北疆典型土壤纵向弥散系数试验

doi:10.6048/j.issn.1001-4330.2021.01.018

新疆农业科学 ›› 2021, Vol. 58 ›› Issue (1): 151-158.DOI: 10.6048/j.issn.1001-4330.2021.01.018

• 植物保护·土壤肥料·贮藏保鲜加工·农业水土工程·微生物·农产品分析检测 • 上一篇下一篇

北疆典型土壤纵向弥散系数试验

虎胆·吐马尔白^1,2, 穆丽德尔·托伙加², 朱珠²

1.南京水利科学研究院水文水资源与水利工程重点实验室,南京 210029;
2.新疆农业大学水利与土木工程学院,乌鲁木齐 830052

收稿日期:2020-03-13 出版日期:2021-01-20 发布日期:2021-01-20
作者简介:虎胆·吐马尔白(1960-),男,新疆博乐人,教授,博士,博士生导师,研究方向为土壤水盐运移及高效节水灌溉,(E-mail)2419439411@qq.com
基金资助:
南京水利科学研究院水文水资源与水利工程科学国家重点实验室“干旱绿洲连作滴灌棉田根系层盐分类累积效应与控盐模式研究”(2018nkms02);塔里木河流域管理局课题“新疆阿克苏河流域平原灌区核桃及红枣需水量研究”(TGJAKSJJG-2019KYXM0001)

Experimental Study on Longitudinal Dispersion Coefficient of Typical Soil in Northern Xinjiang

Hudan Tumaerbai^1,2, Mulideer Tuohuojia², ZHU Zhu²

1. Key Laboratory of Water Science and Engineering, Ministry of Water Resources, Nanjing Hydraulic Research Institute, Nanjing 210029, China;
2. College of Water Conservancy and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China

Received:2020-03-13 Online:2021-01-20 Published:2021-01-20
Correspondence author: Hudan Tumaerbay(1960-),male,native of Bole,Xinjiang,Professor,Doctor,Doctoral Supervisor,Research field:The Theory and Practice of Soil Water and Salt Migration and Efficient Water-saving Irrigation,(E-mail)2419439411@qq.com.
Supported by:
The Project of Key Laboratory of Water Science and Engineering of Nanjing Hydraulic Research Institute "Study on the Positive Effect of Root Layer Salt Classification in Continuous Drip Irrigation Cotton Field in Arid Oasis" (2018nkms02); the Project of Tarim River Basin Authority "Study on Water Demand of Walnut and Jujube in Plain Irrigation Area of Aksu River Basin, Xinjiang" (TGJAKSJJG-2019KYXM0001)

摘要/Abstract

摘要： 【目的】 研究不同土壤质地对土壤纵向弥散系数和弥散度的影响。【方法】 根据土壤物理学及水动力弥散理论,以新疆北疆较为常见的典型砂壤土、粉壤土、壤土为例,NaCI为示踪剂,采用室内一维土柱垂直入渗试验测定纵向弥散系数。【结果】 不同土壤质地,渗流速度越小弥散系数越小,渗流流速越大,达到土壤溶质浓度峰值的时间越短,且峰值浓度越大。砂壤土渗流速为0.020 cm/min,纵向弥散度为2.88 cm;粉壤土渗流速度为0.018 1 cm/min,纵向弥散度为3.85 cm;壤土渗流速度为0.011 cm/min最小,纵向弥散度为2.44 cm。【结论】 弥散系数和弥散度取决于土壤质地类型与渗流流速。

关键词: 典型土壤; 盐分运移; 纵向弥散系数

Abstract: 【Objective】 In order to explore the effect of different soil texture on soil longitudinal dispersion coefficient and dispersion degree.【Method】 According to the soil physics and hydrodynamic dispersion theory, typical sandy loam, silty loam and loam in northern xinjiang were taken as examples. NaCI was used as tracer and the longitudinal dispersion coefficient of one-dimensional vertical infiltration test was carried out in the laboratory.【Result】 Because of the coarse texture of sandy loam, soil compactness is not big, the liquid is easy to diffuse. The smaller the seepage velocity, the smaller the dispersion coefficient, and the larger the seepage velocity, the shorter the time to reach the peak of soil solute concentration, and the larger the peak concentration, and the smaller the vice versa. The seepage velocity of sandy loam was 0.020 cm/min, and the longitudinal dispersion degree was 2.88 cm. The silty loam was 0.018,1 cm/min and the longitudinal dispersion degree was 3.85 cm. The loam seepage velocity was the smallest at 0.011 cm/min, and the longitudinal dispersion degree was 2.44 cm.【Conclusion】 The results show that the dispersion coefficient depends on soil texture type and seepage velocity.

Key words: typical soil; soil salinity transport; longitudinal coefficient

中图分类号:

虎胆·吐马尔白, 穆丽德尔·托伙加, 朱珠. 北疆典型土壤纵向弥散系数试验[J]. 新疆农业科学, 2021, 58(1): 151-158.

Hudan Tumaerbai, Mulideer Tuohuojia, ZHU Zhu. Experimental Study on Longitudinal Dispersion Coefficient of Typical Soil in Northern Xinjiang[J]. Xinjiang Agricultural Sciences, 2021, 58(1): 151-158.

参考文献

[1]魏峰,王全九,周蓓蓓.考虑尺度效应的瞬时输入溶质运移模型及解析解[J].农业工程学报,2014,30(16):129-135.
WEI Feng, WANG Quanjiu, ZHOU Beibei. Analytical solution for scale-dependent solute transport model with instantaneous source[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2014,30(16):129-135.
[2]丁家平,李樟苏.地下水弥散系数的野外试验新方法[J].水利学报,1998,(8):38-42.
DING Jiaping,LI Zhangshu.A new method for field tracing test of groundwater[J]. Journal of Hydraulic Engineering, 1998,(8):38-42.
[3]杨金忠.多孔介质中水分及盐分溶质运移的随机理论[M].北京:科学出版社,2000.
YANG Jinzhong. Stochastic theory of water and salt solute transport in porous media [M].Beijing:science press,2000.
[4]李炎,王丹.非饱和土壤水动力弥散系数的研究[J].湖北农业科学,2015,54(12):2887-2890.
LI Yan,WANG Dan.Study on hydrodynamic dispersion coefficient of unsaturated soil[J]. Hubei Agricultural Sciences, 2015,54(12):2887-2890.
[5]Clothier B E,Kirkham M B, McleanJE.In situ measurements or the effective transport volume for solute moving through Soil[J]. Soil Science Society of America, 1992,(56):733-736.
[6]Lapidus L, Amundson N R. Mathematics of Adsorption in Beds[J].Physical Chemistry Chemical Physics ,1952,56:984-988.
[7]Nielsen D R, Biggar J W.Miscible displaccment in soils:III[J]. Soil Science Society of America, 1962,(26) :216 -221.
[8]Comparison of batch and column methods for determining strontium distribution, coefficient for unsaturated transport in basalt. Environ.Sci. Technol.2000,(34):1679-1686.
[9]任长江,白丹,何凡,等.非饱和土壤水动力弥散系数研究[J].西安理工大学学报,2017,33(4):419-424.
REN Changjiang,BAI Dan,HE Fan,et al.Study on hydrodynamic dispersion coefficient in unsaturated soil[J]. Journal of Xi'an University of Technolog, 2017,33(4):419-424.
[10]Bear J. The transition zone between fresh sat water in coastal aquifer[D].Berkeley:Uiniversity of Calinifornia, Berkeley,1960.
[11]Pfankuch H O. On the correlation of electrical conductivity properties of porous systems with iscous flow transport coefficients[A].[S.n],1969:78-92.
[12]Taylor G I. Dispersion of Soluble Matter in Solvent Flowing Slowly Through a Tube[C].Royal Soc.1953:186-187.
[13]Klotz,D.Seiler, K.P.,Moser, H.Dispersivity and velocity relationship from laboratory and field experiments[J]. HydroL. 1980, 45(3/4):169-184.
[14]程金茹,郭择德.黄土包气带土壤水动力弥散系数的测定研究[J].辐射防护通讯,2001, (5):24-26.
CHENG Jinru,Guo Zede.Determination of Hydrodynamic Diffusion Coefficient for Soils in Loess Aerated Zone[J]. Radiation Protection Bulletin, 2001, (5):24-26.
[15]邵爱军,刘广明,杨劲松,等.土壤水动力弥散的室内测定[J].土壤学报,2002,39(2):184-189.
SHAO Aijun,Liu Guangming,YANG Jingsong,etal.In-lab Determination of Soil Hydrodynamic Disperson Coefficient[J]. Acta Pedologica Sinica, 2002,39(2):184-189.
[16]张银妹,张燕君,等.示踪剂弥散试验影响因子分析[J].地下水,2014,36(2):4-6.
ZHANG Yinmei,ZHANG Yanjun,et al. Analysis of Impact Factors in Tracer Dispersion Test [J]. Ground Water, 2014,36(2):4-6.
[17]张明泉,曾正中,高洪宣,等.室内二维弥散试验研究[J].兰州大学学报,1993,29(4):274-278.
ZHANG Mingquan,ZENG Zhengzhong,GAO Hongxuan,et al.Two-dimensional dispersion experiment in laboratory[J]. Journal of Lanzhou University(Natural Sciences), 1993,29(4):274-278.
[18]赵雪琼,卞建民,杨坡,等.长春西部串湖多孔介质弥散试验及污染质运移研究[J].地下水,2008,30(5):12-14.
ZHAO Xueqiong,BIAN Jianmin,YANG Po,et al. Indoor Test of 2-D Hydrodynamic Dispersion and Analysis of Pollutant Migration in Chuanhu Water-bearing Medium[J].地下水,2008,30(5):12-14.
[19]S.Zou,A.parr.Two-dimensional dispersivity extimation using tracer experiment data,[J]. Groundwater. 1994,l32(3):367-373.
[20]王全九,邵明安,郑纪勇.土壤中水分运动与溶质迁移[M].北京:中国水利水电出版社,2007:81-83.
WANG Quanjiu,SHAO Mingan,ZHENG Jiyong. Water movement and solute migration in soil[M].Beijing:China water resources and hydropower press,2007:81-83.
[21]陈崇希,李国敏.地下水溶质运移理论及模型[M].北京:中国地质大学出版社,1996:59-70.
CHEN Chongxi, LI Guomin.Theory and model of solute transport in groundwater [M].Beijiang:China University of Geosciences Press, 1996:59-70.
[22]丁佳.银川地区潜水含水层弥散参数试验确定方法研究[D].西安:长安大学,2010.
Ding Jia. Experimental determination of diffusion Parameters of unconfined aquifers in Yinchuan[D].Xian:Chang,an University,2010.
[23]Huang K,van Genuchten M Th,Zhang R.Exact solutions for one-dimensional transport with asymptotic scale-dependent dispersion[J]. Applied Mathematical Modelling, 1996,20(4):298-308.
[24]Kai Uwe Totsche, etal. Evaluation of fluoride-induced mobilization in soil columns.J.Environ.Qual.,2000,29:454-459.

北疆典型土壤纵向弥散系数试验

Experimental Study on Longitudinal Dispersion Coefficient of Typical Soil in Northern Xinjiang

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