不同地下水埋深条件下再生水灌溉的试验研究
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摘要
为地下水埋深不同地区再生水的安全高效利用提供理论依据,本试验在地中渗透仪中进行,用马氏瓶控制地下水位分别为2m、3m、4m,取污水处理厂的再生水灌溉冬小麦和夏玉米,并与清水对照,对其各项生育指标变化及灌水前后氮素运移进行了研究,结果表明:
     1、再生水灌溉有利于冬小麦叶面积指数、干物质积累量和产量的增加,与清水相比,能为作物提供更多的营养元素。相同灌水量和施肥条件下,低水处理冬小麦产量与地下水埋深成指数相关,高水处理产量与地下水埋深为多项式关系。从冬小麦各生育指标、干物质积累量、产量和水分利用效率分析得出,地下水埋深为2m的地区,再生水灌溉选用低水处理较好;地下水埋深为3m和4m的地区,再生水灌溉选用高水处理较好。
     2、地下水位埋深对夏玉米的叶面积指数影响较大,叶面积指数随着地下水位埋深的增加而减小,其中4m地下水位对叶面积指数的影响最大。灌水量相同时,低水处理和高水处理的夏玉米产量与地下水埋深都为多项式关系;地下水埋深相同时,高水灌溉的产量比低水灌溉的大。
     3、灌水前和灌水后,土壤的硝态氮含量都是先随深度增加而增大,在达到一个峰值后,再随深度增加而减小。与灌水前相比,灌水后硝态氮含量的峰值都出现下移现象,灌水前峰值出现在20~40cm土层处,灌水后峰值出现在40~80cm处,说明灌水对表层土壤的硝态氮有强烈的淋洗作用。
     4、灌水后0~200cm土壤的硝态氮平均含量升高,地下水埋深相同时,高灌水量处理增加的硝态氮含量比低灌水量处理的增加值大;灌水量相同时,土壤中硝态氮增加量和地下水中硝态氮的增量与地下水埋深成多项式关系。
The aim of the article is to provide theoretical foundation for safe and efficient utilization of reclaimed water in the areas of different depths of groundwater. The experiment is made in the lysimeter, and the groundwater tables are 2m, 3m and 4m controlled by Mariotte. In the experiment, the reclaimed water acquired from sewage treatment plant is used to irrigate winter wheat and summer corn, and the variation of all indexes and nitrogen transportation of the wheat and corn are studied. The results are as following:
     1. The reclaimed water irrigation greatly affects the leaf area index, the dry matter accumulation and the output of the winter wheat. Under the same condition of irrigation amount and fertilization, the output of winter wheat with low water treatment has the exponential correlation with groundwater table, and the output of winter wheat with high water treatment has the polynomial correlation with groundwater table. Low water handling is better for reclaimed water irrigation in the areas of groundwater depth of 2m through analyzing the physiological indexes, the dry matter accumulation, the output and the water use efficiency. In the meantime, high water handling is better for reclaimed water irrigation in the areas of groundwater depth of 3m and 4m.
     2. The leaf area index of summer corn is affected by the groundwater depth, and it decreases with the groundwater depth raising. The groundwater depth of 4m has the most significant influence. Under the same condition of irrigation amount and fertilization, the output of summer corn with low or high water treatment has the polynomial correlation with groundwater table. And under the same condition of groundwater, the output with high water treatment is more than the output with low water treatment.
     3. The nitrate nitrogen content of soil firstly increases along depth direction, and after getting to a summit decreases along depth direction, no matter before irrigation or after irrigation. Compared with the time before irrigation, the summit of nitrate nitrogen content after irrigation shifts down, from the summit on the soil layer of 20-40cm before irrigation to the summit on the soil layer of 40-80cm after irrigation, which illustrates that irrigation has the dramatically leaching influence to nitrate nitrogen of surface soil.
     4. The average content of nitrate nitrogen on the soil layer of 0-200cm has increased after irrigation. And with the same groundwater depth, the increasing of nitrate nitrogen content of high water handling is more than low water handling, because the more irrigation amount contains more nitrogen. With the same irrigation amount, the increasing of nitrate nitrogen content both in the soil and groundwater has the polynomial correlation with groundwater table.
引文
[1] 郑晓萍,单为春.我国中水的开发与利用[J].冶金动力,2005(5):47~49.
    [2] 魏娜,程晓如,刘宇鹏.浅谈国内外城市污水回用的主要途径[J] .节水灌溉,2006(1):31~34.
    [3] 张超品,刘洪禄,吴文勇等.再生(污)水灌溉利用研究[J] .北京水利,2004,(4):17~19.
    [4] 王德荣,尸远培.推进城镇污水资源化户国农业水危机对策研究[M].北京:中国农业科技出版社,1998:142~154.
    [5] 魏新平, 王文焰, 王全九,等.溶质运移理论的研究现状和发展趋势[J ]..灌溉排水, 1998,(4):58~63.
    [6] Q Z geng, G G Irard and E L edoux.Modeling of N itrogen Cycle and N itrate T ransfer in Regional hydrogeo logic System s[J] .Groundwater,1996,34(2):293~304.
    [7] Shahalam A., Abuzahra B. M., Jaradat A. Wastewater irrigation effect on soil, crop and environment: A pilot scale study at Irbid, Jordan[J] .Water Air and Soil Pollution, 1998, 106(3~4): 425~445.
    [8] Clark D. R., Green C. J., Allen V. G. et al. Influence of salinity in irrigation water on forage sorghum and soil chemical properties[J] .Journal of Plant Nutrition, 1999, 22(12): 1905~1920.
    [9] Friedel J. K., Langer T., Siebe C., et al. Effect of long-term waste water irrigation on soil matter, soil microbial biomass and its activities in central Mexico[J] .Biological Fertilize Soil, 2000, (31): 414~421.
    [10] Reyes S. I. E., Garcia C. N. E., Servin R. D. E. Wastewater-irrigation effect in physical and chemical soil properties of Mezquital Valley, Hidalgo state, Mexico[J] .Geochimica et Cosmochimica Acta, 2003, 67(18): 396.
    [11] Neilsen G. H., Stevenson D. S., Fitzpatrick J. J., et al.Soil and sweet cherry responses to irrigation with wastewater[J] .Canadian Journal of Soil Science, 1991, 71(2): 31~41.
    [12] Chakrabarti C.Residual effect of long-term land application of domestic waste-water[J] .Environment International, 1995, 21(3): 333~339.
    [13] Stevens D. P., McLaughlin M. J., Smart M. K.Effect of long-term with reclaimed water on soils of the Northern Adelaide Plains, South Australia[J] .Australian Journal of Soil Research, 2003, (41): 933~948.
    [14] Dagan G,Bresler E.Solute transport in unsaturated heterogeneous soil at field scale I[J] .Theong,Soil SocAm J,1979,43:461~467.
    [15] Gureghion A B,Ward D S,Cleary R W.Simultaneous transport of water and reacting solute through multlayered soils under transient unsaturated flow conditions. [J] .Hydrol,1979,41:253~278.
    [16] L.Cacazza,P.Rossi Pissa.Effect of watertable depth and waterlogging on crop yield[J] .Agricultural water management,volume14,issues 1-4,August-1988,pages29~34.
    [17] 张红梅,速宝玉.土壤及地下水污染研究进展[J] .灌溉排水学报,2004(6),23(3):70~74.
    [18] 王超.土壤及地下水污染研究综述[J] .水利水电科技进展.1996(12), 16(6):1~4.
    [19] 王秉忱,杨天行,王宝金等.地下水污染地下水水质模拟方法.北京:北京师范大学出版社,1985.
    [20] Garve G, Freeze R A.Theoretical analysis of the role of groundwater flow in the genesis ore deposits I mathematical and numerical model[J] .Am J Soi,1984,284:1085~112.
    [21] Refsgaard A et al.Three dimensional modeling of groundwater flow and solute transport[J] .Cot Tran,1991.
    [22] Barry D A, Sposito G.Analytical solution of a convection -dispersion model with time2dependent transport coefficients[J] .Water Resource Res,1989,25:2407~2416.
    [23] Yates S A.An analytical solution for one2 dimensional transport in hetergeneous porousmedia[J] .Water Resour Res,1990,26:2331~2338.
    [24] Smith L, F W Sehwartz. Mass transport I.a stochastic analysis of macroscopic dispersion[J] .Water Resour Res,1980,16(2):303~313.
    [25] Rubin Y.Stochastic modeling of macrodispersion in hetergeneous porous media[J] .Water Resour Res,1990,26(1):133~141.
    [26] Vassilis, Z.A.Simulation of water and nitrogen dynamics in soils during waste water application by using a finite-element model[J] .Water Resources Management .(7):237~251.
    [27] Selim, H.M. and Iskandar.I.K. Modeling nitrogen transport and transformation in soil [J] .Soil Science ,131(2):233~241.
    [28] 张福锁,龚元石,李晓林.土壤与植物研究新动态[M].北京:中国农业出版社,1995.
    [29] Van Genuchten, M.Th. and Dalton.F.N. Models for simulating salt movement in aggregated field soils[J] .Geoderma,1986,(38):165~183.
    [30] Steenhuis, T.S., Parlange, J.Y. and Andreini, M.S. A numerical model for preferential solute movement in structured soils[J] .Geoderma,1990,(46):193~208.
    [31] Hopmans, J.W.Treatment of spatially variable groundwater levels in one-dimensional stochastic unsaturated water flow modeling[J] .Agric. Water Manage.,1988,(15):19~36.
    [32] Jarvis, N.J., Jansson, P.E., and Dik,P.E.Modeling water and solute transport in macro-porous soil,I.Model description and sensitivity analysis[J] .Soil Sci.,1991,(42):59~70.
    [33] 杨邦杰,隋红建.土壤水热运动模拟[M].北京:中国科学出版社,1997.
    [34] Addiscott and Wagenet.Concepts of solute leaching in soil: a review of modeling approaches[J] .Soil Sci.,1985,36:411~424.
    [35] Warrick, A.W., Biggar, J.W., and Nielsen, D.R.Simultaneous solute and water transfer for unsaturated soil[J] .Water Resour. Res.,1971,7:1216~1225.
    [36] Laughlin, M.D., and Wood, E.F.A distributed parameter approach for evaluating the accuracy of groundwater model predictions [J] .Theory. Water Resour. Res.,1988,27(7):1037~1047.
    [37] Mansell, R.S., Bloom S.A.,and Aylmore, L.A.G.Simulating cation transport during unsaturated water flow in sandy soil[J] .Soil Sci.,1990,150:730~744.
    [38] William A.Jury.Simulation of solute transport using a transfer function model [J] .Water Resource Research ,1982,18(2):363~368.
    [39] Kurt Roth and W William A.Jury.Modeling the transport of solutes to groundwater using transfer function[J] .Envir. Qual. ,1993,22:487~493.
    [40] 叶自桐.利用盐分迁移函数模型研究入渗条件下土层的水盐动态[J] .水利学报.1990,21:1~9.
    [41] 冯绍元,张瑜芳等.排水条件下饱和土中氮肥转化与运移模型[J] .水利学报,1995(6),6:16~22.
    [42] 冯绍元,张瑜芳等.非饱和土壤中氮素运移与转化试验及其数值模拟[J] .水利学报,1996(8),8:8~14.
    [43] 陆垂裕,杨金忠.污水灌溉系统中氮素转化运移的数值模拟分析[J] .水利学报,2004(5),5:83~88.
    [44] 姜翠玲,夏自强.污水灌溉土壤及地下水三氮的变化动态分析[J] .水科学进展,1997(6),8(2):184~188.
    [45] 李法虎,M. Benhur.劣质水灌溉对土壤盐碱化及作物产量的影响[J] .农业工程学报,2003(1),19(1):63~66.
    [46] 孟春香,郭建华.污水灌溉对作物产量及土壤质量的影响[J] .河北农业科学,1999(6)。3(2):15~17.
    [47] 曹淑萍.重金属污染元素在天津土壤剖面中的纵向分布特征[J] .地质找矿论丛,2004年12月,19(4):270~274.
    [48] 刘凌,陆桂华.含氮污水灌溉实验研究及污染风险分析[J] .水科学进展,2002(5),13(3):313~320.
    [49] 高洪阁,陈丽惠等. 污灌区与非污灌区的地下水主要水质指标变化趋势及对比研究[J] .环境污染治理技术与设备,3(6),2002: 25~28.
    [50] 万正成,李明武等.城市污水灌溉对地下水水质的影响分析[J] .江苏环境科技,2004(3),17(1):29~31.
    [51] 冯绍元,齐志明.重金属在夏玉米作物体中残留特征的田间试验研究[J] .灌溉排水学报,2003(12),22(6):9~13.
    [52] 冯绍元,邵洪波.重金属在小麦作物体中残留特征的田间试验研究[J] .农业工程学报,2002(7),18(4):113~115.
    [53] 邵洪波.污水灌溉条件下冬小麦生长及重金属分布规律的试验研究[D] .中国农业大学学位论文.
    [54] 查贵锋,黄冠化.夏玉米污水灌溉时水分与氮素利用效率的研究[J] .农业工程学报,2003(5),19(3):63~67.
    [55] 孟雷,左强.污水灌溉对冬小麦根长密度和根系吸水速率分布的影响[J] .灌溉排水学报,2003(8),22(4):25~29.
    [56] 王友保,刘登义.污灌对作物生长及其活性氧清除系统的影响[J] .环境科学学报,2003(7),23(4):555~557.
    [57] 韩冰.白银市污水灌溉对农田环境及小麦产量质量的影响研究[J] .甘肃农业科技,1999,6:46~47.
    [58] 冯绍元.排水条件下饱和土壤中氮肥转化与运移模拟[J] .水利学报,1995, No.6.
    [59] 王超.氮类污染物在土壤中迁移转化规律试验研究[J] .水科学进展,1997,8(2):176~182.
    [60] 王红旗,陈家军.城市污水不同土地处理条件下土壤-作物系统中氮净化模拟模型与模拟分析[J].北京师范大学学报(自然科学版),1998,34(3):414~420.
    [61] 闫秀懿,鲁雅梅,刘贤荣等.含氮污水净化的数学模型及其实例模拟[J] .吉林地质,2002,21(4):56~63.
    [62] 唐国勇,黄道友等.土壤氮素循环模型及其模拟研究进展[J] .应用生态学报,2005,16(11):2208~2212.
    [63] 袁耀武,张伟.污水灌溉对土壤中不同微生物类群数量的影响[J] .节水灌溉,2003, 6:15~17
    [64] 罗固源,周健.污水蚯蚓土地处理与资源回归[J] .重庆环境科学,1997(4),第19卷第2期,27~29.
    [65] 袁安秀,邢焕琴.郑州市城市污水灌溉农田的卫生学评价[J] .河南医学研究,1994(6),167~171.
    [66] 何鹏,刘德华.污水灌溉区儿童血红蛋白含量及其影响因素分析[J] .中国学校卫生,1994 15(4):261~262.
    [67] 吕毅,王渭.污水灌溉致环境铅污染及人群健康效应研究[J] .环境与健康杂志,1997 14(1):10~12.
    [68] 袁安秀,邢焕琴.郑州市城市污水灌溉农田的卫生学评价[J] .河南医学研究,1994(6),167~171.
    [69] 杨继富.污水灌溉农业问题与对策[J],水资源保护,2000(6), 2,4~8.
    [70] 董克虞,杨春惠,林春野.北京市污水农业利用区划的研究[M].北京:中国环境科学出版社,1994.51~125.
    [71] 封超年,郭文善等.地下水位对产量影响的研究[J] .江苏农学院学报,1995,16(1),39~42.
    [72] 杨建锋,万书勤.地下水对作物生长影响研究[J] .节水灌溉,2002(2):36~38.
    [73] 巴比江,郑大玮等.地下水埋深对冬小麦田土壤水分及产量的影响[J] .节水灌溉,2004(5):5~9.
    [74] 巴比江,郑大玮等.地下水埋深对春玉米田土壤水分及产量的影响[J] .水土保持学报,2004,18(3):57~60.
    [75] 姜翠玲,夏自强,崔广柏.土壤含水量与氮化合物迁移转化的相关性分析[J] .河海大学学报(自然科学版),2003(5),31(3):241~245.

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