8]TANG S Q, SHE D L. Synergistic effects of rock fragment cover and polyacrylamide application on erosion of saline-sodic soils[J]. Catena, 2018,171:154-165.
[9]佘冬立, 高雪梅, 房凯. 利用圆盘入渗仪测定不同利用类型土壤吸渗率[J]. 农业工程学报, 2014,30(18):151-158.
[10]WOODING R A. Steady infiltration from a circular shallow circular pond [J]. Water resources research, 1968,4(4):1 259-1 273.
[11]HU W, SHAO M G, WANG Q J, et al. Temporal changes of soil hydraulic properties under different land uses [J]. Geoderma, 2009,149(3):355-366.
[12]GARDNER W R. Some steady-state solutions of the unsaturated moisture flow equation with application to evaporation from a water table[J]. Soil science, 1958,85(4):228-232.
[13]REYNOLDS W D, GREGORICH E G, CURNOE W E. Characterisation of water transmission properties in tilled and untilled soils using tension infiltrometers[J]. Soil & tillage research, 1995,33(2):117-131.
[14]周蓓蓓, 邵明安. 不同碎石含量及直径对土壤水分入渗过程的影响[J]. 土壤学报, 2007,44(5):801-807.
[15]佘冬立, 邵明安, 俞双恩. 黄土高原水蚀风蚀交错带小流域土壤矿质氮空间变异性[J]. 农业工程学报, 2010,26(6):89-96.
[16]郭丽俊, 李毅, 李敏, 等. 塿土土壤水力特性空间变异的多重分形分析[J]. 农业机械学报, 2011,42(9):50-58.
[17]朱元骏, 邵明安. 利用圆盘入渗仪推求含碎石土壤饱和水力传导度[J]. 农业工程学报, 2006,22(11):1-5.
[18]李雪垠, 李朝霞, 王天巍, 等. 紫色土中砾石夹层对土壤水分入渗的影响[J]. 水科学进展, 2016,27(5):662-669.
[19]周蓓蓓, 邵明安. 土石混合介质饱和导水率的研究[J]. 水土保持学报, 2006,20(6):62-66.
[20]杨艳芬, 王全九, 曾辰, 等. 土石混合介质水分入渗特性试验研究[J]. 水土保持学报, 2009,23(5):87-90.
[21]COUSIN I, NICOULLAND B, COUTANDEUR C. Influence of rock fragment on the water retention and water percolation in a calcareous soil[J]. Catena, 2003, 53: 97-114.
[22]符素华. 土壤中砾石存在对入渗影响研究进展[J]. 水土保持学报, 2005,19(1):171-175.
PDF(671 KB)

249

Accesses

0

Citation

Detail

Sections
Recommended

/