Spatial Distribution Characteristics of Soil Moisture on Tea Garden Slope and Its Response to Rainfall Replenishment in the Three Gorges Reservoir Area

LI Xueting; LIU Muxing; LU Shiguo; WANG Weijie; YI Jun; WAN Jinhong

doi:10.13870/j.cnki.stbcxb.2023.05.017

您当前的位置：

首页 >

文章列表页 >

Spatial Distribution Characteristics of Soil Moisture on Tea Garden Slope and Its Response to Rainfall Replenishment in the Three Gorges Reservoir Area

更新时间：2025-03-12

- Spatial Distribution Characteristics of Soil Moisture on Tea Garden Slope and Its Response to Rainfall Replenishment in the Three Gorges Reservoir Area
- Vol. 37, Issue 5, Pages: 137-144(2023)
- 作者机构：
  
  1. 地理过程分析与模拟湖北省重点实验室,武汉,430079
  2. 华中师范大学城市与环境科学学院,武汉,430079
  3. 中国水利水电科学研究院水利史研究所,北京,100038
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2023.05.017
  CLC： S152.7
- Published：2023
- 稿件说明：
移动端阅览
LI Xueting, LIU Muxing, LU Shiguo, et al. Spatial Distribution Characteristics of Soil Moisture on Tea Garden Slope and Its Response to Rainfall Replenishment in the Three Gorges Reservoir Area[J]. 2023, 37(5): 137-144.
DOI：

LI Xueting, LIU Muxing, LU Shiguo, et al. Spatial Distribution Characteristics of Soil Moisture on Tea Garden Slope and Its Response to Rainfall Replenishment in the Three Gorges Reservoir Area[J]. 2023, 37(5): 137-144. DOI： 10.13870/j.cnki.stbcxb.2023.05.017.

摘要

利用高频率(5 min)的土壤水分探针和自动气象站监测三峡库区典型茶园坡面与林地坡面的土壤水分变化过程及其对降雨的响应

明确了林地和茶园土壤水分变化的规律

揭示了土地利用方式和微地形对土壤水分和降雨储蓄的影响机制。结果表明:(1)在时间上

茶园和林地土壤含水率随降雨量的变化而改变

土壤含水率随土层深度呈现"W"型和"S"型变化。土壤含水率年内变异系数随着土层深度的增加而降低

表层土壤(10 cm)含水率为中等变异水平(10%p<0.05)

砂粒比表面积小

保水性差

因此林地各坡位储水量明显大于茶园。(3)坡位对林地和茶园土壤水分的影响体现为上坡土壤水分的季节变化幅度小于中下坡

在80-120 cm土层表现最明显

上坡80-120 cm土层水分较稳定

而中下坡80-120 cm土层水分波动较大。坡位对储水量补给量的影响表现为下坡补给量大于中上坡。(4)Pearson相关分析表明

林地和茶园各坡位土壤水分补给量与降雨量呈显著正相关关系(p<0.01)

且线性回归结果表明

决定系数(R)除茶园上坡外均大于0.81

说明土壤水分补给量和降雨量的拟合度较好。研究结果可为山地丘陵区茶园坡面降水资源的合理利用和区域水土流失治理提供参考。

Abstract

High frequency (5 min) soil moisture probes and automatic weather stations were used to monitor the soil moisture change process and its response to rainfall on typical tea garden slopes and woodland slopes in the Three Gorges Reservoir Area. The regularity of soil moisture change in woodland and tea garden was clarified

and the impact mechanism of land use patterns and microtopography on soil moisture and rainfall storage was revealed. The results indicated that:(1) The soil moisture of the tea garden and woodland varied with the rainfall

and the soil moisture of woodland and tea garden varied with the depth in "W" and "S" shape

respectively. The annual variation coefficient of soil moisture decreased with the increasing of soil depth. The change of water content was at moderate level (10% < CV < 100%) in surface soil (10 cm)

while it was at a weak variation level (0< CV < 10%) in deep soil (20-120 cm). (2) Furthermore

the results of One-way ANOVA showed that sand content in tea garden was significantly greater than that in woodland (p<0.05)

while the clay content was less than that in woodland. The specific surface area of sand particles was small

and the water retention was poor. Therefore

the water storage capacity of each slope of woodland was obviously greater than that of tea garden. (3) The influences of slope position on soil moisture in woodland and tea garden were similar. Specifically

the seasonal variation of soil moisture on upper slope was smaller than that on middle and lower slopes

and was most evident in the 80-120 cm soil layer. The water content of the 80-120 cm soil layer on the upper slope was relatively stable

while it changed dramatically on middle and lower slopes. The impact of slope position on water storage recharge was shown as the recharge amount on the lower slope was greater than that on the middle and upper slopes. (4) Pearson correlation analysis showed that the soil water supplementary amount and rainfall were in a significant (p<0.01) positive correlation in tea garden and woodland. And the linear regression results showed that the determination coefficient R was greater than 0.81 except for the upper slope of tea garden

indicating a good fit between soil water supplementary and rainfall. These results could provide reference for the rational utilization of rainfall resources on tea garden slopes and regional soil erosion control in mountainous and hilly areas.

关键词

Keywords

references

高露,张圣微,朱仲元,等.干旱半干旱区退化草地土壤水分变化及其对降雨时间格局的响应[J].水土保持学报,2020,34(1):195-201.

陈伟,李亚新,王红阳,等.黄土丘陵区坡耕地与撂荒地土壤水分对降雨的响应特征[J].生态学报,2022,42(1):332-339.

Seneviratne S I, Corti T, Davin E L, et al. Investigating soil moisture-climate interactions in a changing climate:A review[J].Earth-Science Reviews,2010,99(3/4):125-161.

冯博.黄土高原北部两种典型草地土壤水分时空分异及对降雨的响应[D].沈阳:沈阳农业大学,2020.

Daly E, Porporato A. A review of soil moisture dynamics:From rainfall infiltration to ecosystem response[J].Environmental Engineering Science,2005,22(1):9-24.

周怡雯,戴翠婷,杜映妮,等.三峡库区典型茶园土壤水分对不同降雨模式的响应[J].生态学报,2023,43(3):1267-1275.

刘宏伟,余钟波,崔广柏,等.湿润地区土壤水分对降雨的响应模式研究[J].水利学报,2009,40(7):822-829.

Zhu Q, Nie X F, Zhou X B, et al. Soil moisture response to rainfall at different topographic positions along a mixed land-use hillslope[J].Catena,2014,119:61-70.

吴远菲,肖培青,郝仕龙,等.黄丘区典型灌木和荒草地土壤含水量变化对降雨的响应[J].水土保持研究,2022,29(4):121-126.

中华人民共和国生态环境部.2017年长江三峡工程生态与环境监测公报[R].北京:2017.

黄道友,王克林,黄敏,等.我国中亚热带典型红壤丘陵区季节性干旱问题研究[J].生态学报,2004,24(11):2516-2523.

彭廷柏.我国中亚热带东部地区农业生态类型成因与发展机制研究[M].北京:科学出版社,1994.

陈玉真,王峰,吴志丹,等.林地转变为茶园对土壤理化性质的影响[J].茶叶学报,2018,59(4):205-210.

Gutierrez-Lopez J, Asbjornsen H, Helmers M, et al. Regulation of soil moisture dynamics in agricultural fields using strips of native prairie vegetation[J].Geoderma,2014,226/227:238-249.

Feng H H, Liu Y B. Trajectory based detection of forest-change impacts on surface soil moisture at a basin scale Poyang Lake Basin,China[J].Journal of Hydrology,2014,514:337-346.

张甘霖,龚子同.土壤调查实验室分析方法[M].北京:科学出版社,2012.

田卓,何建华,张帅普,等.龙脊梯田典型坡面表层土壤水分的空间变异特征[J].西南农业学报,2021,34(10):2197-2203.

印家旺,阿拉木萨,苏宇航,等.科尔沁沙地不同土地利用类型土壤入渗特征比较研究[J].水土保持通报,2022,42(4):90-98.

常颖,秦富仓.希拉穆仁草原坡度对土壤入渗规律影响试验研究[J].北京农业,2013(21):196-197.

赵丹阳,毕华兴,侯贵荣,等.晋西黄土区典型林地土壤水分变化特征[J].水土保持学报,2021,35(1):181-187.

张梦雅,马育军,谢婷.青海湖流域生长季土壤水分空间分布特征研究.水利水电技术(中英文),2022:1-15. (2022-08-17). https://kns.cnki.net/kcms/detail/10.1746.TV.20220816.1410.002.html.

王艳莉,刘立超,高艳红,等.人工固沙植被区土壤水分动态及空间分布[J].中国沙漠,2015,35(4):942-950.

张海林,杨秀锋,易军,等.亚热带红壤区不同土地利用方式下的土壤剖面水流特征[J].水土保持学报,2019,33(6):233-241.

刘营营,佘冬立,刘冬冬,等.土地利用与土壤容重双因子对土壤水分入渗过程的影响[J].水土保持学报,2013,27(5):84-88,94.

Zhang J Y, Duan L M, Liu T X, et al. Experimental analysis of soil moisture response to rainfall in a typical grassland hillslope under different vegetation treatments[J].Environmental Research,2022,213:e113608.

Fu B J, Wang J, Chen L D, et al. The effects of land use on soil moisture variation in the Danangou Catchment of the Loess Plateau, China[J].Catena,2003,54(1/2):197-213.

Zhu Y J, Shao M G. Variability and pattern of surface moisture on a small-scale hillslope in Liudaogou Catchment on the northern Loess Plateau of China[J].Geoderma,2008,147(3/4):185-191.

姚雪玲,傅伯杰,吕一河.黄土丘陵沟壑区坡面尺度土壤水分空间变异及影响因子[J].生态学报,2012,32(16):4961-4968.

王鹏祥,朱清科,申明爽,等.陕北黄土区陡坡微地形土壤水分对降雨的响应[J].干旱区资源与环境,2020,34(8):167-172.

冯伟,杨文斌,党宏忠,等.毛乌素沙地流动沙丘土壤水分对降雨的响应[J].中国沙漠,2015,35(2):400-406.

Views

969

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Spatial Variation Characteristics of Soil Moisture in the Three Gorges Mountain Catchment Area of the Yangtze River

Soil Moisture Variation Characteristics of Different Land Use Types in the Moderate Slope Sandy Area of Loess Hilly Region

Soil Moisture Retrieval Under Different Land Use Types in the Loess Area Using Electrical Resistivity Tomography

Regulation Mechanism of Rainstorm Intensity and Process on Soil Moisture Deficit in the Edge Zones of Weibei Rainfed Plateau

Influence of Stem Diameter of Hedgerow-Grass Ditch System on Sediment Particle Size and Nitrogen and Phosphorus Transport in Purple Soil Areas under Simulated Rainfall

Related Author

HU Lexin

LIU Muxing

ZHAO Lu

YI Jun

ZHANG Hailin

WAN Jinhong

ZHANG Min

LIU Shuang

Related Institution

Hubei Key Laboratory for Geographical Process Analyzing&Modeling

Institute of Water Conservancy History, China Academy of Water Resources and Hydropower Sciences

Institute of Loess Plateau,Shanxi University

College of Environment and Resource Sciences, Shanxi University

State Key Laboratory of Soil and Water Conservation and Desertification Control， Northwest A&F University， Yangling

⁰