黄海麻坑群沉积物磷的保存与转化及环境效应

李梦露, 冉祥滨, 刘军, 吴文涛, 王昊, 刘晓瑜, 臧家业

中国环境科学 ›› 2020, Vol. 40 ›› Issue (4) : 1757-1770.

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中国环境科学 ›› 2020, Vol. 40 ›› Issue (4) : 1757-1770.
环境生态

黄海麻坑群沉积物磷的保存与转化及环境效应

  • 李梦露1, 冉祥滨1,2, 刘军1, 吴文涛1, 王昊1, 刘晓瑜3, 臧家业1
作者信息 +

The preservation and transformation of phosphorus in the pockmark sediments of the Yellow Sea and its environmental effect

  • LI Meng-lu1, RAN Xiang-bin1,2, LIU Jun1, WU Wen-tao1, WANG Hao1, LIU Xiao-yu3, ZANG Jia-ye1
Author information +
文章历史 +

摘要

基于对北黄海典型麻坑群海域某单位麻坑内部和外缘沉积物中不同赋存形态的磷、甲烷(CH4)和硫化物等参数的分析,探讨了麻坑独特的环境中磷的转化与埋藏机制、沉积物-水体系磷的释放及对区域磷循环的影响.研究表明,沉积物中碎屑态磷(Det-P)是磷主要的赋存形态(>50%),其次是有机磷(Org-P)、铁结合态磷(Fe-P)和自生态磷(Auth-P),交换态磷(Exch-P)对总磷的贡献较小;麻坑内部与麻坑外缘处沉积物中溶解态活性磷(DRP)向水体的释放通量分别为2.84μmol/(cm2·a)和1.03μmol/(cm2·a),对上层水体的贡献依次为19.6%和3.03%,是上层水体磷的重要来源.麻坑内外磷的埋藏速率与转化过程存在不同;研究区地下水的渗漏是磷的沉积速率和释放通量都普遍高的原因.北黄海麻坑区沉积物中磷的保存与转化还与浅层CH4的逸出相关,潜在提高黄铁矿的生成速率.较高的沉积物-水界面磷通量必然对区域富营养化等生态环境问题产生深远影响,值得关注.

Abstract

In this paper, determinations of phosphorus forms, methane and sulfate and so on were implemented in the typical pockmark area of north Yellow Sea to explore the controlling mechanism of phosphorus transformation and burial under this unique environment and its effect of phosphorus release from sediment-water system on regional phosphorus cycle. The results showed that Det-P(>50%) was the dominant P form in the sediments, followed by Org-P, Fe-P and Auth-P. Exch-P was the minor phase of Tot-P. The diffusive fluxes of dissolved reactive phosphorus (DRP) at B9 and B11 stations were 2.84μmol/(cm2·a) and 1.03μmol/(cm2·a), and their contributions to surface water P loadings were 19.6% and 3.03%, respectively. Observed burial and transformation of phosphorus in and out the pockmark were different; the leakage of groundwater in the study area was the reason for both the high deposition rate and release flux of phosphorus. The preservation of phosphorus in the sediments of the pockmark area in the north Yellow Sea was also related to the escape of shallow methane, which could possibly enhance the formation of pyrite in cores. The higher DRP flux in the sediment-water interface would yield some ecological environment problems like regional eutrophication, which would have far-reaching ecological influence and should be thus worthy of more attention.

关键词

北黄海 / 地下水 / 甲烷 / 磷形态 / 麻坑

Key words

groundwater / methane / North Yellow Sea / phosphorus species / pockmark

引用本文

导出引用
李梦露, 冉祥滨, 刘军, 吴文涛, 王昊, 刘晓瑜, 臧家业. 黄海麻坑群沉积物磷的保存与转化及环境效应[J]. 中国环境科学. 2020, 40(4): 1757-1770
LI Meng-lu, RAN Xiang-bin, LIU Jun, WU Wen-tao, WANG Hao, LIU Xiao-yu, ZANG Jia-ye. The preservation and transformation of phosphorus in the pockmark sediments of the Yellow Sea and its environmental effect[J]. China Environmental Science. 2020, 40(4): 1757-1770
中图分类号: X55   

参考文献

[1] Elser J J, Bracken M E S, Cleland E E, et al. Global analysis of nitrogen and phosphorus limitation of primary producers in freshwater, marine and terrestrial ecosystems[J]. Ecology letters, 2007,10(12):1135-1142.
[2] Mather R L, Reynolds S E, Wolff G A, et al. Phosphorus cycling in the North and South Atlantic Ocean subtropical gyres[J]. Nature Geoscience, 2008,1(7):439.
[3] Judd A G, Hovland M. The evidence of shallow gas in marine sediments[J]. Continental Shelf Research, 1992,12(10):1081-1095.
[4] Lashof D A, Ahuja D R. Relative contributions of greenhouse gas emissions to global warming[J]. Nature, 1990,344(6266):529.
[5] Levy E M, Lee K. Potential contribution of natural hydrocarbon seepage to benthic productivity and the fisheries of Atlantic Canada[J]. Canadian Journal of Fisheries and Aquatic Sciences, 1988,45(2):349-352.
[6] Ruttenberg K C. Phosphorus cycle. In:Encyclopedia of Ocean Sciences(3rd Edition, Cochran J K, Bokuniewicz H J, Yager P L. (eds))[M]. Oxford:Academic Press, 2019:447-460.
[7] Zabel M, Dahmke A, Schulz H D. Regional distribution of diffusive phosphate and silicate fluxes through the sediment-water interface:the eastern South Atlantic[J]. Deep Sea Research Part I Oceanographic Research Papers, 1998,45(2):277-300.
[8] Linsy P, Nagender Nath B, Mascarenhas-Pereira M B L, et al. Distribution and diagenesis of phosphorus in the deep-sea sediments of the Central Indian Basin[J]. Journal of Geophysical Research:Oceans, 2018,123(11):7963-7982.
[9] 刘军,臧家业,冉祥滨,等.长江口低氧区沉积物中磷的形态及其环境意义[J]. 环境科学, 2017,38(8):3243-3253. Liu J, Zang J Y, Ran X B, et al. Sedimentary phosphorus speciation in the coastal hypoxic area of Changjiang Estuary and its environmental significance[J]. Environmental Science, 2017,38(8):3243-3253.
[10] Egger M, Rasigraf O, Sapart C J, et al. Iron-mediated anaerobic oxidation of methane in brackish coastal sediments[J]. Environmental Science & Technology, 2014,49(1):277-283.
[11] Dijkstra N, Kraal P, Kuypers M M M, et al. Are iron-phosphate minerals a sink for phosphorus in anoxic Black Sea sediments?[J]. PloS one, 2014,9(7):e101139.
[12] Judd A, Hovland M. Seabed fluid flow:the impact on geology, biology and the marine environment[M]. Cambridge:Cambridge University Press, 2009.
[13] Ondréas H, Olu K, Fouquet Y, et al. ROV study of a giant pockmark on the Gabon continental margin[J]. Geo-Marine Letters, 2005,25(5):281-292.
[14] Paull C K, Ussler Iii W, Borowski W S. Freshwater ice rafting:an additional mechanism for the formation of some high-latitude submarine pockmarks[J]. Geo-Marine Letters, 1999,19(1/2):164-168.
[15] Hovland M, Talbot M R, Qvale H, et al. Methane-related carbonate cements in pockmarks of the North Sea[J]. Journal of Sedimentary Research, 1987,57(5):881-892.
[16] 刘晓瑜,冯秀丽,陈义兰,等.北黄海海底麻坑群形态的定量研究及控制因素[J]. 海洋学报, 2018,40(3):36-49. Liu X Y, Feng X L, Chen Y L, et al. Quantitative study of morphological features and control factors of seabed pockmarks in the North Yellow Sea[J]. Haiyang Xuebao, 2018,40(3):36-49
[17] Cathles L M, Su Z, Chen D. The physics of gas chimney and pockmark formation, with implications for assessment of seafloor hazards and gas sequestration[J]. Marine and Petroleum Geology, 2010,27(1):82-91.
[18] Hovland M, Judd A G. Seabed pockmarks and seepages:Impact on geology, biology and the marine environment[M]. London:Graham and Trotman, 1988,293.
[19] Kelley J T, Dickson S M, Belknap D F, et al. Giant sea-bed pockmarks:evidence for gas escape from Belfast Bay, Maine[J]. Geology, 1994, 22(1):59-62.
[20] Koch S, Berndt C, Bialas J, et al. Gas-controlled seafloor doming[J]. Geology, 2015,43(7):571-574.
[21] Thoma M I. Modeling near surface, gas-induced seafloor deformation using thin plate mechanics in the Thunder Horse Oil Field, Gulf of Mexico and Ninilchik Field, Cook Inlet Basin, Alaska[D]. Baton Rouge:Louisiana State University, 2014.
[22] Jané G, Maestro A, Ercilla G, et al. Occurrence of pockmarks on the Ortegal Spur continental margin, Northwestern Iberian Peninsula[J]. Marine and Petroleum Geology, 2010,27(7):1551-1564.
[23] Defforey D, Paytan A. Phosphorus cycling in marine sediments:Advances and challenges[J]. Chemical Geology, 2017,477:1-11.
[24] Qi L, Wang J, Algeo T J, et al. Enhanced framboidal pyrite formation related to anaerobic oxidation of methane in the sulfate-methane transition zone of the northern South China Sea[J]. Marine Geology, 2016,379:100-108.
[25] Egger M, Jilbert T, Behrends T, et al. Vivianite is a major sink for phosphorus in methanogenic coastal surface sediments[J]. Geochimica et Cosmochimica Acta, 2015,169:217-235.
[26] Flury S, Røy H, Dale A W, et al. Controls on subsurface methane fluxes and shallow gas formation in Baltic Sea sediment (Aarhus Bay, Denmark)[J]. Geochimica et Cosmochimica Acta, 2016,188:297-309.
[27] Sun Y, Torgersen T. Rapid and precise measurement method for adsorbed 224Ra on sediments[J]. Marine Chemistry, 1998,61(3):163-171.
[28] Peterson R N, Burnett W C, Dimova N, et al. Comparison of measurement methods for radium-226 on manganese-fiber[J]. Limnology and Oceanography:Methods, 2009,7(2):196-205.
[29] Waska H, Kim S, Kim G, et al. An efficient and simple method for measuring 226Ra using the scintillation cell in a delayed coincidence counting system (RaDeCC)[J]. Journal of environmental radioactivity, 2008,99(12):1859-1862.
[30] Moore W S, Arnold R. Measurement of 223Ra and 224Ra in coastal waters using a delayed coincidence counter[J]. Journal of Geophysical Research:Oceans, 1996,101(C1):1321-1329.
[31] Garcia-Solsona E, Garcia-Orellana J, Masqué P, et al. Uncertainties associated with 223Ra and 224Ra measurements in water via a Delayed Coincidence Counter (RaDeCC)[J]. Marine Chemistry, 2008,109(3/4):198-219.
[32] 许博超.天然镭同位素富集和测定方法及对河口混合过程的示踪研究[D]. 青岛:中国海洋大学, 2011:36-43. Xu B C. Preconcentration and determination of radium isotppesand their applications as tracers to assess water mixing processes in estuaries[D]. Qingdao:Ocean University of China, 2011:36-43.
[33] 夏冬,米铁柱,甄毓,等.海水对含水层沉积物中镭解吸的模拟实验[J]. 海洋环境科学, 2016,35(1):63-67. Xia D, Mi T Z, Zhen Y, et al. Simulating the process of radium desorption from coastal aquifer sediments by seawater[J]. Marine Environmental Science, 2016,35(1):63-67.
[34] Ruttenberg K C. Development of a sequential extraction method for different forms of phosphorus in marine sediments[J]. Limnology and oceanography, 1992,37(7):1460-1482.
[35] Slomp C P, Epping E H G, Helder W, et al. A key role for iron-bound phosphorus in authigenic apatite formation in North Atlantic continental platform sediments[J]. Journal of marine Research, 1996, 54(6):1179-1205.
[36] 黄德佩.海洋沉积物中硫化物的测定[J]. 环境污染与防治, 1984, 24(3):41-42. Huang D P. Determination of sulfide in Marine sediments[J]. Environmental pollution and prevention, 1984,24(3):41-42.
[37] Berner R A. Early diagenesis:a theoretical approach[M]. Princeton:Princeton University Press, 1980:241-242.
[38] Boudreau B P. Diagenetic modes and their implementation:modelling transport and reactions in aquatic sediments[M]. Berlin:Springer-Verlag, 1997:91-140.
[39] Ogdahl M E, Steinman A D, Weinert M E. Laboratory determined phosphorus flux from lake sediments as a measure of internal phosphorus loading[J]. Journal of Visualized Experiments, 2014,85:e51617.
[40] Ingall E D, Jahnke Richard A. Evidence for enhanced phosphorus regeneration from marine sediments overlain by oxygen depleted waters[J]. Geochimica et Cosmochimica Acta, 1994,58(11):2571-2575.
[41] Nozaki Y, Tsubota H, Kasemsupaya V, et al. Residence times of surface water and particle-reactive 210Pb and210Po in the East China and Yellow seas[J]. Geochimica et Cosmochimica Acta, 1991,55(5):1265-1272.
[42] Wu M, Liu G. Distribution of 226Ra and the residence time of the shelf water in the Yellow Sea and the East China Sea[J]. Journal of Radioanalytical & Nuclear Chemistry, 2015,303(3):2333-2344.
[43] 张磊.长江口、东海的镭同位素及其在水团混合分析中的应[D]. 上海:华东师范大学, 2007. Zhang L. Radium isotopes in Changjiang estuary/East China Sea and their application in analysis of mixing among multiple water mass[D]. Shanghai:East China Normal University, 2007.
[44] Nozaki Y, Kasemsupaya V, Tsubota H. Mean residence time of the shelf water in the East China and the Yellow Seas determined by 228Ra/226Ra measurements[J]. Geophysical Research Letters, 2013, 16(11):1297-1300.
[45] Kraal P, Burton E D, Rose A L, et al. Sedimentary iron-phosphorus cycling under contrasting redox conditions in a eutrophic estuary[J]. Chemical Geology, 2015,392:19-31.
[46] Dong L, Yang Z, Liu X. Phosphorus fractions, sorption characteristics, and its release in the sediments of Baiyangdian Lake, China[J]. Environmental Monitoring & Assessment, 2011,179(1-4):335-345.
[47] McKee B A, Aller R C, Allison M A, et al. Transport and transformation of dissolved and particulate materials on continental margins influenced by major rivers:benthic boundary layer and seabed processes[J]. Continental Shelf Research, 2004,24(7/8):899-926.
[48] 何桐,谢健,余汉生,等.大亚湾表层沉积物中磷的形态分布特征[J]. 中山大学学报自然科学版, 2010,49(6):126-131. He T, Xie J. Yu H S, et al. Distribution Characteristics of Phosphorus Forms in Surface Sediments in the Daya Bay[J]. Acta Scientiarum Naturalium Universities Sunyatseni, 2010,49(6):126-131.
[49] Raimonet M, Andrieux-Loyer F, Ragueneau O, et al. Strong gradient of benthic biogeochemical processes along a macrotidal temperate estuary:focus on P and Si cycles[J]. Biogeochemistry, 2013,115(1-3):399-417.
[50] Jilbert T, Slomp C P. Iron and manganese shuttles control the formation of authigenic phosphorus minerals in the euxinic basins of the Baltic Sea[J]. Geochimica et Cosmochimica Acta, 2013,107(3):155-169.
[51] Vink S, Chambers R M, Smith S V. Distribution of phosphorus in sediments from Tomales Bay, California[J]. Marine Geology, 1997, 139(139):157-179.
[52] He H, Chen H, Yao Q, et al. Behavior of different phosphorus species in suspended particulate matter in the Changjiang estuary[J]. Chinese Journal of Oceanology and Limnology, 2009,27(4):859-868.
[53] Schenau S J, Lange G J D. Phosphorus regeneration vs. burial in sediments of the Arabian Sea[J]. Marine Chemistry, 2001,75(3):201-217.
[54] Ingall E D, Cappellen P V. Relation between sedimentation rate and burial of organic phosphorus and organic carbon in marine sediments[J]. Geochimica et Cosmochimica Acta, 1990,54(2):373-386.
[55] Charette M A, Gonneea M E, Morris P J, et al. Radium isotopes as tracers of iron sources fueling a Southern Ocean phytoplankton bloom[J]. Deep Sea Research Part II:Topical Studies in Oceanography, 2007,54(18-20):1989-1998.
[56] Swarzenski P W. U/Th series radionuclides as coastal groundwater tracers[J]. Chemical Reviews, 2007,107(2):663-674.
[57] Moore W S. The role of submarine groundwater discharge in coastal biogeochemistry[J]. Journal of Geochemical Exploration, 2006, 88(1-3):389-393.
[58] Wang B, Zhang X, Luan Z, et al. Seabed domes with circular depressions in the North Yellow Sea[J]. Journal of Oceanology and Limnology, 2018,36:2154-2165.
[59] Zhang G, Zhang J, Ren J, et al. Distributions and sea-to-air fluxes of methane and nitrous oxide in the North East China Sea in summer[J]. Marine Chemistry, 2008,110(1/2):42-55.
[60] Zhang G L. Distributions and fluxes of methane in the East China Sea and the Yellow Sea in spring[J]. Journal of Geophysical Research, 2004,109(C7):C07011.
[61] 李佩佩.黄河口及黄、渤海溶存甲烷和氧化亚氮的分布与释放通量[D]. 青岛:中国海洋大学, 2010. Li P P. Methane and nitrous oxide in the Yellow River Estuary, the Yellow Sea and the Bohai Sea[D]. Qingdao:Ocean University of China, 2010.
[62] Yang J, Zhang G L, Zheng L X, et al. Seasonal variation of fluxes and distributions of dissolved methane in the North Yellow Sea[J]. Continental shelf research, 2010,30(2):180-192.
[63] 赵静.长江和海南东部典型水体中溶存甲烷和氧化亚氮的分布与释放[D]. 青岛:中国海洋大学, 2009. Zhao J. Methane and nitrous oxide in the Changjiang and typical waters in eastern part of Hainan[D]. Qingdao:Ocean University of China, 2009.
[64] 李佩佩,张桂玲,赵玉川,等.夏季渤海溶解甲烷的分布与通量研究[J]. 海洋科学进展, 2010,28(4):478-488. Li P P, Zhang G L, Zhao Y C, et al. Study on distributions and flux of methane dissolved in the Bohai Sea in summer[J]. Advances in Marine Science, 2010,28(4):478-488.
[65] 曹兴朋,张桂玲,马啸,等.春季东、黄海溶解甲烷的分布和海气交换通量[J]. 环境科学, 2013,34(7):2565-2573. Cao X P, Zhang G L, Ma X, et al. Distribution and air-sea fluxes of methane in the Yellow Sea and the East China Sea in the spring[J]. Environmental Science, 2013,34(7):2565-2573.
[66] Jørgensen B B, Kasten S. Sulfur cycling and methane oxidation[M]//Marine geochemistry. Springer, Berlin, Heidelberg, 2006:271-309.
[67] Dale A W, Regnier P, Knab N J, et al. Anaerobic oxidation of methane (AOM) in marine sediments from the Skagerrak (Denmark):II. Reaction-transport modeling[J]. Geochimica et Cosmochimica Acta, 2008,72(12):2880-2894.
[68] 尹希杰.珠江口沉积物中硫循环和海洋甲烷分布的生物地球化学研究[D]. 北京:中国科学院大学, 2008. Yin X J. Sulfur cycle and methane biogeochemistry in the sediments of Pearl Estuary[D].Beijing:University of Chinese Academy of Sciences, 2008.
[69] Holmkvist L, Ferdelman T G, Bo B J. A cryptic sulfur cycle driven by iron in the methane zone of marine sediment (Aarhus Bay, Denmark)[J]. Geochimica Et Cosmochimica Acta, 2011,75(12):3581-3599.
[70] Liu J, Izon G, Wang J, et al. Vivianite formation in methane-rich deep-sea sediments from the South China Sea[J]. Biogeosciences, 2018,15(20):6329-6348.
[71] Nembrini G P, Capobianco J A, Viel M, et al. A Mössbauer and chemical study of the formation of vivianite in sediments of Lago Maggiore (Italy)[J]. Geochimica et Cosmochimica Acta, 1983,47(8):1459-1464.
[72] Rooze J, Egger M, Tsandev I, et al. Iron-dependent anaerobic oxidation of methane in coastal surface sediments:Potential controls and impact[J]. Limnology and Oceanography, 2016,61:S267-S282.
[73] Lin Z, Sun X, Peckmann J, et al. How sulfate-driven anaerobic oxidation of methane affects the sulfur isotopic composition of pyrite:A SIMS study from the South China Sea[J]. Chemical Geology, 2016,440:26-41.
[74] 杨茜,孙耀东,黄海生源要素的埋藏通量及其时空分布特征[J]. 海洋环境科学, 2015,34(5):680-685. Yang Q, SUN Y. The spatial and temporal distribution of the biogenic elements sedimentation flux in the East China Sea and the Yellow Sea[J]. Marine Environmental Science, 2015,34(5):680-685.
[75] Liu S M, Qi X H, Li X N, et al. Nutrient dynamics from the Changjiang (Yangtze River) estuary to the East China Sea[J]. Journal of Marine Systems, 2016,154:15-27.
[76] 赵晨英,臧家业,刘军,等.黄渤海氮磷营养盐的分布、收支与生态环境效应[J]. 中国环境科学, 2016,36(7):2115-2127. Zhao C Y, Zang J Y, Liu J, et al. Distribution and budget of nitrogen and phosphorus and their influence on the ecosystem in the Bohai Sea and Yellow Sea[J]. China Environmental Science, 2016,36(7):2115-2127.
[77] Liu X, Feng X, Sun Y, et al. Acoustic and biological characteristics of seafloor depressions in the North Yellow Sea Basin of China:Active fluid seepage in shallow water seafloor[J]. Marine Geology, 2019,414:34-46.
[78] Tan S C, Shi G Y, Shi J H, et al. Correlation of Asian dust with chlorophyll and primary productivity in the coastal seas of China during the period from 1998 to 2008[J]. Journal of Geophysical Research:Biogeosciences, 2011,116:G02029(1-10).
[79] Liu S M, Zhang J, Li D J. Phosphorus cycling in sediments of the Bohai and Yellow Seas[J]. Estuarine Coastal and Shelf Science, 2004,59(2):209-218.
[80] Song G D, Liu S M. Phosphorus speciation and distribution in surface sediments of the Yellow Sea and East China Sea and potential impacts on ecosystem[J]. Acta Oceanologica Sinica, 2015,34(4):84-91.
[81] 沈园,张景平,张霞,等.大亚湾沉积物磷的形态特征及其潜在可释放性[J]. 海洋环境科学, 2017,36(5):641-648. Shen Y, Zhang J P, Zhang X, et al. Form characteristics of phosphorus and its releasing potential in the sediments of Daya Bay[J]. Marine Environmental Science, 2017,36(5):641-648.

基金

中央级公益性科研院所基本科研业务费资助项目(2019JH02);国家自然科学基金资助项目(41806097,41776089和41506069)


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