闽江河口湿地沉积物磷、硫及其分形研究
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摘要
以闽江河口区上、中、下段的尤溪洲、蝙蝠洲和鳝鱼滩湿地为研究区域,分别对鳝鱼滩芦苇、咸草和藨草湿地及尤溪洲和蝙蝠洲芦苇湿地沉积物P、S形态、含量和空间分布特征进行研究。结果表明：(1)闽江河口湿地沉积物OP含量范围为0.01～0.25g kg-1之间,占TP含量的1.9%～33.1%,构成OP的主要成分是MLOP和MROP,IP含量范围为0.13～1.44g kg-1之间,占TP含量的63.7%～98.5%,构成IP的主要成分是Ca-P和(Fe+Al)-P；TS含量在0.13～3.63 g kg-1之间,AS含量很少,只占TS含量的0.2%～9.5%。(2)鳝鱼滩芦苇湿地沉积物LOP、MLOP、Exch-P、(Fe+Al)-P、Ca-P及TS和AS含量均呈现出近潮沟>远潮沟的现象,差异显著(P<0.05),其余各组分含量差异不显著(P>0.05);咸草湿地各形态P含量呈现出近潮沟<远潮沟的现象,除了LOP、MROP和HROP含量在近潮沟和远潮沟区域差异显著外,其余组分含量差异不显著,TS和AS含量呈现出近潮沟>远潮沟的现象,差异极显著(P<0.01)；藨草湿地沉积物各形态P含量呈现出近潮沟>远潮沟的现象,差异极显著,TS和AS含量差异不显著。(3)位于闽江河口区下段的鳝鱼滩芦苇湿地沉积物各形态OP、TS和AS含量均大于上段和中段的尤溪洲和蝙蝠洲湿地,各形态IP含量则表现为蝙蝠洲湿地最大。
The Minjiang River estuary wetland is one of the most representative and typical estuary wetland in the southeast seashore of China. This article mainly studied on P and S fractions and contents in the sediments of the Youxizhou,Bianfuzhou and Shanyutan wetland. The results indicated:(1) The sediments OP concentration ranged between 0.01-0.25g kg-1, which account for 1.9%-33.1%, of which primary fractions are MLOP and MROP; IP concentration ranged between 0.13-1.44g kg-1, which account for 63.7%-98.5%, and Ca-P and (Fe+Al)-P are the primary fractions;TS concentration ranged between 0.13～3.63 g kg-1, and AS concentration account for 0.2%-9.5%。(2) The contents of LOP、MLOP、Exch-P、(Fe+Al)-P、Ca-P、TS and AS in the sediments which in the section near the tide ditch were higher significantly than that in the area far from the tide ditch in the Phragmites australis wetland of the Shanyutan; for the Cyperus malaccensis var. wetland in the Shanyutan, the contents of P fractions of the sediments which in the section near the tide ditch were lower than that in the area far from the tide ditch, and the contents of LOP、MROP and HROP which in the section far from the tide ditch were higher significantly than that in the area near the tide ditch, but other fractions of P contents in the sections far and near the tide ditch were similar, the contents of TS and AS which in the section near the tide ditch were higher significantly than that in the area far from the tide ditch;the contents of P fractions in the sediments of Scirpus triqueter wetland in the section near the tide ditch were higher significantly than that in the area far from the tide ditch of the Shanyutan, however the contents of Ts and AS in the sections far and near the tide ditch were similar。(3) Fractions of OP、TS and AS contents in the sediments of Phragmites australis wetland in the Shanyutan were higher than that in the Bianfuzhou and Youxizhou wetland, fractions of IP contents in the sediments of the Bianfuzhou Phragmites australis wetland were the higherst in the three studied wetlands。
The Minjiang River estuary wetland is one of the most representative and typical estuary wetland in the southeast seashore of China. This article mainly studied on P and S fractions and contents in the sediments of the Youxizhou,Bianfuzhou and Shanyutan wetland. The results indicated:(1) The sediments OP concentration ranged between 0.01-0.25g kg-1, which account for 1.9%-33.1%, of which primary fractions are MLOP and MROP; IP concentration ranged between 0.13-1.44g kg-1, which account for 63.7%-98.5%, and Ca-P and (Fe+Al)-P are the primary fractions;TS concentration ranged between 0.13～3.63 g kg-1, and AS concentration account for 0.2%-9.5%。(2) The contents of LOP、MLOP、Exch-P、(Fe+Al)-P、Ca-P、TS and AS in the sediments which in the section near the tide ditch were higher significantly than that in the area far from the tide ditch in the Phragmites australis wetland of the Shanyutan; for the Cyperus malaccensis var. wetland in the Shanyutan, the contents of P fractions of the sediments which in the section near the tide ditch were lower than that in the area far from the tide ditch, and the contents of LOP、MROP and HROP which in the section far from the tide ditch were higher significantly than that in the area near the tide ditch, but other fractions of P contents in the sections far and near the tide ditch were similar, the contents of TS and AS which in the section near the tide ditch were higher significantly than that in the area far from the tide ditch;the contents of P fractions in the sediments of Scirpus triqueter wetland in the section near the tide ditch were higher significantly than that in the area far from the tide ditch of the Shanyutan, however the contents of Ts and AS in the sections far and near the tide ditch were similar。(3) Fractions of OP、TS and AS contents in the sediments of Phragmites australis wetland in the Shanyutan were higher than that in the Bianfuzhou and Youxizhou wetland, fractions of IP contents in the sediments of the Bianfuzhou Phragmites australis wetland were the higherst in the three studied wetlands。
引文
[1]杨永兴,王世岩,何太蓉,等.三江平原典型湿地生态系统生物量及其季节动态研究[J].中国草地,2002,24(1)：1-7.
[2]Klump J V, Martens C S. Biogeochemical cycling in an organic rich coastal marine bassin-Ⅱ:Nutrinet sediment-water exchange processes[J]. Geochimica et Cosmochimica Acta,1981,45:101-12.
[3]尹大强,覃秋荣,阎航.环境因子对五里湖沉积物磷释放的影响[J].湖泊科学,1994,6(3)：240-244.
[4]Fielding P J, Damstra J, Branch G M. Benthic diatom biomass, production and sediment chlorophyll in Langebaan Lagoon, South Africa[J]. Estuarine, Coastal and Shelf Science,1988,27:413-426.
[5]Cahoon L B, Nearhoof J E, Tilton C L. Sediment gain size effect on benthic microalgal biomass in shallow aquatic ecosystems[J]. Estuarines,1999,22 (3B): 735-741.
[6]迟传德.安徽升金湖湿地土壤碳、磷的分布研究[D].南京农业大学土壤学专业硕士学位论文,2006.
[7]王国平,刘景双,张玉霞.向海湿地全硫与有效硫垂向分布[J].水土保持通报,2003,2(2)：5-8.
[8]Bowman R A, Cole C V. An exploratory method for fractionation of organic phosphorus from grassland soil[J]. Soil Science,1978,125:95-101.
[9]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,1999：16-170.
[10]Hedley M J, Stewart J W B, Chauhan B S. Changes in inorganic and organic soil phosphorus fractions induced by cultivation practices and by laboratory incubations [J]. Soil Sci Soc of Am J,1982,46:970-975.
[11]Tiessen H, Stewart J W B, Moir J O. Changes in organic and inorganic phosphorus composition of two grassland soils and their particle size fractions during 60-90 years of cultivation [J]. Journal of Soil Science,1983,34:815-823.
[12]贺铁,李世俊.Bowman-Cole土壤有机磷分组方法的探讨[J].土壤学报,1987, 24(2)：152-159.
[13]Chang S C, Jackson M L. Fractionation of soil phosphorus in soil[J]. Soil Science, 1957,84:1334-1347.
[14]蒋柏藩,顾益初.石灰性土壤无机磷分级体系的研究[J].中国农业科学,1989,22(3)：58-66.
[15]顾益初,蒋柏藩.石灰性土壤无机磷的测定方法[J].土壤,1990,22(2)：101-102.
[16]刘敏,陆敏,许世远,等.长江河口及其上海岸带水体沉积物中磷的存在形态[J].地学前缘,2000,7(增刊)：94-98.
[17]侯立军,刘敏,许世远,等.长江口岸带柱状沉积物中磷的存在形态及其环境意义[J].海洋学报,2001,20(2)： 7-12.
[18]李敏,韦鹤平,王光谦,等.长江口、杭州湾水域沉积物中磷的化学形态分布特征[J].海洋学报,2004,26(2)：125-131.
[19]高效江,陈振楼,许世远,等.长江口滨岸潮滩沉积物中磷的环境地球化学特征[J].环境科学学报,2003,23(6)：713-715.
[20]邓焕广,陈振楼,张兴正.长江口潮滩表层样中分级磷的时空变化[J].国土与自然资源研究,2004,3： 56-57.
[21]刘绿叶,高效江,陈卓敏,等.长江口潮滩沉积物中磷的分布和形态特征[J].复旦学报(自然科学版)2005,44(6)：1033-1036.
[22]徐明德,韦鹤平,李敏,等.长江口泥沙和沉积物中磷酸盐存在形态的研究[J].四川环境,2006,25(1)：52-54.
[23]侯立军,陆健健,刘敏,等.长江口沙洲表层沉积物磷的赋存形态及生物有效性[J].环境科学学报,2006,26(3)：488-494.
[24]李莹,周新革,郭博书.黄河(黄河口、渤海、三门峡)沉积物中磷的赋存形态[J].集宁师专学报,2008,30(4)：38-40.
[25]林荣根,吴景阳.黄河口沉积物中无机磷酸盐的存在形态[J].海洋与湖沼,1992,23(4)：387-395.
[26]陈松,廖文卓,许爱玉.九龙江口磷的界面分配和转移[J].台湾海峡,1997,16(3)：293-297.
[27]何清溪.大亚湾沉积物中磷的化学形态分布特征[J].海洋环境科学,1990,9 (4)：6-10.
[28]扈传昱,潘建明,刘小涯.珠江口沉积物中磷的赋存形态[J].海洋环境科学,2001,20(4)：21-25.
[29]岳维忠,黄小平,孙翠慈.珠江口表层沉积物中氮、磷的形态分布特征及污染评价[J].海洋与湖沼,2007,38(2)：111-117.
[30]岳维忠,黄小平.珠江口柱状沉积物中磷的分布特征及其环境意义[J].热带海洋学报,2005,24(1)：21-27.
[31]许金树,李亮歌,台湾海峡中、北部沉积物中磷的存在形态[J].海洋与湖沼,1990,21(1)：62-69.
[32]Koch M S, Benz R E, Rudnick D T. Solid-phase phosphorus pools in highly organic carbonate sediments of northeastern Florida bay, Estuarine[J].Coastal and Shelf Science,2001, Vol,52,279-291.
[33]MorseJ W, Cook N. The distribution and form of phosphorus in North Atlantic Ocean deep-sea and continetal slope sediments [J]. Limnology and Oceanography, 1978,23 (3):825-830.
[34]Yamada H, Kayama M. Distribution and dissolution of several forms of phosphorus in coastal marine sediments[J]. Oceanal Acta,1987,10(3):311-321.
[35]李金,董巧香,杜虹,等.柘林湾表层沉积物中氮和磷的时空分布[J],海洋环境科学,2004,23(4)：63-71.
[36]Andrieux-Layer F, Aminot A. Phosphorus forms related to sediment grain size and geochemical characteristics in French coastal areas. Estuarine[J],Coastal and Shelf Science,2001,52:617-629.
[37]刘巧梅,刘敏,许世远,等.上海滨岸潮滩不同粒径沉积物中无机形态磷的分布特征[J].海洋环境科学,2002,21(3)：23-33.
[38]刘敏,侯立军,许世远,等.长江河口潮滩表层沉积物对磷酸盐的吸附特征[J].地理学报,2002,57(4)：397-406.
[39]王爱萍,杨守业,周琪.长江口崇明东滩湿地沉积物对磷的吸附特征[J].生态学杂志,2006,25(8)：926-930.
[40]白军红,余国营,张玉霞.向海湿地土壤中无机磷酸盐的存在形态研究[J].水土保持学报,2001,15(1)：98-101.
[41]Sondergarrd M, Windolf J, Jeppesen E. Phosphorus fractions and profiles in the sediment of shallow Danish lakes as related to phosphorus load, sediment composition and lake chemistry [J]. Wat Res,1996,30 (4):992-1002.
[42]Schnug E. Sulfur nutritional status of European crops and consequences for agriculture [J]. Sulfur Agtic,1991,15:7-12.
[43]罗奇祥.土壤硫素状况及其测试法[J].江西农业学报,1994,6(2)：135-143.
[44]单孝全,陈斌,铁军,等.土壤和河流沉积物中硫的形态分析[J].环境科学学报,1991,11(2)：172-177.
[45]于泽民,付国臣.土壤中硫的形态分析及其测定方法研究进展[J].内蒙古环境科学,2009,21(4)：94-96.
[46]Tabatabai M A, Payne A L, Freney J R, et al. Methods of soil Analysis. Part2: Chemical and Microbiological properties[M]. American Society of Agronomy.1982,501-538.
[47]Freney J R. Soil observations on the nature of organic sulphur compounds in soils [J]. Aust Agric.Res,1961,12:424-432.
[48]迟凤琴.东北地区黑土硫素形态分布及其有效性的研究[D].沈阳农业大学土壤学专业博士学位论文,2003.
[49]幸颖,刘常宏,安树青.海岸盐沼湿地土壤硫循环中的微生物及其作用[J].生态学杂志,2007,26(4)：577-581.
[50]刘崇群,曹淑卿,陈国安.中国南方农业中的硫[J].土壤学报,1990,27(4)：398-404.
[51]Tabatabai M A. J M Bremner. Forms of sulfur and carbon, nitrogen and sulfur relationships in Lowa sols [J]. Soil Science,1972,114(5):380-385.
[52]孙建中,戴昭华,盛学斌.华北地区土壤中硫的赋存特征[J].环境科学学报,1997,17(2)：187-192.
[53]郝庆菊,王起超,王跃思.三江平原典型湿地土壤中硫的分布特征[J].土壤通报,2004,35(3)：331-335.
[54]郝庆菊,王起超,王跃思.三江平原典型湿地土壤植物总硫及水中硫酸盐的分布特征[J].生态环境,2003,12(4)：401-404.
[55]郝庆菊,王起超,王跃思,等.开垦利用对三江平原湿地土壤硫含量的影响 [J].环境科学学报,2003,23(5)：614-618.
[56]郝庆菊,王起超,王其存,等.三江平原典型湿地及其开垦后土壤中总硫变化的初步研究[J].应用生态学报,2003,14(12)：2191-2194.
[57]李新华,刘景双,孙志高.三江平原小叶樟湿地植物-土壤系统中硫素分布及季节变化动态[J].土壤通报,2007,38(1)：85-88.
[58]李新华,刘景双,孙晓军,等.三江平原小叶樟湿地土壤硫的组成与垂直分布[J].生态与农村环境学报,2009,25(2)：34-38.
[59]李新华,刘景双,孙志高,等.三江平原小叶樟湿地生态系统硫的生物地球化学循环[J].生态学报,2007,27(6)：1999-2207.
[60]李新华,刘景双,杨继松.三江平原小叶樟湿地枯落物和根分解及其硫元素释放动态[J].湿地科学,2007,5(1)：76-82.
[61]李新华,刘景双.三江平原小叶樟湿地土壤有机硫矿化特征[J].农业系统科学与综合研究,2007,23(1)：86-94.
[62]张汝国.珠江口红树林硫的累积和循环研究[J].热带亚热带土壤科学,1996,5(2)：67-73.
[63]廖家隆,姚素平,丁海.滨海红树林泥炭沉积物中硫的赋存特点及其控制因素[J].高效地质学报,2008,14(4)：620-630.
[64]陈皓文,徐家声.北部湾东侧沉积物硫酸盐还原菌含量及其意义[J].广西科学院学报,1999,15(3)：103-107.
[65]陈皓文.胶州湾潮间带和沿岸区硫酸盐还原菌含量分布[J].海洋环境科学,1999,18(2)：27-30.
[66]高爱国,陈皓文,孙海青.北极沉积物中硫酸盐还原菌与生物地球化学要素的相关分析[J].环境科学学报,2003,23(5)：619-624.
[67]陈皓文,李培英,王波.浙江-闽北陆架沉积物硫酸盐还原菌及与生物地球化学因子关系的分析[J].环境科学学报,2000,20(4)：478-482.
[68]刘剑秋,曾从盛,陈宁.闽江河口湿地研究[M].北京：科学出版社,2006.
[69]金相灿.湖泊富营养化调查规范[M].北京：中国环境科学出版社,1990.
[70]翟继红,曾从盛,仝川,等.闽江河口湿地沉积物有机磷和无机磷含量及垂直分布特征[J].亚热带资源与环境学报,2010,5(1)：9-14.
[71]刘崇群.中国南方土壤硫的状况和对硫肥的需求[J].磷肥与复肥,1995,3： 14-18.
[72]李峥,沈志良,周淑青,等.长江口及其邻近海域磷的分布变化特征[J].海洋科学,2007,31(1)：28-36.
[73]黄自强,暨卫东.长江口水体中总磷、有机磷、磷酸盐的变化特征及相互关系[J].海洋学报,1994,16(1)：51-60.
[74]Fang T H. Partitioning and behavior of different forms of phosphorus in the Tanshui estury and one of its tributaries, Northern Taiwan [J]. Estuarine, Coastal and Shelf Science,2000,50:689-701.
[75]Nixon S W. The fate of nitrogen and phosphorus at the land-sea margin of the North Atlantic Ocean [J]. Biogeochemisty,1996,35:141-180.
[76]Francoise A, lain A. A two-year survey of phosphorus speciation in the sediments of the Bay of Seine(France) [J]. Continental Shelf Rearch,1997,17 (10): 1229-1245.
[77]陆健健,何文珊,童春富,等.湿地生态学[M].高等教育出版社,2006.
[78]王爱萍.长江口滨海湿地磷的迁移转化及净化功能的研究[D].同济大学环境科学与工程学院博士学位论文,2005.
[79]徐宏伟.三江平原小叶樟湿地生态系统对氮磷净化功能研究[D].中国科学院环境研究中心学位论文,2005.
[80]吴振斌,陈辉蓉,贺峰等.人工湿地系统对污水磷的净化效果[J].水生生物学报,2001,25(1)：28-35.
[81]杨昌风,谢其明.模拟人工湿地处理污水的实验研究[J].应用生态学报,1991,2(4)：350-354.
[82]吴晓磊.人工湿地废水处理机理[J].环境科学,1995,16(3)：83-86.
[83]House C H, Broome S W, Hoover M T. Treatment of nitrogen and phosphorus by a constructed upland-wetland wastewater treatment system [J]. Water Science and Technology,1994,29 (4):177-184.
[84]李科德,胡正嘉.人工模拟芦苇床系统处理污水的效能[J].华中农业大学学报,1994,13(5)：511-517.
[85]王卫东,王大力,尹澄清等.芦苇型湿地生态系统的潜水水质状态研究[J].生态学报,2001,21(6)：919-926.
[86]Walsh, J J. The role of ocean biota in accelerated ecological cycles:A temporal view[J]. BioScience,1984,34 (4):495-507.
[87]贾瑞霞.闽江河口湿地沉积物碳、氮、磷含量及储量特征[D].福建师范大学地理科学学院硕士学位论文,2009.
[88]Vale'ryl L, Bouchard V, Lefeuvre J. Impact of the invasive native species Elymus athericus on carbon pools in a salt marsh [J]. Wetlands,2004,24(2):268-276.
[89]欧冬妮,刘敏,侯立军,等.长江口潮滩植物根际沉积物磷的累积及其生物有效性[J].土壤通报,2004,35(3)：290-294.
[90]刘敏、侯立军、许世远,等.盐度变化对崇明东部河口潮滩氮营养盐循环影响实验模拟研究[J].海洋环境科学,2004,23(4)：6-9.
[91]吕晓霞,翟世奎,于增慧,等.长江口内外表层沉积物中营养元素的分布特征研究[J].海洋通报,2005,24(2)：40-45.
[92]李敏,倪晋仁,王光谦,等.环境因素对长江口水域沉积物吸附磷酸盐的影响研究[J].应用基础与工程科学学报,205,13(1)：19-25.
[93]胡玲珍,陈振楼.河口沉积物反硝化反应影响因素综述[J].环境科学动态,2003,4：41-43.
[94]侯立军,许世远.长江河口潮滩表层沉积物对磷酸盐的吸附作用[J].海洋环境科学,2002,57(4)：397-406.
[95]Hisashi J. Fractionation of phosphorus and releasable fraction in sediment mud of Osaka Bay [J]. Bull Jap Soc Sci Fish,1983,49 (3):447-454.
[96]商少凌,洪华生.厦门西海域磷的研究[J].海洋环境科学,1996,15(1)：15-21.
[97]Salomons W, Gerritse R G. Some observations on the occurrence of phosphorus in recent sediments from Western Europe [J]. The Science of the Total Environment, 1981,17:37-49.
[98]蔡爱智.粤东柘林湾的泥沙来源和沉积环境[J].厦门大学学报(自然科学版),1994,33(4)：515-520.
[99]任伟,尚榆民.洱海环境沉积学研究[J].沉积学报,2003,7：46-48.
[2]Klump J V, Martens C S. Biogeochemical cycling in an organic rich coastal marine bassin-Ⅱ:Nutrinet sediment-water exchange processes[J]. Geochimica et Cosmochimica Acta,1981,45:101-12.
[3]尹大强,覃秋荣,阎航.环境因子对五里湖沉积物磷释放的影响[J].湖泊科学,1994,6(3)：240-244.
[4]Fielding P J, Damstra J, Branch G M. Benthic diatom biomass, production and sediment chlorophyll in Langebaan Lagoon, South Africa[J]. Estuarine, Coastal and Shelf Science,1988,27:413-426.
[5]Cahoon L B, Nearhoof J E, Tilton C L. Sediment gain size effect on benthic microalgal biomass in shallow aquatic ecosystems[J]. Estuarines,1999,22 (3B): 735-741.
[6]迟传德.安徽升金湖湿地土壤碳、磷的分布研究[D].南京农业大学土壤学专业硕士学位论文,2006.
[7]王国平,刘景双,张玉霞.向海湿地全硫与有效硫垂向分布[J].水土保持通报,2003,2(2)：5-8.
[8]Bowman R A, Cole C V. An exploratory method for fractionation of organic phosphorus from grassland soil[J]. Soil Science,1978,125:95-101.
[9]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,1999：16-170.
[10]Hedley M J, Stewart J W B, Chauhan B S. Changes in inorganic and organic soil phosphorus fractions induced by cultivation practices and by laboratory incubations [J]. Soil Sci Soc of Am J,1982,46:970-975.
[11]Tiessen H, Stewart J W B, Moir J O. Changes in organic and inorganic phosphorus composition of two grassland soils and their particle size fractions during 60-90 years of cultivation [J]. Journal of Soil Science,1983,34:815-823.
[12]贺铁,李世俊.Bowman-Cole土壤有机磷分组方法的探讨[J].土壤学报,1987, 24(2)：152-159.
[13]Chang S C, Jackson M L. Fractionation of soil phosphorus in soil[J]. Soil Science, 1957,84:1334-1347.
[14]蒋柏藩,顾益初.石灰性土壤无机磷分级体系的研究[J].中国农业科学,1989,22(3)：58-66.
[15]顾益初,蒋柏藩.石灰性土壤无机磷的测定方法[J].土壤,1990,22(2)：101-102.
[16]刘敏,陆敏,许世远,等.长江河口及其上海岸带水体沉积物中磷的存在形态[J].地学前缘,2000,7(增刊)：94-98.
[17]侯立军,刘敏,许世远,等.长江口岸带柱状沉积物中磷的存在形态及其环境意义[J].海洋学报,2001,20(2)： 7-12.
[18]李敏,韦鹤平,王光谦,等.长江口、杭州湾水域沉积物中磷的化学形态分布特征[J].海洋学报,2004,26(2)：125-131.
[19]高效江,陈振楼,许世远,等.长江口滨岸潮滩沉积物中磷的环境地球化学特征[J].环境科学学报,2003,23(6)：713-715.
[20]邓焕广,陈振楼,张兴正.长江口潮滩表层样中分级磷的时空变化[J].国土与自然资源研究,2004,3： 56-57.
[21]刘绿叶,高效江,陈卓敏,等.长江口潮滩沉积物中磷的分布和形态特征[J].复旦学报(自然科学版)2005,44(6)：1033-1036.
[22]徐明德,韦鹤平,李敏,等.长江口泥沙和沉积物中磷酸盐存在形态的研究[J].四川环境,2006,25(1)：52-54.
[23]侯立军,陆健健,刘敏,等.长江口沙洲表层沉积物磷的赋存形态及生物有效性[J].环境科学学报,2006,26(3)：488-494.
[24]李莹,周新革,郭博书.黄河(黄河口、渤海、三门峡)沉积物中磷的赋存形态[J].集宁师专学报,2008,30(4)：38-40.
[25]林荣根,吴景阳.黄河口沉积物中无机磷酸盐的存在形态[J].海洋与湖沼,1992,23(4)：387-395.
[26]陈松,廖文卓,许爱玉.九龙江口磷的界面分配和转移[J].台湾海峡,1997,16(3)：293-297.
[27]何清溪.大亚湾沉积物中磷的化学形态分布特征[J].海洋环境科学,1990,9 (4)：6-10.
[28]扈传昱,潘建明,刘小涯.珠江口沉积物中磷的赋存形态[J].海洋环境科学,2001,20(4)：21-25.
[29]岳维忠,黄小平,孙翠慈.珠江口表层沉积物中氮、磷的形态分布特征及污染评价[J].海洋与湖沼,2007,38(2)：111-117.
[30]岳维忠,黄小平.珠江口柱状沉积物中磷的分布特征及其环境意义[J].热带海洋学报,2005,24(1)：21-27.
[31]许金树,李亮歌,台湾海峡中、北部沉积物中磷的存在形态[J].海洋与湖沼,1990,21(1)：62-69.
[32]Koch M S, Benz R E, Rudnick D T. Solid-phase phosphorus pools in highly organic carbonate sediments of northeastern Florida bay, Estuarine[J].Coastal and Shelf Science,2001, Vol,52,279-291.
[33]MorseJ W, Cook N. The distribution and form of phosphorus in North Atlantic Ocean deep-sea and continetal slope sediments [J]. Limnology and Oceanography, 1978,23 (3):825-830.
[34]Yamada H, Kayama M. Distribution and dissolution of several forms of phosphorus in coastal marine sediments[J]. Oceanal Acta,1987,10(3):311-321.
[35]李金,董巧香,杜虹,等.柘林湾表层沉积物中氮和磷的时空分布[J],海洋环境科学,2004,23(4)：63-71.
[36]Andrieux-Layer F, Aminot A. Phosphorus forms related to sediment grain size and geochemical characteristics in French coastal areas. Estuarine[J],Coastal and Shelf Science,2001,52:617-629.
[37]刘巧梅,刘敏,许世远,等.上海滨岸潮滩不同粒径沉积物中无机形态磷的分布特征[J].海洋环境科学,2002,21(3)：23-33.
[38]刘敏,侯立军,许世远,等.长江河口潮滩表层沉积物对磷酸盐的吸附特征[J].地理学报,2002,57(4)：397-406.
[39]王爱萍,杨守业,周琪.长江口崇明东滩湿地沉积物对磷的吸附特征[J].生态学杂志,2006,25(8)：926-930.
[40]白军红,余国营,张玉霞.向海湿地土壤中无机磷酸盐的存在形态研究[J].水土保持学报,2001,15(1)：98-101.
[41]Sondergarrd M, Windolf J, Jeppesen E. Phosphorus fractions and profiles in the sediment of shallow Danish lakes as related to phosphorus load, sediment composition and lake chemistry [J]. Wat Res,1996,30 (4):992-1002.
[42]Schnug E. Sulfur nutritional status of European crops and consequences for agriculture [J]. Sulfur Agtic,1991,15:7-12.
[43]罗奇祥.土壤硫素状况及其测试法[J].江西农业学报,1994,6(2)：135-143.
[44]单孝全,陈斌,铁军,等.土壤和河流沉积物中硫的形态分析[J].环境科学学报,1991,11(2)：172-177.
[45]于泽民,付国臣.土壤中硫的形态分析及其测定方法研究进展[J].内蒙古环境科学,2009,21(4)：94-96.
[46]Tabatabai M A, Payne A L, Freney J R, et al. Methods of soil Analysis. Part2: Chemical and Microbiological properties[M]. American Society of Agronomy.1982,501-538.
[47]Freney J R. Soil observations on the nature of organic sulphur compounds in soils [J]. Aust Agric.Res,1961,12:424-432.
[48]迟凤琴.东北地区黑土硫素形态分布及其有效性的研究[D].沈阳农业大学土壤学专业博士学位论文,2003.
[49]幸颖,刘常宏,安树青.海岸盐沼湿地土壤硫循环中的微生物及其作用[J].生态学杂志,2007,26(4)：577-581.
[50]刘崇群,曹淑卿,陈国安.中国南方农业中的硫[J].土壤学报,1990,27(4)：398-404.
[51]Tabatabai M A. J M Bremner. Forms of sulfur and carbon, nitrogen and sulfur relationships in Lowa sols [J]. Soil Science,1972,114(5):380-385.
[52]孙建中,戴昭华,盛学斌.华北地区土壤中硫的赋存特征[J].环境科学学报,1997,17(2)：187-192.
[53]郝庆菊,王起超,王跃思.三江平原典型湿地土壤中硫的分布特征[J].土壤通报,2004,35(3)：331-335.
[54]郝庆菊,王起超,王跃思.三江平原典型湿地土壤植物总硫及水中硫酸盐的分布特征[J].生态环境,2003,12(4)：401-404.
[55]郝庆菊,王起超,王跃思,等.开垦利用对三江平原湿地土壤硫含量的影响 [J].环境科学学报,2003,23(5)：614-618.
[56]郝庆菊,王起超,王其存,等.三江平原典型湿地及其开垦后土壤中总硫变化的初步研究[J].应用生态学报,2003,14(12)：2191-2194.
[57]李新华,刘景双,孙志高.三江平原小叶樟湿地植物-土壤系统中硫素分布及季节变化动态[J].土壤通报,2007,38(1)：85-88.
[58]李新华,刘景双,孙晓军,等.三江平原小叶樟湿地土壤硫的组成与垂直分布[J].生态与农村环境学报,2009,25(2)：34-38.
[59]李新华,刘景双,孙志高,等.三江平原小叶樟湿地生态系统硫的生物地球化学循环[J].生态学报,2007,27(6)：1999-2207.
[60]李新华,刘景双,杨继松.三江平原小叶樟湿地枯落物和根分解及其硫元素释放动态[J].湿地科学,2007,5(1)：76-82.
[61]李新华,刘景双.三江平原小叶樟湿地土壤有机硫矿化特征[J].农业系统科学与综合研究,2007,23(1)：86-94.
[62]张汝国.珠江口红树林硫的累积和循环研究[J].热带亚热带土壤科学,1996,5(2)：67-73.
[63]廖家隆,姚素平,丁海.滨海红树林泥炭沉积物中硫的赋存特点及其控制因素[J].高效地质学报,2008,14(4)：620-630.
[64]陈皓文,徐家声.北部湾东侧沉积物硫酸盐还原菌含量及其意义[J].广西科学院学报,1999,15(3)：103-107.
[65]陈皓文.胶州湾潮间带和沿岸区硫酸盐还原菌含量分布[J].海洋环境科学,1999,18(2)：27-30.
[66]高爱国,陈皓文,孙海青.北极沉积物中硫酸盐还原菌与生物地球化学要素的相关分析[J].环境科学学报,2003,23(5)：619-624.
[67]陈皓文,李培英,王波.浙江-闽北陆架沉积物硫酸盐还原菌及与生物地球化学因子关系的分析[J].环境科学学报,2000,20(4)：478-482.
[68]刘剑秋,曾从盛,陈宁.闽江河口湿地研究[M].北京：科学出版社,2006.
[69]金相灿.湖泊富营养化调查规范[M].北京：中国环境科学出版社,1990.
[70]翟继红,曾从盛,仝川,等.闽江河口湿地沉积物有机磷和无机磷含量及垂直分布特征[J].亚热带资源与环境学报,2010,5(1)：9-14.
[71]刘崇群.中国南方土壤硫的状况和对硫肥的需求[J].磷肥与复肥,1995,3： 14-18.
[72]李峥,沈志良,周淑青,等.长江口及其邻近海域磷的分布变化特征[J].海洋科学,2007,31(1)：28-36.
[73]黄自强,暨卫东.长江口水体中总磷、有机磷、磷酸盐的变化特征及相互关系[J].海洋学报,1994,16(1)：51-60.
[74]Fang T H. Partitioning and behavior of different forms of phosphorus in the Tanshui estury and one of its tributaries, Northern Taiwan [J]. Estuarine, Coastal and Shelf Science,2000,50:689-701.
[75]Nixon S W. The fate of nitrogen and phosphorus at the land-sea margin of the North Atlantic Ocean [J]. Biogeochemisty,1996,35:141-180.
[76]Francoise A, lain A. A two-year survey of phosphorus speciation in the sediments of the Bay of Seine(France) [J]. Continental Shelf Rearch,1997,17 (10): 1229-1245.
[77]陆健健,何文珊,童春富,等.湿地生态学[M].高等教育出版社,2006.
[78]王爱萍.长江口滨海湿地磷的迁移转化及净化功能的研究[D].同济大学环境科学与工程学院博士学位论文,2005.
[79]徐宏伟.三江平原小叶樟湿地生态系统对氮磷净化功能研究[D].中国科学院环境研究中心学位论文,2005.
[80]吴振斌,陈辉蓉,贺峰等.人工湿地系统对污水磷的净化效果[J].水生生物学报,2001,25(1)：28-35.
[81]杨昌风,谢其明.模拟人工湿地处理污水的实验研究[J].应用生态学报,1991,2(4)：350-354.
[82]吴晓磊.人工湿地废水处理机理[J].环境科学,1995,16(3)：83-86.
[83]House C H, Broome S W, Hoover M T. Treatment of nitrogen and phosphorus by a constructed upland-wetland wastewater treatment system [J]. Water Science and Technology,1994,29 (4):177-184.
[84]李科德,胡正嘉.人工模拟芦苇床系统处理污水的效能[J].华中农业大学学报,1994,13(5)：511-517.
[85]王卫东,王大力,尹澄清等.芦苇型湿地生态系统的潜水水质状态研究[J].生态学报,2001,21(6)：919-926.
[86]Walsh, J J. The role of ocean biota in accelerated ecological cycles:A temporal view[J]. BioScience,1984,34 (4):495-507.
[87]贾瑞霞.闽江河口湿地沉积物碳、氮、磷含量及储量特征[D].福建师范大学地理科学学院硕士学位论文,2009.
[88]Vale'ryl L, Bouchard V, Lefeuvre J. Impact of the invasive native species Elymus athericus on carbon pools in a salt marsh [J]. Wetlands,2004,24(2):268-276.
[89]欧冬妮,刘敏,侯立军,等.长江口潮滩植物根际沉积物磷的累积及其生物有效性[J].土壤通报,2004,35(3)：290-294.
[90]刘敏、侯立军、许世远,等.盐度变化对崇明东部河口潮滩氮营养盐循环影响实验模拟研究[J].海洋环境科学,2004,23(4)：6-9.
[91]吕晓霞,翟世奎,于增慧,等.长江口内外表层沉积物中营养元素的分布特征研究[J].海洋通报,2005,24(2)：40-45.
[92]李敏,倪晋仁,王光谦,等.环境因素对长江口水域沉积物吸附磷酸盐的影响研究[J].应用基础与工程科学学报,205,13(1)：19-25.
[93]胡玲珍,陈振楼.河口沉积物反硝化反应影响因素综述[J].环境科学动态,2003,4：41-43.
[94]侯立军,许世远.长江河口潮滩表层沉积物对磷酸盐的吸附作用[J].海洋环境科学,2002,57(4)：397-406.
[95]Hisashi J. Fractionation of phosphorus and releasable fraction in sediment mud of Osaka Bay [J]. Bull Jap Soc Sci Fish,1983,49 (3):447-454.
[96]商少凌,洪华生.厦门西海域磷的研究[J].海洋环境科学,1996,15(1)：15-21.
[97]Salomons W, Gerritse R G. Some observations on the occurrence of phosphorus in recent sediments from Western Europe [J]. The Science of the Total Environment, 1981,17:37-49.
[98]蔡爱智.粤东柘林湾的泥沙来源和沉积环境[J].厦门大学学报(自然科学版),1994,33(4)：515-520.
[99]任伟,尚榆民.洱海环境沉积学研究[J].沉积学报,2003,7：46-48.