Effects of Slope Shape and Vegetation Type on Soil Infiltration on Slope in the Loess Area of Xining Basin

YANG Fucheng; LI Jiangyao; YU Dongmei; LIU Changyi; MIU Xiaoxing; WANG Yanxiu; HU Xiasong; LU Haijing; FU Jiangtao; YAN Cong; HE Weipeng

doi:10.13870/j.cnki.stbcxb.2022.06.005

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Effects of Slope Shape and Vegetation Type on Soil Infiltration on Slope in the Loess Area of Xining Basin

更新时间：2025-03-12

- Effects of Slope Shape and Vegetation Type on Soil Infiltration on Slope in the Loess Area of Xining Basin
- Vol. 36, Issue 6, Pages: 30-40(2022)
- 作者机构：
  
  1. 青海大学地质工程系,西宁,810016
  2. 中国科学院大学,北京,100049
  3. 中国科学院青海盐湖研究所盐湖资源综合高效利用重点实验室,西宁,810008
  4. 青海省盐湖地质与环境重点实验室,西宁,810008
  5. 青海省水土保持中心,西宁,810000
  6. 青海大学农牧学院,西宁,810016
  7. 青海大学农林科学院,西宁,810016
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2022.06.005
  CLC： S157.2
- Published：2022
- 稿件说明：
移动端阅览
YANG Fucheng, LI Jiangyao, YU Dongmei, et al. Effects of Slope Shape and Vegetation Type on Soil Infiltration on Slope in the Loess Area of Xining Basin[J]. 2022, 36(6): 30-40.
DOI：

YANG Fucheng, LI Jiangyao, YU Dongmei, et al. Effects of Slope Shape and Vegetation Type on Soil Infiltration on Slope in the Loess Area of Xining Basin[J]. 2022, 36(6): 30-40. DOI： 10.13870/j.cnki.stbcxb.2022.06.005.

摘要

为进一步探讨青藏高原东北部黄土区草本植物护坡机理

选取西宁盆地长岭沟流域自建试验区

通过设计2种不同坡形和选取适宜当地气候条件生长的3种草本植物

采用野外试验区人工模拟降雨方法

首先分析了坡面土壤水文参数(土壤入渗、坡面土体含水量)分布变化

进而探讨了影响种植草本坡面土壤水分入渗的主要因素与特征

最后对坡面土壤水分入渗过程进行模型模拟与评价。结果表明:种植垂穗披碱草阶梯形边坡产流时间相对最晚

直形裸坡阶段产流量最大

其最大阶段累积径流量在降雨试验40~45 min时

为17 730 mL;2种坡形边坡坡面平均稳定入渗速率由大到小依次为阶梯形种植垂穗披碱草边坡(0.519 mm/min)、直形垂穗披碱草边坡(0.423 mm/min)、直形老芒麦边坡(0.422 mm/min)、直形细茎冰草边坡(0.318 mm/min)、阶梯形裸坡(0.321 mm/min)和直形裸坡(0.192 mm/min)

且种植垂穗披碱草和老芒麦边坡土体含水量在地表以下0—50 cm增幅相对最高

说明种植草本有助于边坡土体内部水分入渗。在此基础上

采用Horton模型、Kostiakov模型和通用经验模型进行坡面土壤水分入渗模拟

结果表明直形边坡土壤水分入渗过程以Horton模型和通用经验模型的拟合效果相对较为理想;阶梯形边坡则以Horton模型得到的土壤水分入渗拟合效果相对最优;最后

通过Pearson相关性分析得出

区内边坡土壤水分入渗特性主要影响因素为土壤有机质与植被覆盖度

且土壤有机质与初始入渗率间呈显著正相关关系(R2为0.986)

植被覆盖度与稳定入渗率间则呈极显著相关关系(R2为0.997)。研究结果对于科学有效防治高寒半干旱区水土流失以及研究不同植被类型及坡形水土保持能力具有理论研究价值和实际指导意义。

Abstract

To further explore the mechanism of slope protection by herbaceous plants in the loess region of northeastern Qinghai-Tibet Plateau

the Changlinggou catchment in Xining Basin was selected as the testing area. By designing two different slope shapes and selecting three herbaceous plants suitable for the local climatic conditions

and using the method of artificial rainfall simulation based on the field experimental area

the distribution and transformation of slope soil hydrological parameters (soil infiltration

soil moisture content) were analyzed first

then characteristics of soil water infiltration and its main influence factors on the slope of planting herbs were discussed. Finally

the process of soil water infiltration on the slope was simulated and evaluated. The results showed that the runoff generation time of the terraced slope planted with Elymus nutans in the area was the latest

and the maximum runoff occurred in straight bare slope

and the maximum stage cumulative runoff was 17 730 mL when the artificial rainfall time was 40~45 min. The average stable infiltration rate of the six different types of slope in the region from large to small was terraced slope planted with E. nutans (0.519 mm/min)

straight slope planted with E. nutans (0.423 mm/min)

straight slope planted with Elymus sibiricus (0.422 mm/min)

straight slope planted with Agropyron trachycaulum (0.318) mm /min)

terraced bare slope (0.321 mm/min)

straight bare slope (0.192 mm/min). The increase of soil moisture content at 0—50 cm below the surface of the slope planted with E. nutans and E. sibiricus were relatively the highest

indicating that planting herbs was conducive to the internal water infiltration of slope soil. On this basis

Horton model

Kostiakov model and general empirical model were used to simulate moisture infiltration on slope. The results showed that Horton model and general empirical model were more suitable for fitting soil moisture infiltration on straight slope. While Horton model was more suitable for fitting soil moisture infiltration process on terraced slope. Pearson correlation analysis showed that soil organic matter and vegetation coverage were the main factors influencing slope infiltration characteristics in the testing area. And initial infiltration rate was significantly and positively correlated with soil organic matter content (R2 was 0.986). And an extremely significant correlation between vegetation coverage and stable infiltration rate was identified (R2 was 0.997). The results of this study had theoretical research value and practical guiding significance for the scientific and effective prevention and control of soil and water loss in alpine and semi-arid areas

and for the study of vegetation types and slope shape soil and water conservation capacity.

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references

李秀春.青海省生态水资源保护措施与改进研究[J].环境科学与管理,2019,44(3):168-172.

张瑜.论加强西宁市水源涵养林建设的思路与对策[J].现代园艺,2021,44(18):181-182.

Valdemir A, Enaiale C de P, Joo A B, et al. Soil and water losses along the cultivation cycle of onion in Irati, Brazil[J].Catena,2021,204:1-7.

Liu B Y, Xie Y, Li Z G, et al. The assessment of soil loss by water erosion in China[J].International Soil and Water Conservation Research,2020,8(4):430-439.

嵇晓雷,杨平.不同降雨强度下植被护坡对边坡位移的影响[J].林业工程学报,2020,5(5):152-156.

龙诚璧,胡伟,李光范,等.热带不同植被边坡水文效应室内模型试验[J].科学技术与工程,2019,19(32):383-388.

Wang D D, Yuan Z J, Cai Y T, et al. Characterisation of soil erosion and overland flow on vegetation-growing slopes in fragile ecological regions: A review[J].Journal of Environmental Management,2021,285:1-6.

于晓杰,魏勇明.不同坡形坡面侵蚀产沙过程的影响研究[J].水土保持研究,2017,7(1):97-100.

靳洋,孙希华,陈凤琴.鲁中山区坡面尺度下的土壤侵蚀特征分析[J].江苏农业科学,2019,47(21):309-312.

Rieke-Zapp D H, Nearing M A. Slope shape effects on erosion: A laboratory study[J].Soil Science Society of America Journal,2005,69(5):1463-1471.

徐勤学,李春茂,陈洪松,等.喀斯特峰丛坡地灌木林地与梯田旱地土壤水分入渗特征[J].农业工程学报,2018,34(8):124-131.

姚单君,任维,王震洪,等.贵阳市花溪河岸喀斯特带地表径流中磷流失和土壤入渗分析[J].山地农业生物学报,2017,36(1):54-60.

郑凯利,邓东周.若尔盖湿地土壤入渗性能及其影响因素[J].水土保持研究,2019,26(3):179-184,191.

Wang J L, Song J Y, Lin H J, et al. Comparison of infiltration models to describe infiltration characteristics of bioretention[J].Journal of Hydro-environment Research,2021,38:35-43.

崔艳红,毕华兴,侯贵荣,等.晋西黄土残塬沟壑区刺槐林土壤入渗特征及影响因素分析[J].北京林业大学学报,2021,43(1):77-87.

Fariba B, Ali A Z, Mohammad R Y, et al. Spatial analysis of infiltration in agricultural lands in arid areas of Iran[J].Catena,2018,170:25-35.

石明章,索生睿,祁栋林.1961—2015年西宁市降水变化特征分析[J].现代农业科技,2018(2):198-200.

许海燕.青海乡土植物园林绿化应用研究进展[J].现代园艺,2020(7):22-23.

王春林.西宁市南北山林木生长量调查及树种选择分析研究[J].现代农业科技,2014(21):151-152,155.

Duan J, Liu Y J, Tang C J, et al. Efficacy of orchard terrace measures to minimize water erosion caused by extreme rainfall in the hilly region of China: Long-term continuous in situ observations[J].Journal of Environmental Management,2021,278:1-15.

陈洪松.黄土区坡地土壤水分运动与转化试验研究[D].陕西杨凌:西北农林科技大学,2003.

王一博,吕明侠,赵海鹏,等.青藏高原多年冻土区活动层土壤入渗特征及机理分析[J].冰川冻土,2021,43(5):1301-1311.

Kostiakov A N. On the dynamics of the coefficient of water-percolation in soils and the necessity for studying it from a dynamic point of view for purposes of amelioration.Transactions of the Sixth Commission of the International Society of Soil Science, Part A, Russian,1932:17-21.

Horton R E. An approach toward a physical interpretation of infiltration-capacity[J].Soil Science Society of America Journal,1941,5:399-417.

Richards L A. Capillary conduction of liquids through porous mediums[J].Physics,1931,1(5):318-333.

李姜瑶,缪晓星,王延秀,等.西宁盆地黄土区不同草本植物和坡形条件下坡面产流产沙特征[J].盐湖研究,2022,30(1):33-45.

曾建辉,李占斌,马波,等.小麦秸秆长度、覆盖量对坡面产流产沙的影响[J].水土保持学报,2020,34(4):98-103,111.

李仕华.梯田水文生态及其效应研究[D].西安:长安大学,2011.

向宇国,张丹,陈凡,等.降雨和坡度对植烟坡耕地产流产沙的影响[J].西南农业学报,2021,34(5):1121-1127.

包含,侯立柱,刘江涛,等.室内模拟降雨条件下土壤水分入渗及再分布试验[J].农业工程学报,2011,27(7):70-75.

樊才睿,张成福,史小红,等.草甸草原不同放牧强度草地土壤水分入渗特征[J].节水灌溉,2020(3):27-31.

赵炯昌,潘岱立,卫伟,等.植被格局对土壤入渗和水沙过程影响的模拟试验研究[J].生态学报,2021,41(4):1373-1380.

张润霞,赵学勇,李晶,等.干旱荒漠区土地利用方式快速转变对土壤入渗性能的影响[J].中国沙漠,2020,40(4):146-153.

李坤,姚文艺,肖培青,等.黄丘区自然草地对坡面土壤入渗的影响机制[J].人民黄河,2017,39(6):82-85,98.

Li Q, Shi X Y, Wu Q Q. Exploring suitable topographical factor conditions for vegetation growth in Wanhuigou catchment on the Loess Plateau, China: A new perspective for ecological protection and restoration[J].Ecological Engineering,2020,158:1-10.

Wei C, Behzad A O, Lei Y K, et al. Studying early stage slope protection effects of vegetation communities for Xinnan Highway in China[J].Ecological Engineering,2018,110:87-98.

刘栋.北京市门头沟地区不同水土保持措施的减水减沙效益[J].水土保持通报,2015,35(4):107-110.

黄锡荃,李慧明,金伯欣.水文学[M].北京:高等教育出版社,1985.

王鑫皓,王云琦,马超,等.根系构型对土壤渗透性能的影响[J].中国水土保持科学,2018,16(4):73-82.

韩冰,吴钦孝,李秧秧,等.黄土丘陵区人工油松林地土壤入渗特征的研究[J].防护林科技,2004(5):1-3,49.

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