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松华坝水源保护区农业种植模式与面源污染控制研究
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摘要
本文通过研究松华坝水源保护区内几种种植模式下(包括传统种植大田、大棚花卉、河滩地等)土壤污染物等各项物理化学性质的变化情况,同时对土壤渗滤水污染物含量变化情况进行跟踪以及对施肥情况进行调查整理,从而揭示水源保护区内农业面源污染的产生、迁移和转化机理,研究结果表明:
     (1)不同种植模式下土壤污染物主要积累在耕作层,耕作层以下(下渗量)污染物含量水平无明显差别。
     (2)地下水淘洗可能是土壤污染物流失的重要途径。地下水浸泡耕作层,可能导致地下水严重污染。
     (3)大棚花卉种植土壤污染物含量显著高于传统种植方式,而且氮和有机质的比例高,氮易流失。
     (4)水源区高污染胁迫种植模式宜转移至地势较高,地下水不会进入耕作层的区域。
     (5)种植模式轮作能够改良土壤养分比例,减少污染物流失。
A survey of 3 land using types which include bottomland, wheat/vegetables rotation field, growing flowers field under greenhouse within the Songhua reservoir basin (Kunming, China) was undertaken to determine soil pollutants and other changes in physical and chemical properties,investigating pollutants content in soil percolating water and fertilizer rate,in order to reveal the generation, migration and transformation mechanisms of agricultural non-point source pollution in Songhua reservoir basin.
     The results showed:?Soil pollutants in different land using types mainly accumulated in the plow layer, and it has no significant difference in the following tillage layer.
     It may be an important way to make the pollutants loss by underground water washing.Water immersion plow layer, may cause serious pollution of groundwater.
     Comparing with traditional cultivation, the soil pollutants in growing flowers field under greenhouse were significantly higher,? and a high proportion of nitrogen and organic matter was made, nitrogen lost very easy.
     Cropping pattern with high pollutants loss can not plant at higher land where underground water will not enter the plow layer.
     Cropping rotation can improve the soil nutrients and reduce the loss of pollutants.
引文
[1]陈吉宁,李广贺,王洪涛.滇池流域面源污染控制技术研究[J].中国水利,2004(9):47- 50.
    [2]叶碎高,王帅.水源地农业面源污染防治研究进展.前沿,2007:18-20.
    [3] Lovejoy S B, Lee, J G, Randhir t O , etal. Research needs for water quality management in the 21st century: A spatial decision support system [J ]. J. Soil Water Conserv, 1997, 52: 19- 23.
    [4] Beasley ,D.B. et al. ANSWERS :A Model for Watershed Planning. trans. ASAE ,1980 , 23 (4) :938- 944.
    [5]张维理,徐爱国,冀红杰,等.中国农业面源污染形式估计及控制对策,中国农业科学,2004(7) :1026 - 1033.
    [6]全为民,严力蛟.农业面源污染对水体富营养化的影响及其防治措施,生态学报,2002 ,22(3) :291 - 299.
    [7] VLADIMIRN,HARVEYO. Water quality: Prevention, identification and management of diffuse . pollution[M].New York :Van Nastrand Reinhold Company ,1993.
    [8]刘楚文.松华坝水库水源区面源污染的防治.水利规划与设计,2006,6:12-14.
    [9]李宗逊,丁宏伟.昆明市松华坝水库氮、磷主要来源的间接证据,西南农业学报,2007,20(3):430-434.
    [10]孔桂芬.松华坝水库水质现状及变化趋势分析.云南环境科学,2006,25(增刊):116-118.
    [11]仓恒瑾,许炼峰,李志安.农田氮流失与农业非点源污染.热带地理,2004,24(4):332-336.
    [12]仓恒瑾,许炼峰,李志安.农业非点源污染控制中的最佳管理措施及其发展趋势.生态科学,2005,24(2):173-177.
    [13]陈利顶,傅伯杰.农田生态系统管理与非点源污染控制[J].环境科学,200,21(2):98-100.
    [14]张水龙,庄季屏.农业非点源污染研究现状与发展趋势.生态学杂志,1998 ,17 (6):51–55.
    [15]马立珊等.苏南太湖水系农业面源污染及其控制对策研究.环境科学学报,1997,17 (1):39-47.
    [16]李玉山等.中美小流域治理和农业的对比研究.水土保持通报,1993,13 (1):11-15.
    [17] Rudra, R. P. et al. The Importance of Precise Rainfall Inputs in Nonpoint Source Pollution Modelling. Trans. Am. Soc. Agric.Eng.1993 ,36 ,44.
    [18]李怀恩.流域非点源污染模型研究进展与发展趋势.水资源保护,1996, (2) :14– 18.
    [19]马立珊.太湖流域水环境硝态氮和亚硝态氮污染的研究.环境科学,1987,8 (2) :60 - 65.
    [20]周祖澄.固体氮肥施入旱田土壤中去向的研究.环境科学,1985,6 (6) :2-7.
    [21]张水铭等.农田排水中磷素对苏南太湖水系的污染.环境科学,1993,14 (6) :24-29.
    [22]冉江华,黄洁.农业面源污染研究现状及发展趋势.山西农业科学2009,37(3):7-10.
    [23]张壮志,孙磊,常维山.水体富营养化中的氮素污染及生物防治技术研究现状[J].山西农业科学,2008,36(6):13-15.
    [24]王超.磷肥污染物在非饱和土壤中迁移特性研究[J].南京大学学报(自然科学版),1997,33(增刊):253-255.
    [25]黄满湘,周成虎,章申.农田暴雨径流侵蚀泥沙流失及其对氮磷的富集[J].水土保持学报,2002,16(4):13-16.
    [26]黄云凤,张珞平,洪华生.不同土地利用对流域土壤侵蚀和氮、磷流失的影响[J].农业环境科学学报,2004,23(4):735- 739.
    [27] WilliamF Ritter,Adel Shirmohammadi. Agricultural nonpoint source pollution: watershed management and hydrology [M].Florida: Lewis publishers,2001.
    [28]黄东风,王果,陈超.农业面源污染研究概况及发展趋势[J].中国农业小康科技,2006(11):39- 46.
    [29]刘鸿渊,刘险峰,闫泓.农业面源污染研究现状及展望,安徽农业科学,2008,36(19):8249-8250.
    [30]张维理,徐爱国,冀红杰.中国农业面源污染形式估计及控制对策[J].中国农业科学,2004(7) :1026– 1033.
    [31]王珍,王平.发展循环农业,治理农村面源污染[J].宏观经济管理,2006(8):46 -47.
    [32]李远,王晓霞.我国农业面源污染的环境管理:背景及演变[J ].环境保护,2005(4) :23– 27.
    [33]文军,骆东奇,罗献宝,等.千岛湖区域农业面源污染及其控制对策[J ].水土保持学报,2004(3) :126-129.
    [34]何浩然,张林秀,李强.农民施肥行为及农业面源污染研究[J].农业技术经济,2006(6) :2– 10.
    [35]李远,王晓霞.我国农业面源污染的环境管理:背景及演变[J].环境保护,2005,330(4) :23 -27.
    [36]叶碎高,王帅.水源地农业面源污染防治研究进展.中国水利.
    [37]张玉斌,郑粉莉,武敏.土壤侵蚀引起的农业非点源污染研究进展[J].水科学进展,2007( 18).
    [38]张燕,张洪,彭补拙,杨浩.不同土地利用方式下农地土壤侵蚀与养分流失.水土保持通报,2003,23(1):23-26.
    [39]肖振国.昆明市松华坝水库水质健康风向评价.环境科学与技术,2007,30(增刊):146-148.
    [40]马立珊等.苏南太湖水系农业面源污染及其控制对策研究.环境科学学报,1997 ,17 (1) : 39 -47.
    [41]张宇.滇池沿岸台地水土、氮磷流失特征与控制对策分析[J].云南环境科学,2006,25(1):31- 34.
    [42]赵荣钦,秦明周,黄爱民.耕地土壤碳固存的措施与潜力生态环境[J].2004,13(1): 81-84.
    [43]王淑平,周广胜,吕育财,邹建军.中国东北样带(NECT)土壤碳、氮、磷的梯度分布及其与气候因子的关系[J].植物生态学报,2002,26(5):513-51.
    [44] R. Lal. Soil carbon sequestration to mitigate climate change[J]. Geoderma, 2004, (123):1-22.
    [45] H.P. Collinse, E.T. Elliott, K. Paustian. Soil carbon pools and fLuxes in long-term corn belt Agro-ecosystems[J].Soil Biology & Biochemistry,2000(32):57-168.
    [46]李海波,韩晓增,王风.长期施肥条件下土壤碳氮循环过程研究进展[J].土壤通报,2007,38(2):384-388.
    [47] Jackson, R.B., Banner, J.L., Joba′ggy, E.G., Pockman, W.T., Wall, D.H.,. Ecosystem carbon loss with woody plant invasion of grasslands[J]. Nature, 2002,18:623–626.
    [48] J.J. Jiménez, R. Lal, H.A.Leblanc, R.O.Russo. Soil organic carbon pool under native tree plantations in the Caribbean lowlands of Costa Rica[J]. Forest Ecology and Management,2007, 241: 134–144.
    [49]王艳芬,陈佐忠,Larry T. Tieszen.人类活动对锡林郭勒地区主要草原土壤铵态氮分布的影响[J].植物生态学报,1998,22(6):545-551.
    [50]朱鹤健,何宜庚.土壤地理学[M].北京:高等教育出版社,1992.
    [51] R.M. Rees, I.J.Bingham, J.A. Baddeley, C.A. Watson. The role of plants and land management in sequestering soil carbon in temperate arable and grassland ecosystems[J].Geoderma, 2005,128:130–154.
    [52]李克让.土地利用变化和温室气体净排放与陆地生态系统碳循环[M].北京:气象出版社,2000.
    [53] Dalai R C,Chan K Y.Soil organic matter in rain fed cropping systems of the Australian cereal belt[J].Australian journal of Soil Research,2001,39:435-464.
    [54]刘满强,胡锋,陈小云.土壤铵态氮稳定机制研究进展[J].生态学报,2007,27(6):2642-2650.
    [55] Evrendilek F., Wali M.K.. Modelling long-term C dynamics in croplands in the context of climate change: a case study from Ohio[J]. Environmental Modelling and software,2001,16(04):361-375.
    [56]张国盛,黄高宝,YIN Chan.农田土壤铵态氮固定潜力研究进展[J].生态学报, 2005,25(2):351-357.
    [57]唐国勇,黄道友,童成立,张文菊,肖和艾,苏以荣,吴金水.红壤丘陵景观单元土壤铵态氮和微生物生物量碳含量特征[J].应用生态学报,2006,17(3):429-433.
    [58] Blair J G, Lefroy R D B, Lisle L. Soil carbon fractions based on the degree of oxidation and the development of a carbon management index for agricultural systems[J]. Austrian Journal of Agricultural Research, 1995, 46: 1459-1466.
    [59] Khanna P K, Kludwig B, Kbaybu S J,et al. Assessment and significance of labile organic C pools in forest soils[A ]. Lal R. KKimble J M .KFouen R. F Keds. Stewarteds. Assessment methods for soil carbon [C ]. Boca RatonK Florida. Lew is publishers. 2001,167- 182.
    [60]柳敏,宇万太,姜子绍,马强.土壤易氧化铵态氮[J].生态学杂志,2006, 25(11):1412-1417.
    [61] S. Hu, D.C. Coleman, C.R. Carroll, P.F. Hendrix, M.H. Beare. Labile soil carbon pools in subtropical forest and agricultural ecosystems as influenced by management practices and vegetation types[J]. Agriculture Ecosystems and Environment,1997(65):69-78.
    [62] Biederbeck B O, Zentner R P. Labile soil organic matter as influenced by cropping practices in an aridenvironment[J]. Soil Biology Biochemistry, 1994, 26(12): 1647-1656.
    [63]徐明岗,于荣,王伯仁.土壤活性有机质的研究进展[J].土壤肥料,2000(6):3-7.
    [64] Guo L.B., Gifford R.M.. Soil carbon stocks and land use change: a metaanalysis[J]. Global Change Biol., 2002, 8:345–360.
    [65]周莉,李保国,周广胜.土壤铵态氮的主导影响因子及其研究进展[J].地球科学进展,2005, 20(1):99-105.
    [66]欧阳学军,黄忠良,周国逸等.鼎湖山南亚热带森林群落演替对土壤化学性质影响的累积效应研究[J].水土保持学报,2003,17(4):51-54.
    [67]宇万太,马强,赵鑫,周桦,李建东.不同种植模式下土壤易氧化铵态氮库的变化[J].生态学杂志,2007,26(12):2013-2016.
    [68]赵世伟,吴金水等.子午岭北部不同植被类型土壤水分特征研究[J].水土保持学报,2002,16(4):119-122.
    [69]吴征镒,朱彦丞,姜汉侨等.云南植被[M].北京:科学出版社,1987.
    [70]叶功富,张清海,卢昌义,林益明.滨海沙地木麻黄林生态系统的凋落物及其热值研究[J].应用与环境生物学报,2007,13(1):23-28.
    [71]张庆费,由文辉,宋永昌.浙江天童植物群落演替对土壤化学性质的影响[J].应用生态学报,1999,10(1):19-22.
    [72]宇万太,姜子绍,李新宇,丁怀香.不同土地利用方式对潮棕壤铵态氮含量的影响[J].应用生态学报,2007,18(12):2760-2764.
    [73]邵月红,剑君,孙波.不同森林植被下土壤铵态氮的分解特征及碳库研究[J].水土保持学报,2005,19(3):24-28.
    [74]史奕,陈欣,杨雪莲,闻大中.土壤“慢”铵态氮库研究进展[J].生态学杂志,2003,22 (5):108~112.
    [75] Hua Zheng, Zhiyun Ouyan,et al. Variation of carbon storage by different reforestation types in the hilly red soil region of southern China[J]. Forest Ecology and Management, 2008, 255: 1113-1121.
    [76]张华,张甘霖.土壤质量指标和评价方法[J].土壤. 2001, 33(6): 326-330.
    [77]黄昌勇.土壤学[M].北京:中国农业出版社, 2000.

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