Geochemical fractionation, potential bioavailability and ecological risk of phosphorus in surface sediments of the Cross River estuary system and adjacent shelf, South East Nigeria (West Africa)

被引:30
|
作者
Dan, Solomon Felix [1 ,3 ]
Liu, Su-Mei [1 ,2 ]
Yang, Bin [3 ]
机构
[1] Ocean Univ China, Inst Adv Ocean Study, Minist Educ, Key Lab Marine Chem Theory & Technol, Qingdao 266100, Shandong, Peoples R China
[2] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Shandong, Peoples R China
[3] Beibu Gulf Univ, Guangxi Key Lab Marine Disaster Beibu Gulf, Qinzhou 535011, Peoples R China
基金
美国国家科学基金会;
关键词
Phosphorus fractionation; Sources; Bioavailability; Ecological risk; Cross River estuary system; Adjacent shelf; ORGANIC-MATTER; MARINE-SEDIMENTS; WATER-QUALITY; SALT-MARSH; CHINA SEA; PARTICULATE PHOSPHORUS; INTERTIDAL SEDIMENTS; CHEMICAL SPECIATION; TEMPORAL VARIATIONS; CHANGJIANG ESTUARY;
D O I
10.1016/j.jmarsys.2019.103244
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Phosphorus (P) as an essential macronutrient, plays a crucial role in the regulation of biological productivity and biogeochemical cycling of other biogenic elements in aquatic environments. Different geochemical fractions of sedimentary P were separated and quantified using the sequential extraction (SEDEX) method to evaluate the abundance, sources, distribution, bioavailability and ecological risk of P in surface sediments of the Cross River estuary system (CRES) and adjacent shelf. Sediment grain size composition and bulk organic carbon were also determined. Total P (TP) ranged from 9.21-18.2 mu mol/g (average, 13.30 +/- 2.08 mu mol/g), and comprised mostly of inorganic P (IP) (IP/TP = similar to 87%). Generally, authigenic P (Ca-P) was the dominant IP fraction (Ca-P/IP = similar to 37 +/- 11.1%), representing an important long-term P reservoir. The range of organic carbon (OC) to organic P (OP) ratio (OC/OP) indicated the predominance of terrestrial OC, and that leachable OP (Le-OP) may be the major OP form in surface sediments of the study area. The partitioning and distribution of different sedimentary P fractions were controlled by the biogeo- and physicochemical conditions favorable for P transformation, sediment grain size composition and sources of sedimentary organic matter. The ratio (Fe/P) of the extractable Fe in citrate-dithionite-bicarbonate solution (Fe-CDB) to ferric oxide-bound P(Fe-P) revealed the presence of reactive Fe- matrices having strong sorption capacity for P. The contents of potential bioavailable P (BAP) (similar to 34-60% of TP) indicated that P amount in the overlying water column may increase substantially if released from surface sediments. The Fe-P was the major component of BAP, and the relationship between BAP and extractable Fe-CDB highlighted the significant impact of Fe(III) (oxyhdr)oxides on P mobility and bioavailability. The estimated P enrichment index (PEI) indicated that surface sediment is less impacted by anthropogenic P and poses less ecological risk with respect to sedimentary TP load in the study area.
引用
收藏
页数:16
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