珠江口夏季水体中的氮和磷

林以安; 苏纪兰; 扈传昱; 张美; 李炎; 管卫兵; 陈介中

珠江口夏季水体中的氮和磷

1.
国家海洋局, 第二海洋研究所, 浙江, 杭州, 310012;国家海洋局海洋动力过程和卫星海洋学重点实验室, 浙江, 杭州, 310012;香港科技大学, 香港, 九龙, 清水湾
2.
国家海洋局, 第二海洋研究所, 浙江, 杭州, 310012;国家海洋局海洋动力过程和卫星海洋学重点实验室, 浙江, 杭州, 310012
3.
香港科技大学, 香港, 九龙, 清水湾

基金项目: 香港赛马会慈善信托基金会资助项目;国家重点基础研究发展规划资助项目(G1999043704).

计量
- 文章访问数: 1001
- HTML全文浏览量: 22
- PDF下载量: 1610
- 被引次数: 0
出版历程
- 收稿日期: 2002-08-23
- 修回日期: 2003-11-07

N and P in waters of the Zhujiang River Estuary in summer

1.
Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;Key Laboratorg of Ocean Dynamic Processes and Satellite Oceanography of State Oceanic Aministration, Hangzhou 310012, China;Center for Coastal and Atmospheric Research, Hong Kong University of Science and Technology (HKUST), Clear Water Bay, Kowloon, Hong Kong, China
2.
Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;Key Laboratorg of Ocean Dynamic Processes and Satellite Oceanography of State Oceanic Aministration, Hangzhou 310012, China
3.
Center for Coastal and Atmospheric Research, Hong Kong University of Science and Technology (HKUST), Clear Water Bay, Kowloon, Hong Kong, China

摘要

摘要: 根据1999年7月17～28日于珠江口现场调查和实验的资料,研究夏季水体中氮、磷的分布、形态变化和初级生产力的限制因素.结果表明该海域氮含量高,N/P属于世界上高值区之一.从河口向外海运输过程中,氮和磷的形态和浓度均有剧烈的变化.虽然氮在中途中有新源的补充;但由于外海水的入侵稀释、生物吸收和形态变化的迁移作用,NO₃^-和可溶无机氮的浓度总的变化趋势仍是随盐度增大而大幅度地降低,以至珠江口外出现N/P低于16.由于夏季水体层化稳定,在表、底层其生物地球化学变化方向相反,PO₄³的浓度变化互成镜像关系并可按盐度分为3段不同特征的反应区.初级生产力的限制因素在大部分区域是磷,但从口门至最大浑浊带和口外区则分别是浊度(或光照)及可溶无机氮.现场培养实验再现了真光层和底层氮和磷的生物地球化学过程差异并表明磷的循环和再生比氮迅速;在可溶无机氮浓度大且高N/P的海域,磷的再生可成为水华的引发因素,而氮被耗尽却是水华消亡的原因.总体上夏季该区水体氮的迁出率比磷高.于水体层化稳定的区域,氮和磷的生物地球化学作用在真光层以浮游生物吸收占优势、在下层以有机物的降解和可溶无机态的再生为主,当层化消失、上下水体充分混合则可完成循环.
- 氮 /
- 磷 /
- 形态变化 /
- 限制因素 /
- 珠江口
Abstract: Based on the data obtained by field survey and experiments of the Zhujiang River Estuary during July 17~28,1999,the cycle,regeneration and restriction of N and P in water masses are studied.The results show that there is a large content of N in the Zhujiang River Estuary waters,and it belongs to a high N/P area in the world.With the water mass transported from river to sea,the speciation and concentration of N and P present a violent variation in the waters.Among others,there is new supply on the N,and the supplemental volume may be even larger than the absorbing capacity of plankton photosynthesis somew here.Because of plankton absorbing,migration action of species variation and being intruded and being diluted by the seawater,the concentration of DIN was so constantly reduced and that the N/P was even lower than 16 off the Zhujiang River Estuary.The variation of concentration of PO₄^3- become mirror image each other between the surface layer and the bottom layer water,which indicates that both the directions of biogeochemicalaction of P are contrary.The plankton absorbing is primary process in the surface layer,but the regeneration takes precedence in the middle layer and the bottom layer.Comparatively speaking,one point is the migrationratio of DIN is greater than DIP and the other is the turbidity (or light),P and N are the limit factors of the primary productivity in three areas (from the river gate to the maximum turbidity zone,middle waters of the estuary and off the estuary) respectively.The results of incubation show that the bloom of plankton lead to the considerabl decrease of concentration of DIN,but the concentration of PO₄^3- is in a small scope vibration and keeps a more steady concentration level.It is inferred that the cycle and regeneration of P are more rapid than N,and the regeneration of P can direct supply primary product in euphotic and become a factor bringing to the plankton bloom in the waters,but the reason of the bloom passing away is the DIN being used up in the end.Through contrast study of biogeochemical cycle of N and P,similarities and differences of the process of cycle and regeneration between N and P are explicated,and infer potentiality of the denitrification action in the hypoxia area is inferred.
- nitrogen /
- phosphorus /
- variation of speciation /
- restriction factor /
- Zhujiang River Estuary

HTML全文

参考文献(24)

胡明辉,杨逸萍,徐春林,等.长江口浮游植物生长的磷酸盐限制[J].海洋学报,1989,11(4):439-443.

WANG Z.Evaluation of water quality in the Zhujiang Estuary,China[A].TOMOTOSHI O,DONALD M A,TAKAHISA Ned.Red Tides Biology,Environmental Science and Toxicology[M].Newyork:Elsevier,1989.109-112.

YANG D B.Nutrients and chlorophyll a variation during red tides in Jinhae Bay,Korea[A].TOMOTOSHI Okaichi,DONALD M Anderson,TAKAHISA Nemato.Red Tides Biology,Environmental Science and Toxicology[M].New york:Elsevier,1989.237-240.

MEYBECK M,CAUWET G,DESSERG S,et al.Nutrients (organic C,P,N,Si) in the eutrophic River Loire (France)and its estuary[J].Estuarine,Coastal and Shelf Science,1988,27:595-624.

POKRYFKI L,RANDALL R E,Nearshore hypoxia in the bottom water of the northwestern Gulf of Mexico from 1981 to1984[J].Mar Envtl Res,1987,22:75-90.

TURNER E,RABALAIS N N.Coastal eutrophication near the Mississippi River Delta[J].Nature,1994,368:619-621.

PAKULSKI J D.Microbial metabolism and nutrient cycling in the Mississippi and Atchafalaya River[J].Plumes Estuarine,Coastal and Shelf Science,2000,50:173-184.

GARBER J H.Laboratory study of nitrogen and phosphorus remineralization during the decomposition of coastal plankton[J].Estuarine,Coastal and Shelf Science,1984,18:685-702.

RENDEL A R,HORROBIN T M,JICKELLS T D,et al.Nutrient cycling in the Great Ouse Estuary and its impact on nutrient fluxes to the Wash,England[J].Estuarine,Coastal and Shelf Science,1997,45:653-668.

HUDSON J J,TAYLOR W D.Measuring regeneration of dissolved phosphorus in planktonic communities [J].Limnol Oceanoger,1996,41:1 560-1 565.

DOWNING J A.Marine nitrogen:phosphorus stoichiometry and the global N:P cycle[J].Biogeochemistry,1997,37:237-252.

HUDSON J J,TAYLOR W D,SCHINDLER D W.Planktonic nutrient regeneration and cycling efficiency in temperate lakes[J].Nature,1999,400(12):659-661.

王肇鼎,彭云辉.珠江口水域的营养元素[A].张经.中国主要河流口的生物地球化学研究"[M].北京:海洋出版社,1996 16-36.

梁松,钱宏林.珠江口及其邻近海域赤潮的研究[A].梁松.南海资源与环境研究文集[C].广州:中山大学出版社,1999.189-195.

GB12764.4-91,海洋调查规范[S].

STEPANAUSKAS R,LEONARDSON L.Bioavailability of wetland-derived DON to freshwateer and marine bacterioplankton[J].Limnol Oceanogr,1999,44(6):1 477-1 485.

潘建明,周怀阳,扈传昱,等.夏季珠江口沉积物中营养盐剖面分布和界面交换通量[J].海洋学报,2002,24(3):52-59.

PHILIP N F.Kinetic control of dissolved phosphate in natural rivers and estuaries:a primer on the phosphate buffer mechanism[J].Limnal Oceanogr,1988,33(4,Part 2):649-668.

LEWIS E F,SHAWN L.Factors controlling the concentration of soluble phosphorus in the Mississippi Estuary[J].Limno Oceangor,1985,30(4):826-832.

MICHAEL D K,ROBERT A B.Adsorption of phosphate in anoxic marine sediments[J].Limnol Oceanogr,1980,25(5):797-806.

REDFIELD A C,KETCHUP B H,RICHARDS F A.The influence of organisms on the composition of seawater[A].HILL M N,GOLDBERG E D,ISELIN C O D et al.The see:Vol.2[M].London:Interscience Publishers,1963.26-77.

TEYRRELL T.The relative influences of nitrogen and phosphorus on oceanic primary production[J].Nature,1999,5(400):525-531.

VALDERRAMA J C.The simultaneous analysis of total nitrogen and total phosphorus in natural waters[J].Marine Chemistry,1981,10:109-122.

WATT W D,HARYES E R.Tracer study of the phosphorus cycle in seawater[J].Limnal Oceanogr,1963,8(2):267-285.

施引文献

资源附件(0)

访问统计