Morphological Distribution Characteristics of Preferential Flow in Red Soil of Forest and Grassland in Arid and Hot Valley of Honghe River

Zhu Mengxue; Zhao Yangyi; Duan Xu; Wang Keqin; Wan Yanping; Lu Huaxing; Qiu Yanhai; Du Yunxiang

doi:10.13961/j.cnki.stbctb.2021.04.002

您当前的位置：

首页 >

文章列表页 >

Morphological Distribution Characteristics of Preferential Flow in Red Soil of Forest and Grassland in Arid and Hot Valley of Honghe River

- Morphological Distribution Characteristics of Preferential Flow in Red Soil of Forest and Grassland in Arid and Hot Valley of Honghe River
- Bulletin of Soiland Water Conservation Vol. 41, Issue 4, Pages: 9-16(2021)
- 作者机构：
  
  1. 西南林业大学生态与环境学院,云南,昆明,650224
  2. 国家林业和草原局云南玉溪森林生态系统国家定位观测研究站,云南,昆明,650224
  3. 新平彝族傣族自治县水利局,云南,玉溪,653400
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2021.04.002
  CLC： S714.2
- Published：2021
- 稿件说明：
移动端阅览
Zhu Mengxue, Zhao Yangyi, Duan Xu, et al. Morphological Distribution Characteristics of Preferential Flow in Red Soil of Forest and Grassland in Arid and Hot Valley of Honghe River[J]. Bulletin of Soiland Water Conservation, 2021, 41(4): 9-16.
DOI：

Zhu Mengxue, Zhao Yangyi, Duan Xu, et al. Morphological Distribution Characteristics of Preferential Flow in Red Soil of Forest and Grassland in Arid and Hot Valley of Honghe River[J]. Bulletin of Soiland Water Conservation, 2021, 41(4): 9-16. DOI： 10.13961/j.cnki.stbctb.2021.04.002.

摘要

[目的

]

在红河干热河谷地区开展优先流形态分布特征及与红壤特性关系的研究，为区域水资源管理和防治水土流失等工作提供理论依据。[方法

]

以干热河谷地区典型植被林地和荒草地为研究对象，采用野外染色示踪法并结合图像处理技术研究优先流的形态分布特征及对红壤特性响应。[结果

]

①林草地上层剖面平均染色面积分别为87.20%和91.97%，染色面积随土层的增加而减小，局部深度内染色面积出现反弹现象；林草地优先流长度指数分别为766.8%和730.0%，林地土壤优先流较荒草地发达；林草地的最大染色深度分别为40 cm和35 cm；②染色路径宽度随土层的增加而减小，0—20 cm土层内以大于250 mm的路径为主，20—40 cm内的染色路径在20—250 mm，而在40 cm以下的土层染色路径集中在20 mm以内；③优先流染色面积比、长度指数、染色路径宽度与土壤因子存在显著相关性，总孔隙度、有机质、含水率等对染色面积比（D

）、长度指数（LI）、染色路径宽度（SPW）累积贡献率分别为97.80%，86.95%，87.45%；含水率、有机质、容重、总孔隙度和Al

等因子与染色面积比、染色路径宽度呈最优线性关系。[结论

]

土壤的孔隙特性、盐基离子和土壤质地等的共同作用最终导致红河干热河谷林草地优先流的差异。

Abstract

[Objective] The preferential flow morphology and characteristics of red soil in the arid and hot valley of the Honghe River was studied

in order to provide theoretical basis for regional water resources management and soil erosion prevention. [Methods] Taking typical vegetation—woodlands and wild grasslands in arid and hot valley regions as the research objects

the morphological distribution characteristics of preferential flow and its response to the characteristics of read soil were studied by using field dye tracing method and image processing technology. [Results] ① The average stained area of forest and grassland was 87.2% and 91.97% respectively. The stained area decreased with the increase of soil layer

and rebounded in local depths. The preferential flow length index of forest and grassland was 766.8% and 730.0% respectively. And the priority flow of the forest was more developed than wasteland. The maximum staining depth of forest and grassland was 40 cm and 35 cm respectively. ② The width of the dyeing path decreases with the increase of the soil layer. In the 0—20 cm soil layer

the main dyeing path was greater than 250 mm. The dyeing path within 20—40 cm was mainly in the layer between 20—250 mm

and the dyeing path was less than 20 mm in the soil layer below 40 cm. ③ There were significant correlations between the priority flow dyeing area

length index

dyeing path width and soil factors. The cumulative contribution rate of total porosity

organic matter

and moisture content to dyeing area ratio (DA)

length index (LI) and dyeing path width (SPW) was 97.8%

86.95%

87.45%

respectively. The factors such as moisture content

organic matter

bulk density

total porosity and Al3+ had the best linear relationship with dyeing area and dyeing path. [Conclusion] The combined effects of soil pore characteristics

base ions

and soil texture ultimately led to the difference in preferential flow between forest and grassland in the arid and hot valley of the Honghe River.

关键词

Keywords

references

金振洲.滇川干热河谷种子植物区系成分研究[J].广西植物, 1999, 19(1):1-14.

刘方炎, 李昆, 孙永玉, 等. 横断山区干热河谷气候及其对植被恢复的影响[J].长江流域资源与环境, 2010, 19(12):1386-1391.

孔继君, 谷丽萍, 郭永清, 等. 元谋干热河谷生态恢复示范区土壤养分状况调查[J].西部林业科学, 2017, 46(6):108-112.

岳学文.金沙江干热河谷不同土地利用方式的土壤水分特征[J].安徽农业科学, 20120, 38(27):14963-14965.

赵元蛟, 苏文华, 张光飞, 等. 云南元谋干热河谷土壤水分季节动态[J].安徽农业科学, 2013, 41(8):3593-3594.

段爱国, 张建国, 张俊佩, 等. 干热河谷主要植被恢复树种水分利用效率动态分析[J].北京林业大学学报, 2010, 32(6):13-19.

Dekker L W, Ritsema C J, Wendroth O, et al. Moisture distributions and wetting rates of soils at experimental fields in the Netherlands, France, Sweden and Germany[J]. Journal of Hydrology, 1999, 215(1).4-22.

Jarvis N. Modeling the Impact of Preferential Flow on Nonpoint Source Pollution[C]//Physical Nonequilibrium in Soils. Ann Arbor Press, 1988.

程金花, 张洪江, 史玉虎, 等. 长江三峡花岗岩地区优先流对渗流和地表径流的作用[J].水土保持通报, 2007, 27(2):18-23.

李伟莉, 金昌杰, 王安志, 等. 长白山主要类型森林土壤大孔隙数量与垂直分布规律[J].应用生态学报, 2007, 18(10):2179-2184.

Karup D, Moldrup P, Paradelo M, et al. Water and solute transport in agricultural soils predicted by volumetric clay and silt contents[J]. Journal of Contaminant Hydrology, 2016, 192(5):194-202.

张英虎, 牛健植, 朱蔚利, 等. 森林生态系统林木根系对优先流的影响[J].生态学报, 2015, 35(6):1788-1797.

王岩, 陈友媛, 彭昌盛, 等. 初始含水量对黄河口潮滩溶质优先运移的影响研究[J].海洋环境科学, 2011, 30(3):310-315.

吕刚, 金兆梁, 凌帅, 等. 浑河源头水源涵养林土壤优先流特征[J].水土保持学报, 2019, 33(4):287-292.

Judit G H, Flury M. Sorption of brilliant blue FCF in soils as affected by pH and ionic strength[J]. Geoderma, 2000, 97(1):87-101.

骆紫藤, 牛健植, 孟晨, 等. 华北土石山区森林土壤中石砾分布特征对土壤大孔隙及导水性质的影响[J].水土保持学报, 2016, 30(3):305-308, 316.

刘目兴, 聂艳, 于婧, 等. 不同初始含水率下粘质土壤的入渗过程[J].生态学报, 2012, 32(3):871-878.

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, 165(6):235-243.

邵一敏, 赵洋毅, 段旭, 等. 基于分形分析的干热河谷区典型地类土壤优先路径分布特征[J].西北农林科技大学学报(自然科学版), 2020, 48(7):102-112.

Nathan W H, Bhabani S, Das P, et al. Dual-domain solute transfer and transport processes:Evaluation in batch and transport experiments[J]. Journal of Contaminant Hydrology, 2004, 75(3):257-280.

Pietro L D, Stephane Ruy, Capowiez Y. Predicting preferential water flow in soils by traveling-dispersive waves[J]. Journal of Hydrology, 2003, 278(1):64-75.

Anderson S H, Peyton R l, Gantzer C J. Evaluation of constructed and natural soil macropores using X-ray computed tomography[J]. Geoderma, 1990, 19(18):97-100.

Feng Jie, Hao Zhenchun. Distribution of soil macropores characterized by CT[J]. Advances in Water Science, 2002, 13(5):611-617.

Vanclooster M, Mallants D, Diels J, et al. Determining local-scale solute transport parameters using time domain reflectometry (TDR)[J]. Journal of Hydrology, 1993, 148(1/4)93-107.

Cheng Jinhua, Zhang Hongjiang, Wang Wei, et al. Changes in preferential flow path distribution and its affecting factors in Southwest China[J]. Soil Science, 2011, 176(12):652-660.

马思文, 张洪江, 程金花, 等. 三峡库区典型城郊防护林土壤饱和导水率特征研究[J].南京林业大学学报(自然科学版), 2018, 42(5):99-106.

Akhtar M S, Richards B K, Medrano P A, et al. Dissolved phosphorus from undisturbed soil cores:Related to adsorption strength, flow rate, or soil structure[J]. Soil Science Society of America Journal, 2003, 67(2):458-470.

Shaw J N, West L T, Radcliffe D E, et al. Preferential flow and pedotransfer functions for transport properties in sandy Kandiudults[J]. Soil Science Society of America Journal, 2000, 64(2):670-678.

李振东, 朱彦光, 陈晓冰, 等. 桂北岩溶区典型农地土壤优先流特征[J].水土保持研究, 2019, 26(5):68-74, 80.

刘伟, 杨涛, 艾志强, 等. 2种土地利用方式下红壤优先流特征及其对氮运移的影响[J].安徽农业科学, 2019, 47(24):100-102, 169.

胡琦, 李仙岳, 史海滨, 等. 基于染色示踪的农膜残留农田土壤优先流特征[J].水土保持学报, 2020, 34(3):142-149.

Lv Gang, Li Jun, Li Yexin, et al. Preferential flow characteristics of reclaimed mine soils in a surface coal mine dump[J]. Environmental Monitoring and Assessment, 2017, 189(6):266.

Morales V L, Parlange J Y, Steenhuis T S. Are preferential flow paths perpetuated by microbial activity in the soil matrix:A review[J]. Journal of Hydrology, 2009, 393(1):29-36.

陈婷婷, 段旭, 赵洋毅, 等. 红河干热河谷区典型地类植物根系特征对土壤大孔隙的影响[J].水土保持研究, 2020, 27(6):107-115.

王伟.三峡库区紫色砂岩林地土壤优先流特征及其形成机理[D].北京:北京林业大学, 2011.

陈晓冰.重庆四面山4种土地利用类型土壤优先流特征研究[D].北京:北京林业大学, 2016.

聂立水, 王登芝.土壤分析[M].北京:中国林业出版社, 2019.

Weiler M, Naef F. An experimental tracer study of the role of macropores in infiltration in grassland soils[J]. Hydrological Processes, 2003, 17(2):477-493.

魏虎伟, 程金花, 杜士才, 等. 利用染色示踪法研究四面山两种林地优先路径分布特征[J].水土保持通报, 2015, 35(2):193-197, 204.

刘目兴, 杜文正.山地土壤优先流路径的染色示踪研究[J].土壤学报, 2013, 50(5):871-880.

朱钊岑, 刘冰, 刘婵, 等. 荒漠绿洲湿地土壤优先流与水分入渗特征[J].生态学报, 2020, 40(12):3979-3990.

Alaoui A, Lipiec J, Gerke H. A review of the changes in the soil pore system due to soil deformation:A hydrodynamic perspective[J]. Soil & Tillage Research, 2011, 115(6):1-15.

张东旭, 程金花, 王伟.鹤大高速(G11)低路基边坡土壤优先流特征[J].水土保持学报, 2016, 30(5):76-81.

程金花, 张洪江, 史玉虎.三峡库区花岗岩林地土壤特性与"优先路径"的关系[J].中国水土保持科学, 2005, 3(1):97-101.

陈晓冰, 张洪江, 李世友, 等. 紫色砂岩区不同植被类型土壤优先流特征及其影响因素[J].中国水土保持科学, 2014, 12(6):42-49.

Bogner C, Borken W, Huwe B. Impact of preferential flow on soil chemistry of a podzol[J]. Geoderma, 2012, 175/176(5):37-46.

Stewart B W. Comparison of preferential flow paths to bulk soil in a weakly aggregated silt loam soil[J]. Vadose Zone Journal, 2009, 8(3):623-627.

Views

1131

下载量

CSCD

Alert me when the article has been cited

提交

Tools

Publicity Resources

Characteristics and influencing factors of soil organic carbon at Picea crassifolia forests in middle part of Qilian Mountains

Correlations Between Characteristics of Alhagi Communities and Soil Factors in Danghe River Basin

Impact of resource-exhausted city transformation on net ecosystem productivity——A case study of Xuzhou City， Jiangsu Province

Soil-water characteristics and softening constitutive model of lime-stabilized loess

Influence of soluble salt content on strength of Ili loess under wet-dry cycle conditions

Related Author

Jiang Zhiren

Zhao Weijun

Wang Junmei

Feng Jinyuan

Jiang Zhicheng

JIN Xiaoying

AN Rong

QU Jianjun

Related Institution

Qilian Mountain National Nature Reserve， Xiama Nature Reserve

Gansu Qilian Mountain National Nature Reserve Management Center

Qilian Mountain National Nature Reserve， Qilian Nature Reserve

Academy of Water Resources Conservation Forests in Qilian Mountains of Gansu Province

Qilian Mountain National Nature Reserve， Wushaoling Mountain Nature Reserve

⁰