PDF DownloadHTML ]" id="html" rel="external">HTML
[1]ZHANG Yuhua,ZHOU Beibei,CHEN Xiaopeng,et al.Effect of Nano Carbon on Soil Moisture Movement Characteristics in the Loess Slope Based on Hydrus Simulation[J].Research of Soil and Water Conservation,2020,27(01):132-138.
Copy

Effect of Nano Carbon on Soil Moisture Movement Characteristics in the Loess Slope Based on Hydrus Simulation

References:
[1] 李健,陈海迟.黄土丘陵区坡面水土流失规律研究[J].干旱区资源与环境,1996,10(1):71-76.
[2] 田卫堂,胡维银,李军,等.我国水土流失现状和防治对策分析[J].水土保持研究,2008,15(4):204-209.
[3] 吴江琪,马维伟,李广,等.黄土高原4种植被类型对土壤物理特征及渗透性的影响[J].水土保持学报,2018,32(4):133-138.
[4] Yi C Q, Fan J. Application of HYDRUS-1D model to provide antecedent soil water contents for analysis of runoff and soil erosion from a slope on the Loess Plateau[J]. Catena, 2016,139:1-8.
[5] 刘小璐,鲁克新,李鹏,等.不同降雨条件下坡面土壤水分入渗过程研究与模拟[J].干旱区资源与环境,2018,32(11):114-118.
[6] 董起广.基于HYDRUS的黄土高原丘陵沟壑区土壤水分入渗模拟[J].节水灌溉,2018(8):90-92,98.
[7] 陈晓鹏.纳米碳对黄土区水土流失及养分运移特征的影响研究[D].西安:西安理工大学,2018.
[8] Karandish F,im/unek J. An application of the water footprint assessment to optimize production of crops irrigated with saline water:A scenario assessment with HYDRUS[J]. Agricultural Water Management, 2018,208:67-82.
[9] 荐圣淇,赵传燕,彭焕华,等.利用染色示踪与图像处理术研究根系对土壤大孔隙的影响[J].兰州大学学报:自然科学版,2011,47(5):62-66.
[10] 吕金榜,周蓓蓓,王全九.地表下纳米碳混合层对土壤入渗过程的影响[J].水土保持学报,2016,30(2):126-130.
[11] 陈风琴,石辉.缙云山常绿阔叶林土壤大孔隙与入渗性能关系初探[J].西南师范大学学报:自然科学版,2005,30(2):350-353.
Similar References:

Memo

-

Last Update: 2020-02-25

Online:11674       Total Traffic Statistics:27385545

Website Copyright: Research of Soil and Water Conservation Shaanxi ICP No.11014090-10
Tel: 029-87012705 Address: Editorial Department of Research of Soil and Water Conservation, No. 26, Xinong Road, Yangling, Shaanxi Postcode: 712100