[1]马富亮,符素华,罗广惠.东北典型黑土区坡耕地涝渍地土壤持水性和导水性研究[J].水土保持研究,2017,24(06):222-226.
　MA Fuliang,FU Suhua,LUO Guanghui.Properties of Soil Water Retention and Hydraulic Conductivity in the Waterlogged Land over Slope Cropland in Typical Black Soil Region of Northeast China[J].Research of Soil and Water Conservation,2017,24(06):222-226.
点击复制

东北典型黑土区坡耕地涝渍地土壤持水性和导水性研究

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 24 期数: 2017年06期 页码: 222-226 栏目: 出版日期: 2017-11-24
Title:
Properties of Soil Water Retention and Hydraulic Conductivity in the Waterlogged Land over Slope Cropland in Typical Black Soil Region of Northeast China
作者:
马富亮1, 符素华1,2, 罗广惠3
1. 北京师范大学 地理学与遥感科学学院, 北京 100875;
2. 中国科学院 水利部 水土保持研究所 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西 杨凌 712100;
3. 北京市一六五中学, 北京 100010
Author(s):
MA Fuliang1, FU Suhua1,2, LUO Guanghui3
1. School of Geography, Beijing Normal University, Beijing 100875, China;
2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China;
3. Beijing No. 165 High School, Beijing 100010, China
关键词:
黑土; 坡耕地; 涝渍地; 土壤水分特征曲线
Keywords:
black soil; slope cropland; waterlogged land; water retention characteristics
分类号:
S152.7+1;S152.3+3
摘要:
中国东北典型黑土区是我国重要的商品粮生产基地，对我国粮食安全和国民经济的稳定起到举足轻重的作用。作为土壤退化的一种特殊形式，涝渍地严重影响着垦区的农业生产。在东北典型黑土区坡面涝渍地及其周围正常耕地中布设采样点，测定了土壤剖面质地分布情况及土壤水分特征曲线，以揭示东北黑土区坡面涝渍地土壤水分过大的根本原因。结果表明，涝渍地土壤剖面中细质地土壤类型所占比例为90%，质地较粘重。涝渍地土壤具有较高的进气值，水吸力较大，保持在中小孔隙中的水分只有在较大吸力范围内才能缓慢释出，这造成涝渍地土壤具有极强的持水能力，不容易失水，再加上极弱的导水能力，水分饱和但不会被释放。以上这些土壤特性导致了涝渍地土壤长期处于湿度过大的状态。本研究结果可为涝渍地治理提供依据。
Abstract:
The typical black soil zone in northeast China is an important commodity grain production base in China and plays crucial roles in the national food security and economic stability. As a special form of soil degradation, waterlogged lands severely affect the agricultural production in reclamation regions. The objective of this study was to analyze the soil water retention characteristics and hydraulic conductivity of waterlogged land and try to find the cause of waterlogged land. The sampling points were set in and around the waterlogged land over the slope cropland in typical black soil region of northeast China. The soil texture distribution along the soil profiles and soil water retention characteristics were measured. The results showed that the fine soil texture accounted for 90% in the soil profile in waterlogged land. It resulted in a very adhesive soil texture. The waterlogged soil had higher air intake value and the larger water suction than the non-waterlogged soil. Therefore, the water in waterlogged soil pore could be released under the much larger water suction. In addition, the waterlogged soil has the strong water holding capacity and the weak soil hydraulic conductivity, which indicated that the water in the saturated soil can not be released and that the soil keeps high soil moisture. The above soil properties are the important reasons that the waterlogged soil remains a wet condition for a long time. These results could provide the technique supports for the control for waterlogged lands.

参考文献/References:

[1] 陆继龙.我国黑土的退化问题及可持续农业[J].水土保持学报,2001,15(2):53-55.
[2] 魏永霞,康百赢,刘学金.黑龙江垦区渍涝治理途径探索[J].水利科技与经济,2005,3(2):83-85.
[3] 朱建强,黄智敏,臧波,等.江汉平原的涝渍地及其开发利用[J].湖北农学院学报,2005,24(4):248-252.
[4] 秦续娟.东北北部黑土坡耕地涝渍成因研究[D].重庆:西南农业大学,2006.
[5] 姚章村,刘宗建.三江平原渍涝分类和不同治理阶段研讨[J].现代化农业,1993(4):004.
[6] 刘兵,朱广石,王平,等.东北农田涝渍成因和治理研究概况[J].广东农业科学,2010(11):276-278.
[7] 郎惠卿,祖文辰,金树仁.中国沼泽[M].济南:山东科学技术出版社,1983.
[8] McFarlane D J, George R J, Farrington P. Changes in the Hydrologic Cycle[M]//Hobbs R J, Saunders D A. Reintegrating Fragmented Landscapes. New York:Springer, 1993.
[9] Cox J W, McFarlane D J. The causes of waterlogging in shallow soils and their drainage in southwestern Australia[J]. Journal of Hydrology, 1995,167(1/4):175-194.
[10] 孙广友.沼泽湿地的形成演化[J].国土与自然资源研究,1998(4):33-35.
[11] Hatton T J, Nulsen R A. Towards achieving functional ecosystem mimicry with respect to water cycling in southern Australian agriculture[J]. Agroforestry Systems, 1999,45(1/3):203-214.
[12] 牛焕光,宋海远.三江平原地区沼泽成因及泥炭分布规律[J].地理科学,1990,10(3):246-256.
[13] 田守成,王于洋.黑龙江省涝渍灾害分析[J].东北水利水电,1996(7):32-35.
[14] 吕宪国.湿地科学研究进展及研究方向[J].中国科学院院刊,2002(3):170-172.
[15] 李红艳,刘庆华,魏永霞.三江平原涝渍灾害成因及治理过程的思考[J].水利科技与经济,2003,9(3):218-219.
[16] 黄丽,何平,孙群晶.2004年与历年三江平原成灾雨型分析[J].黑龙江水专学报,2005,32(1):1-3.
[17] 朱建强.易涝易渍农田排水应用基础研究[M].北京:科学出版社,2007.
[18] 乔樵,沈善敏,周绍权东北北部黑土水分状况之研究.Ⅰ:黑土水分状况的基本特征及其与成土过程的关系[J].土壤学报,1963,11(2):143-158.
[19] 郭大本,王清.三江平原沼泽湿地开垦前后下垫面水理性质变化研究[J].黑龙江水专学报,1995,02(1):1-8,18.
[20] 鲁如坤.土壤农业化学分析方法[M].北京:中国农业科技出版社,2000.
[21] 赵雅琼,王周锋,王文科,等.不同粒径下土壤水分特征曲线的测定与拟合模型的研究[J].中国科技论文,2015(3):287-290.
[22] 伊盼盼,牛圣宽,韦昌富.干密度和初始含水率对非饱和重塑粉土土水特征曲线的影响[J].水文地质工程地质,2012,39(1):42-46.
[23] Yang C, Sheng D, Carter J P. Effect of hydraulic hysteresis on seepage analysis for unsaturated soils[J]. Comput. Geotech, 2012,41:36-56.
[24] 高惠嫣,杨路华.不同质地土壤的水分特征曲线参数分析[J].河北农业大学学报,2012,35(5):129-132.
[25] 雷志栋,杨诗秀,谢森传.土壤水动力学[M].北京:清华大学出版社,1988.
[26] 史海滨,田军仓,刘庆华.灌溉排水工程学[M].北京:中国水利水电出版社,2006:16-17.

相似文献/References:

[1]梁彦荣,张 岩,李坤衡,等.基于高分遥感调查东北黑土区10年尺度切沟治理效果[J].水土保持研究,2024,31(06):67.[doi:10.13869/j.cnki.rswc.2024.06.025]
　Liang Yanrong,Zhang Yan,Li Kunheng,et al.Investigation on the Effects of Gully Control in China's Black Soil Region over a 10-Year Scale Based on High-Resolution Remote Sensing[J].Research of Soil and Water Conservation,2024,31(06):67.[doi:10.13869/j.cnki.rswc.2024.06.025]
[2]朱红春,张友顺.陕北黄土高原坡耕地生态退耕经济效益评价与分析[J].水土保持研究,2003,10(02):41.
　ZHU Hongchun,ZHANG Youshun.Economic Benefit Value and Analysis of Biologic Rescue in the North Shanxi Sloping Plantation of the Loess Plateau[J].Research of Soil and Water Conservation,2003,10(06):41.
[3]郑粉莉,唐克丽,陈文亮.细沟侵蚀过程的研究方法[J].水土保持研究,1993,(01):107.
　Zheng Fenli,Tang Keli,Chen Wenliany.Research Methods of Rill Erosion Process[J].Research of Soil and Water Conservation,1993,(06):107.
[4]刘晓昱.黑土农田生态系统的保育与发展[J].水土保持研究,2006,13(05):143.
　LIU Xiao-yu.Safeguard and Sustainable Development of the Black Soil Ecosystem[J].Research of Soil and Water Conservation,2006,13(06):143.
[5]农淦,路培,王林华,等.黄土高原坡耕地小麦根系分布特征研究[J].水土保持研究,2013,20(05):92.
　NONG Gan,LU Pei,WANG Lin-hua,et al.Study on Root Distribution of Winter Wheat on Slope Farmland on the Loess Plateau[J].Research of Soil and Water Conservation,2013,20(06):92.
[6]吴素业.皖西南山区坡耕地水土流失防治措施[J].水土保持研究,1996,3(04):38.
　Wu Suye.The Control Practice of Water and Soil Loss in Hillside Fields of Southwestern Mountain Area of Anhui Province[J].Research of Soil and Water Conservation,1996,3(06):38.
[7]林永知.丘陵地区坡耕地水土流失动态监测分析[J].水土保持研究,1997,4(01):120.
　Lin Yongzhi.Analysis on the Dynamic Monitoring of Soil and Water Loss of Slope Farmland in Hilly Area[J].Research of Soil and Water Conservation,1997,4(06):120.
[8]高岚,王振颖.辽宁省坡耕地资源普查及成果分析[J].水土保持研究,1997,4(04):44.
　Gao Lan,Wang Zhenying.General Survey of Hillyland Resources and Result Analysis in Liaoning Province[J].Research of Soil and Water Conservation,1997,4(06):44.
[9]杨玉阁,黄毅,曹忠杰.辽宁坡耕地的生产能力与开发治理前景[J].水土保持研究,1997,4(04):50.
　Yang Yuge,Huang Yi,Cao Zhongjie.Soil Productivity and Its Exploitate Prospect for Hillside Fields in Liaoning Province[J].Research of Soil and Water Conservation,1997,4(06):50.
[10]张本家.辽宁省坡耕地低产原因与治理措施[J].水土保持研究,1997,4(04):53.
　Zhang Benjia.Low Output Problems of Hilly Field and Its Harnessing Measures in Liaoning Province[J].Research of Soil and Water Conservation,1997,4(06):53.

备注/Memo

收稿日期:2016-10-18;改回日期:2016-11-08。
基金项目:国家自然科学基金（41571259）；国家自然科学基金重点项目（41530858）；中国科学院“西部之光”人才培养引进计划的资助
作者简介:马富亮(1985-),男,山东夏津人,博士研究生,主要从事土壤水分运动方面的研究。E-mail:flma0620@163.com
通讯作者:符素华(1973-),女,四川岳池人,教授,主要从事土壤侵蚀与水土资源管理方面的研究。E-mail:suhua@bnu.edu.cn

更新日期/Last Update: 1900-01-01