黄渤海氮磷营养盐的分布、收支与生态环境效应

Abstract
Figure/Table
References (74)
Related Citation (4)

Download: PDF (5927 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract

Based on results obtained from the comprehensive investigation in the Bohai Sea and the Yellow Sea (BYS), distributions and sources of dissolved inorganic nitrogen (DIN) and dissolved inorganic phosphorus (DIP) in the sea water and sediment pore water in the study area were discussed; and a budget model of nitrogen (N) and phosphorus (P) in the BYS was established. Concentrations of DIN and DIP in the study area are affected by riverine input and benthic flux. The major sources of the DIN in the water column of the BYS are benthic diffusion, followed by the atmospheric deposition and inputs from adjacent rivers the groundwater and the East China Sea; while the dominant removals of DIN from water column in the BYS are phytoplankton utilization and sedimentation. The key sources of the DIP are phosphorus minerals desorption and weathering, accounting for 91%, followed by benthic flux and atmospheric deposition, then riverine flux and groundwater input; while the dominant outputs of DIP are sedimentation and the outflow to the East China Sea. There was a 11Gmol/a of nitrogen accumulated in the BYS, which would result in an increasing of DIN concentration by 0.6 μmol/(L·a). DIN concentrations and N/P ratio in the Bohai Sea and the Yellow Sea BYS kept increasing in recent decades due to the increasing of nitrogen N accumulation and phosphorus P sedimentation. Terrestrial nitrogen loadings might enhance the primary production and alter the structure and function of ecosystem, which had would have significant effects on the ecosystem of Bohai Sea and Yellow Sea the BYS in the long-time scale. We, therefore, should reduce the riverine nitrogen N loads to maintain the ecosystem stability in the BYS Bohai Sea and Yellow Sea.

Key words： Bohai Sea and Yellow Sea dissolved inorganic nitrogen dissolved inorganic phosphorus phosphate flux and budget

Received: 07 December 2015

X55

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	ZHAO Chen-ying
	ZANG Jia-ye
	LIU Jun
	SUN Tao
	RAN Xiang-bin

Cite this article:

ZHAO Chen-ying,ZANG Jia-ye,LIU Jun等. Distribution and budget of nitrogen and phosphorus and their influence on the ecosystem in the Bohai Sea and Yellow Sea[J]. CHINA ENVIRONMENTAL SCIENCECE, 2016, 36(7): 2115-2127.

URL:

http://www.zghjkx.com.cn/EN/ OR http://www.zghjkx.com.cn/EN/Y2016/V36/I7/2115

[1]	Tyrrell, T. The relative influences of nitrogen and phosphorus on oceanic primary production [J]. Nature, 1999,400:525-531.
[2]	Tang Q, Jin X, Wang J, et al. Decadal-scale variations of ecosystem productivity and control mechanisms in the Bohai Sea [J]. Fisheries Oceanography, 2003,12(4/5):223-233.
[3]	高嵩,范士亮,韩秀荣,等.浒苔绿潮与南黄海近岸海域水质的关系 [J]. 中国环境科学, 2014,34(1):213-218.
[4]	Diaz R J, Rosenberg R. Spreading dead zones and consequences for marine ecosystems [J]. Science, 2008,321(5891):926-929.
[5]	Wei G F, Tang D L, Wang S. Distribution of chlorophyll and harmful algal blooms (HABs): A review on space based studies in the coastal environments of Chinese marginal seas [J]. Advances in Space Research, 2008,41(1):12-19.
[6]	Wu Z, Yu Z, Song X, et al. The spatial and temporal characteristics of harmful algal blooms in the southwest Bohai Sea [J]. Continental Shelf Research, 2013,59:10-17.
[7]	Rousseaux C S, Gregg W W. Recent decadal trends in global phytoplankton composition [J]. Global Biogeochemical Cycles, 2015,29(10):1674-1688.
[8]	Bauer J E, Cai W J, Raymond P A, et al. The changing carbon cycle of the coastal ocean [J]. Nature, 2013,504:61-70.
[9]	Berner R A. Burial of organic carbon and pyrite sulfur in the modern ocean: its geochemical and environmental significance [J]. American Journal of Science, 1982,282(4):451-473.
[10]	Hedges J I, Keil R G. Sedimentary organic matter preservation: an assessment and speculative synthesis [J]. Marine chemistry, 1995,49(2):81-115.
[11]	Mantoura R F C, Martin J M, Wollast R. Ocean margin processes in global change [M]. John Wiley and Sons Ltd, 1991.
[12]	Muller-Karger F E, Varela R, Thunell R, et al. The importance of continental margins in the global carbon cycle [J]. Geophysical Research Letters, 2005,32(1), L01602.
[13]	Dai Z, Du J, Zhang X, et al. Variation of Riverine Material Loads and Environmental Consequences on the Changjiang (Yangtze) Estuary in Recent Decades (1955-2008) [J]. Environmental Science & Technology, 2010,45(1):223-227.
[14]	Andrews J E, Burgess D, Cave R R, et al. Biogeochemical value of managed realignment, Humber estuary, UK [J]. Science of the Total Environment, 2006,371:19-30.
[15]	Smith S V, Swaney D P, Buddemeier R W, et al. River nutrient loads and catchment size [J]. Biogeochemistry, 2005,75(1):83- 107.
[16]	曾呈奎,鸿儒,春林.中国海洋志 [M]. 郑州:大象出版社, 2003.
[17]	巩瑶.黄河下游利津站营养盐输送规律及影响因素研究 [D]. 青岛:中国海洋大学, 2012,75-80.
[18]	Liu S M. Response of nutrient transports to water-sediment regulation events in the Huanghe basin and its impact on the biogeochemistry of the Bohai [J]. Journal of Marine Systems, 2015,141:59-70.
[19]	Ran X B, Che H, Zang J Y, et al. Variability in the composition and export of silica in the Huanghe River Basin [J]. Science China: Earth Sciences, 2015,58(11):2078-2089.
[20]	Wang H, Yang Z, Saito Y, et al. Stepwise decreases of the Huanghe (Yellow River) sediment load (1950-2005): Impacts of climate change and human activities [J]. Global and Planetary Change, 2007,57(3):331-354.
[21]	王婷.2002~2004年及调水调沙期间黄河下游营养盐的变化特征 [D]. 青岛:中国海洋大学, 2007:14-59.
[22]	Ning X, Lin C, Su J, et al. Long-term environmental changes and the responses of the ecosystems in the Bohai Sea during 1960~ 1996 [J]. Deep Sea Research Part II: Topical Studies in Oceanography, 2010,57(11):1079-1091.
[23]	Liu S M, Li L W, Zhang Z. Inventory of nutrients in the Bohai [J]. Continental Shelf Research, 2011,31(16):1790-1797.
[24]	Wei Q, Yao Q, Wang B, et al. Long-term variation of nutrients in the southern Yellow Sea [J]. Continental Shelf Research, 2015, 111:184-196.
[25]	孙萍,李瑞香,李艳,等.2005年夏末渤海网采浮游植物群落结构 [J]. 海洋科学进展, 2008,26(3):354-363.
[26]	Liu S M, Zhang J, Chen S Z, et al. Inventory of nutrient compounds in the Yellow Sea [J]. Continental Shelf Research, 2003,23(11):1161-1174.
[27]	刘军,臧家业,张丽君,等.黄海硅的分布与收支研究 [J]. 中国环境科学, 2016,36(1):157-166.
[28]	Redfield A C. The biological control of chemical factors in the environment [J]. American scientist, 1958:205-221.
[29]	朱明远,毛兴华,吕瑞华,等.黄海海区的叶绿素a和初级生产力 [J]. 黄渤海海洋, 1993,11(3):38-51.
[30]	檀赛春,石广玉.中国近海初级生产力的遥感研究及其时空演化 [J]. 地理学报, 2007,61(11):1189-1199.
[31]	Liu S M, Zhang J, Chen H T, et al. Nutrients in the Changjiang and its tributaries [J]. Biogeochemistry, 2003,62(1):1-18.
[32]	Zhang J, Yu Z G, Raabe T, et al. Dynamics of inorganic nutrient species in the Bohai seawaters [J]. Journal of Marine Systems, 2004,44(3):189-212.
[33]	Zhang G, Zhang J, Liu S. Characterization of nutrients in the atmospheric wet and dry deposition observed at the two monitoring sites over Yellow Sea and East China Sea [J]. Journal of Atmospheric Chemistry, 2007,57(1):41-57.
[34]	Martin J M, Zhang J, Shi M C, et al. Actual flux of the Huanghe (Yellow River) sediment to the western Pacific Ocean [J]. Netherlands Journal of Sea Research, 1993,31(3):243-254.
[35]	Berner R A. Early diagenesis: A theoretical approach [M]. Princeton University Press, Princeton, 1980:241-242.
[36]	李玲伟.沉积物-水界面交换和黄河输入对渤海营养盐的影响 [D]. 青岛:中国海洋大学, 2010:47-55.
[37]	Li Y H, Gregory S. Diffusion of ions in sea water and in deep-sea sediments [J]. Geochimica et Cosmochimica Acta, 1974,38(5): 703-714.
[38]	Ullman W J, Aller R C. Diffusion coefficients in nearshore marine sediments [J]. Limnology and Oceanography, 1982,27(3):552- 556.
[39]	Kim G, Ryu J W, Yang H S, et al. Submarine groundwater discharge (SGD) into the Yellow Sea revealed by 228Ra and 226Ra isotopes: Implications for global silicate fluxes [J]. Earth and Planetary Science Letters, 2005,237(1):156-166.
[40]	Peterson R N, Burnett W C, Taniguchi M, et al. Radon and radium isotope assessment of submarine groundwater discharge in the Yellow River delta, China [J]. Journal of Geophysical Research, 2008,113,C09021.
[41]	Waska H, Kim G. Submarine groundwater discharge (SGD) as a main nutrient source for benthic and water-column primary production in a large intertidal environment of the Yellow Sea [J]. Journal of Sea Research, 2011,65(1):103-113.
[42]	Seitzinger S, Harrison J A, Böhlke J K, et al. Denitrification across landscapes and waterscapes: a synthesis [J]. Ecological Applications, 2006,16(6):2064-2090.
[43]	张润.中国边缘海生物固氮作用的研究 [D]. 厦门:厦门大学, 2011.
[44]	Slomp C P, Malschaert J F P, Van Raaphorst W. The role of adsorption in sediment‐water exchange of phosphate in North Sea continental margin sediments [J]. Limnology and Oceanography, 1998,43(5):832-846.
[45]	Slomp C P, Van Cappellen P. The global marine phosphorus cycle: sensitivity to oceanic circulation [J]. Biogeosciences, 2007,4: 155-171.
[46]	韦钦胜,傅明珠,李艳,等.南黄海冷水团海域溶解氧和叶绿素最大现象值及营养盐累积的季节演变 [J]. 海洋学报, 2013, 35(4):142-154.
[47]	Liu S M, Hong G H, Zhang J, et al. Nutrient budgets for large Chinese estuaries [J]. Biogeosciences, 2009,6(10):2245-2263.
[48]	Moore W S. The Effect of Submarine Groundwater Discharge on the Ocean [J]. Annual Review of Marine Science, 2010,2:59-88.
[49]	Seitzinger S P, Kroeze C. Global distribution of nitrous oxide production and N inputs in freshwater and coastal marine ecosystems [J]. Global biogeochemical cycles, 1998,12(1):93- 113.
[50]	中华人民共和国水利部.中国河流泥沙公报2007-2013 [DB/OL]. http://www.mwr.gov.cn/.
[51]	水利部海河水利委员会.海河流域水资源公报2005年[EB/OL]. [2014-12-01] http://www.hwcc.gov.cn/pub/hwcc/static/szygb/ gongbao2005/index.htm.
[52]	卞少伟,孙韧,梅鹏蔚,等.2013年春夏季天津近岸海域浮游植物的群落结构 [J]. 水生态学杂志, 2015,36(1):47-52.
[53]	夏斌.2005年夏季环渤海16条主要河流的污染状况及入海通量 [D]. 青岛:中国海洋大学, 2007:13-16.
[54]	刘敬伟,李富祥,刘月,等.鸭绿江下游径流时序变化特征研究 [J]. 人民黄河, 2011,33(10):34-36.
[55]	Kim J K, Jung S, Eom J, et al. Dissolved and particulate organic carbon concentrations in stream water and relationships with land use in multiple-use watersheds of the Han River (Korea) [J]. Water International, 2013,38(3):326-339.
[56]	杨守业,Jung Hoi-soo,李从先,等.黄河,长江与韩国Keum, Yeongsan江沉积物常量元素地球化学特征 [J]. 地球化学, 2004,33(1):99-105.
[57]	米铁柱,姚庆祯,孟佳,等.2011年春、夏季黄海、东海营养盐分布特征的研究 [J]. 海洋与湖沼, 2012,43(3):678-688.
[58]	董太禄.渤海现代沉积作用与模式的研究 [J]. 海洋地质与第四纪地质, 1996,16(4):43-53.
[59]	卢博,李赶先,黄韶健,等.中国黄海,东海和南海北部海底浅层沉积物声学物理性质之比较 [J]. 海洋技术, 2005,24(2):28-33.
[60]	赵志梅.渤海湾沉积物磷形态及营养盐在沉积物-水界面交换的研究 [D]. 杨凌:西北农林科技大学, 2005,27-28.
[61]	李凤业,高抒,贾建军,等,黄、渤海泥质沉积区现代沉积速率 [J]. 海洋与湖沼, 2002,33(4):364-369.
[62]	宋国栋.黄东海沉积物中磷的形态及其影响因素研究 [D]. 青岛:中国海洋大学, 2014,22-25.
[63]	王保栋,单宝田,战闫.黄、渤海无机氮的收支模式初探 [J]. 海洋科学, 2002,(2):33-36.
[64]	田恬,魏皓,苏健,等.黄海氮磷营养盐的循环和收支研究 [J]. 海洋科学进展, 2003,21(1):1-11.
[65]	江辉煌,刘素美.渤海沉积物中磷的分布与埋藏通量 [J]. 环境科学学报, 2013,33(1):125-132.
[66]	Li H M, Zhang C S, Han X R, et al. Changes in concentrations of oxygen, dissolved nitrogen, phosphate, and silicate in the southern Yellow Sea, 1980-2012: Sources and seaward gradients [J]. Estuarine, Coastal and Shelf Science, 2014,163(20):44-55.
[67]	国家海洋局.中国海洋灾害公报1995~2011 [EB/OL]. http://www.soa.gov.cn/zwgk/hygb/zghyzhgb/.
[68]	Li Z Y, Bai J, Shi J H, et al. Distributions of inorganic nutrients in the Bohai Sea of China [J]. Journal of Ocean University of Qingdao, 2003,2(1):112-116.
[69]	孙军,刘东艳,徐俊,等.1999年春季渤海中部及其邻近海域的网采浮游植物群落 [J]. 生态学报, 2004(9):179-192.
[70]	苑明莉,孙军,翟惟东.2012年秋季渤海和北黄海浮游植物群落 [J]. 天津科技大学学报, 2014,29(6):56-64.
[71]	张志锋,贺欣,张哲,等.渤海富营养化现状,机制及其与赤潮的时空耦合性 [J]. 海洋环境科学, 2012,31(4):465-468.
[72]	Wang X, Cui Z, Guo Q, et al. Distribution of nutrients and eutrophication assessment in the Bohai Sea of China [J]. Chinese Journal of Oceanology and Limnology, 2009,27:177-183.
[73]	孙军,刘东艳,柴心玉,等.1998~1999年春秋季渤海中部及其邻近海域叶绿素a浓度及初级生产力估算 [J]. 生态学报, 2003,23(3):517-526.
[74]	Nelson D M, Brzezinski M A. Kinetics of silicate acid uptake by natural diatom assemblages in two Gulf and Stream warm-core rings [J]. Marine Ecology Progress Series, 1990,62:283-292.