PHOSPHORUS IN SEDIMENTS OF THE AMAZON RIVER AND ESTUARY - IMPLICATIONS FOR THE GLOBAL FLUX OF PHOSPHORUS TO THE SEA

被引:157
作者
BERNER, RA
RAO, JL
机构
[1] Department of Geology and Geophysics, Yale University, New Haven
关键词
D O I
10.1016/0016-7037(94)90014-0
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The distribution of various forms of P in suspended and depositional bank sediments of the Amazon River and bottom sediments of the mixing and freshwater portions of the Amazon estuary and shelf have been determined using a modified sequential extraction method. Forms of P distinguished are: P associated with ferric oxides/hydroxides (Fe-P), organic P (org-P), P extracted with acetate buffer at pH 4 (acet-P), and detrital apatite (detr-P). Results indicate that there is a distinct drop in Fe-P, org-P, and total P after deposition of suspended sediment on the banks of the river. Similar results are found for sediment deposited on the freshwater portion (river channel bottom) of the continental shelf. Sediment deposited on estuarine portions of the shelf also shows a significant drop in total P, due mostly to a drop in org-P. No appreciable change in acet-P was found between river suspended sediments and those of either the river banks or of the estuarine shelf. An inverse correlation is found for all sediments between concentrations of Fe-P and detr-P because of the association of detrital apatite with the coarser fractions of the sediments and Fe-P with the finer fractions. These results suggest that considerable amounts of P are added to the oceans by the bacterial decomposition of river transported organic matter and by the desorption of P from iron oxides/hydroxides (some desorption from Al silicates may also occur.) The organic P is released to interstitial solution during early diagenesis and this P may be adsorbed by Fe oxides in the sediment. During frequent resuspension events, the Fe oxides are carried to the overlying water where the P is desorbed and thereby released to solution. Based on our Amazon results, the total global P flux to the oceans by rivers may be more than three times that carried only in solution by the rivers. Further work is needed on other river systems to check these preliminary results.
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页码:2333 / 2339
页数:7
相关论文
共 26 条
[1]   DIAGENESIS OF FE AND S IN AMAZON INNER SHELF MUDS - APPARENT DOMINANCE OF FE REDUCTION AND IMPLICATIONS FOR THE GENESIS OF IRONSTONES [J].
ALLER, RC ;
MACKIN, JE ;
COX, RT .
CONTINENTAL SHELF RESEARCH, 1986, 6 (1-2) :263-289
[2]  
[Anonymous], 1987, GLOBAL WATER CYCLE G
[3]   SEMIAUTOMATED METHOD FOR DETERMINATION OF INORGANIC, ORGANIC AND TOTAL PHOSPHATE IN SEDIMENTS [J].
ASPILA, KI ;
AGEMIAN, H ;
CHAU, ASY .
ANALYST, 1976, 101 (1200) :187-197
[4]   ROLE OF CLAY MINERALS IN THE TRANSPORTATION OF IRON [J].
CARROLL, D .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1958, 14 (1-2) :1-&
[5]   PHOSPHORUS IN SUSPENDED SEDIMENTS OF THE AMAZON RIVER [J].
CHASE, EM ;
SAYLES, FL .
ESTUARINE AND COASTAL MARINE SCIENCE, 1980, 11 (04) :383-391
[6]   THE CHEMICAL MASS BALANCE IN THE AMAZON PLUME I - THE NUTRIENTS [J].
EDMOND, JM ;
BOYLE, EA ;
GRANT, B ;
STALLARD, RF .
DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS, 1981, 28 (11) :1339-1374
[7]   THE CHEMICAL CONTROL OF SOLUBLE PHOSPHORUS IN THE AMAZON ESTUARY [J].
FOX, LE ;
SAGER, SL ;
WOFSY, SC .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1986, 50 (05) :783-794
[10]   THE MARINE PHOSPHORUS CYCLE [J].
FROELICH, PN ;
BENDER, ML ;
LUEDTKE, NA ;
HEATH, GR ;
DEVRIES, T .
AMERICAN JOURNAL OF SCIENCE, 1982, 282 (04) :474-511