Effects of Shrub Encroachment on Soil Hydraulic Properties in Alpine Meadow

YIN Xia; LI Dongmei; LI Yi; WANG Ping; LIU Shuying; GAO Yongheng

doi:10.13870/j.cnki.stbcxb.2022.05.017

您当前的位置：

首页 >

文章列表页 >

Effects of Shrub Encroachment on Soil Hydraulic Properties in Alpine Meadow

更新时间：2025-03-12

- Effects of Shrub Encroachment on Soil Hydraulic Properties in Alpine Meadow
- Vol. 36, Issue 5, Pages: 121-129(2022)
- 作者机构：
  
  1. 甘肃农业大学资源与环境学院,兰州,730070
  2. 中国科学院水利部成都山地灾害与环境研究所,成都,610041
  3. 中国科学院成都生物研究所,成都,610041
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2022.05.017
  CLC： S152.7
- Published：2022
- 稿件说明：
移动端阅览
YIN Xia, LI Dongmei, LI Yi, et al. Effects of Shrub Encroachment on Soil Hydraulic Properties in Alpine Meadow[J]. 2022, 36(5): 121-129.
DOI：

YIN Xia, LI Dongmei, LI Yi, et al. Effects of Shrub Encroachment on Soil Hydraulic Properties in Alpine Meadow[J]. 2022, 36(5): 121-129. DOI： 10.13870/j.cnki.stbcxb.2022.05.017.

摘要

全球气候变化背景下

青藏高原高寒草甸灌丛化已经成为青藏高原植被景观的主要变化趋势。为了更好地认识和理解灌丛化与高寒草甸生态系统的关系

以青藏高原东缘川西锦鸡儿(Caragana Erinacea Kom)和金露梅(Potentilla Fruticosa)灌丛化高寒草甸为对象

采用环刀浸泡法和双环入渗法研究了其在未灌丛化、轻度灌丛化、中度灌丛化和重度灌丛化阶段土壤持水和入渗能力特征。结果表明:(1)2种灌丛化草甸土壤容重在中度灌丛化阶段最低

总孔隙度在中度灌丛化阶段最高。(2)随着灌丛化程度的增加

2种灌丛化草甸土壤含水量呈增加趋势

表现为在重度灌丛化阶段最高;土壤毛管持水量、田间持水量和最大持水量呈抛物线变化趋势

在中度灌丛化阶段最大。(3)2种灌丛化草甸土壤的初渗率、稳渗率和入渗速度随灌丛化程度的增加总体表现为增加趋势

其中在中度和重度灌丛化阶段显著高于未灌丛化阶段。(4)相关性分析表明

灌丛化草甸土壤的入渗指标与土壤含水量、非毛管孔隙度有显著相关关系。因此

高寒草甸灌丛化过程中

土壤水力性质的改变通常发生在中度和重度灌丛化阶段。

Abstract

Under the background of global climate change

shrub development of alpine meadow has become the main trend of landscape change in Qinghai-Tibet Plateau.In order to better understand the relationship between shrub and alpine meadow ecosystem

this paper taking shrub alpine meadow of Caragana Erinacea Kom and Potentilla Fruticosa in the eastern margin of the Qinghai-Tibet Plateau as an example

characteristics of soil water holding capacity and infiltration capacity during non-shrub

mild shrub

moderate shrub and severe shrub were studied by using ring knife soaking method and double ring infiltration method. The results showed that: (1) Soil bulk density was the lowest and total porosity was the highest in moderate shrub stage. (2) With the increase of degree of shrub

soil water content of two kinds of shrub meadows showed an increasing trend

and it was the highest in heavy shrub stage. Soil capillary water capacity

field water capacity and maximum water capacity showed a parabolic trend

and maximum water capacity was the highest in moderate shrub stage. (3) The initial infiltration rate

stable infiltration rate and infiltration rate of two kinds of shrub meadow showed an increasing trend with increase of degree of shrub

and infiltration rates in moderate and severe shrub stages was significantly higher than that in non-shrub stage. (4) Correlation analysis showed that soil infiltration index was significantly correlated with soil water content and non-capillary porosity. Therefore

changes of soil hydraulic properties usually occur in moderate and severe shrub stages during alpine meadow shrub development.

关键词

Keywords

references

Carlos E, Guiomar R P, Cristina P, et al. Assessment of remotely sensed near-surface soil moisture for distributed eco-hydrological model implementation[J].Water,2019,11(12):e2613.

邢媛媛,王永东,雷加强.草地灌丛化对植被与土壤的影响[J].干旱区研究,2017,34(5):1157-1163.

Peng H Y. Shrub encroachment with increasing anthropogenic disturbance in the semiarid Inner Mongolian grasslands of China[J].Catena,2013,109(10):39-48.

李巧燕,来利明,周继华,等.鄂尔多斯高原草地灌丛化不同阶段主要植物水分利用特征[J].生态学杂志,2019,38(1):89-96.

Jodi S B. Regime shift on the roof of the world:Alpine meadows converting to shrublands in the southern Himalayas[J].Biological Conservation,2013,46(2):116-127.

Zhao D S, Wu S H, Yin Y H, et al. Vegetation distribution on Tibetan Plateau under climate change scenario[J].Regional Environmental Change,2011,11(4):905-915.

彭海英,童绍玉,李小雁.内蒙古典型草原土壤及其水文过程对灌丛化的响应[J].自然资源学报,2017,32(4):642-653.

He Y H. The relationship between an invasive shrub and soil moisture:Seasonal interactions and spatially covarying relations[J].Isprs International Journal of Geo-Information,2014,3(3):1139-1153.

Guo X X, Fu Q, Hang Y H, et al. Spatial variability of soil moisture in relation to land use types and topographic features on hillslopes in the black soil area of northeast China[J].Sustainability,2020,12(9):e3552.

李小军,高永平.腾格里沙漠东南缘沙质草地灌丛化对地表径流及氮流失的影响[J].生态学报,2012,32(24):7828-7835.

Daniel L P. Woody plants modulate the temporal dynamics of soil moisture in a semi-arid mesquite savanna[J].Ecohydrology,2010,3(1):20-27.

Dirk L, Britta T, Niels B, et al. Prescribed fire as a tool for managing shrub encroachment in semi-arid savanna rangelands[J].Journal of Arid Environments,2014,107(8):49-56.

蔡育蓉.灌丛化草原土壤功能空间异质性及其对放牧的响应[D].北京:中国农业科学院,2021.

杨益帆,胡宗达,李亚非,等.川西亚高山川滇高山栎灌丛地被物与土壤持水性能[J].应用与环境生物学报,2020,26(4):951-960.

聂秀青,熊丰,李长斌,等.青藏高原高寒灌丛生态系统草本层生物量分配格局[J].生态学报,2018,38(18):6664-6669.

Russell L S, William L H. The ecohydrologic significance of hydraulic redistribution in a semiarid savanna[J].Water Resources Research,2008,44(2):564-575.

张镱锂,李炳元,郑度.《论青藏高原范围与面积》一文数据的发表:青藏高原范围界线与面积地理信息系统数据[Z].全球变化科学研究数据出版系统,2014,69:65-68.

张镱锂,刘林山,李炳元,等.青藏高原范围数据集2021与2014年版本比较研究[J].全球变化数据学报,2021,5(3):322-332.

张镱锂,李炳元,刘林山,等.再论青藏高原范围[J].地理研究,2021,40(6):1543-1553.

张镱锂,刘林山,李炳元,等.青藏高原范围数据集2021年版与2014年版比较[Z].全球变化数据学报,2021,5(4):32-42.

张镱锂,任慧霞,潘小多.青藏高原边界数据总集[J].国家青藏高原科学数据中心,2019.

徐翠,张林波,杜加强,等.三江源区高寒草甸退化对土壤水源涵养功能的影响[J].生态学报,2013,33(8):2388-2399.

Liao C, Clark P E, Degloria S D. Bush encroachment dynamics and rangeland management implications in southern Ethiopia[J].Ecology and Evolution,2018,8(23):11694-11703.

吕宸,宫渊波,龚伟,等.川西高寒山地灌丛草甸土壤水文效应特征[J].应用与环境生物学报,2021,27(5):1170-1177.

何露露,庞学勇.川西亚高山4种典型灌丛岛土壤持水能力及其影响因素[J].应用与环境生物学报,2021,27(3):632-638.

赵亚楠,于露,周玉蓉,等.宁夏东部荒漠草原灌丛引入对土壤水分动态及亏缺的影响[J].生态学报,2020,40(4):1305-1315.

彭海英,李小雁,童绍玉.内蒙古典型草原小叶锦鸡儿灌丛化对水分再分配和利用的影响[J].生态学报,2014,34(9):2256-2265.

Li X Y. Soil water and temperature dynamics in shrub-encroached grasslands and climatic implications:Results from inner mongolia steppe ecosystem of north China[J].Agricultural and Forest Meteorology,2013,6(11):20-30.

邹慧,高光耀,傅伯杰.干旱半干旱草地生态系统与土壤水分关系研究进展[J].生态学报,2016,36(11):3127-3136.

赵晶忠,金铭,敬文茂,等.祁连山东段典型灌丛分布区的土壤物理性质[J].林业科技通讯,2020(11):17-20.

Hu X. Influence of shrub encroachment on CT-measured soil macropore characteristics in the inner mongolia grassland of northern China[J].Soil and Tillage Research,2015,150(4):1-9.

李小军.地表径流对荒漠灌丛生境土壤水分空间特征的影响[J].中国沙漠,2012,32(6):1576-1582.

何露露,强薇,张燕,等.川西亚高山针叶林次生演替对土壤持水量的影响[J].应用与环境生物学报,2021,27(3):639-647.

赵维俊,刘贤德,张学龙,等.祁连山西水林区亚高山灌丛土壤入渗性能研究[J].水土保持学报,2015,29(2):106-110.

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.

Views

685

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Influencing Mechanisms of Plant Roots on Soil Preferential Flow in Loess Hilly-Gully Region

Effects of Freeze-Thaw Cycles on the Pore Structure of Alpine Meadow Soils with Different Degrees of Degradation

Soil Infiltration Characteristics and Influencing Factors Under Different Vegetation Cover Types in Dianchi Lake Basin

Field Simulation of Runoff and Sand Production on Degraded and Revegetated Slopes in Alpine Meadows Under Rainfall Conditions

Response of Three-Phase Composition of Soil "Solid-Liquid-Gas" to Altitude and Slope Aspects in Alpine Meadow of the Eastern Qilian Mountains

Related Author

WEN Yongfu

LI Mengzhen

DING Jianchuan

ZHOU Yuchen

GAO Peng

MU Xingmin

HONG Chenze

ZHU Haili

Related Institution

Department of Computer Science， Hebei University of Water Resources and Electric Engineering

Research Center of Soil and Water Conservation and Ecological Environment， Chinese Academy of Sciences and Ministry of Education， Yangling

Hebei Technology Innovation Center for Coastal Wetland Water Resources Allocation and Ecological Protection

Department of Hydraulic Engineering， Hebei University of Water Resources and Electric Engineering

Key Laboratory of Cenozoic Resources and Environment on the Northern Edge of the Qinghai

⁰