Particle-size distribution and phosphorus forms as a function of hydrological forcing in the Yellow River
Autor: | Zhigang Yu, Hongtao Chen, Jun-Tao Du, Qingzhen Yao |
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Rok vydání: | 2015 |
Předmět: |
Geologic Sediments
010504 meteorology & atmospheric sciences Health Toxicology and Mutagenesis chemistry.chemical_element 010501 environmental sciences 01 natural sciences Flux (metallurgy) Rivers Water Movements Environmental Chemistry Particle Size 0105 earth and related environmental sciences Chemistry Phosphorus Sediment General Medicine Authigenic Particulates Pollution Environmental chemistry Particle-size distribution Particle Particulate Matter Particle size Hydrology |
Zdroj: | Environmental Science and Pollution Research. 23:3385-3398 |
ISSN: | 1614-7499 0944-1344 |
DOI: | 10.1007/s11356-015-5567-3 |
Popis: | Samples were collected monthly from January to December in 2010, and daily observations were made during the water-sediment regulation event in June-July 2010. Sequential extractions were applied to determine the forms of P in different particle-size fractions and to assess the potential bioavailability of particulate phosphorus (PP). The results indicated that exchangeable phosphorus, organic phosphorus, authigenic phosphorus, and refractory phosphorus increased with the decreasing of particulate size; conversely, detrital phosphorus decreased with the decreasing of particulate size. The content of bioavailable particulate phosphorus (BAPP) varied greatly in different sizes of particles. In general, the smaller the particle size, the higher the content of bioavailable phosphorus and its proportion in total phosphorous was found in these particles. Hydrological forcing controlled the variability in the major P phases found in the suspended sediments via changes in the sources and the particle grain-size distribution. The variation of particle sizes can be attributed also to different total suspended sediment (TSS) sources. Water-sediment regulation (WSR) mobilized only particulate matter from the riverbed, while during the rainstorm soil erosion and runoff were the main source. The BAPP fluxes associated with the "truly suspended" fraction was approximately 200 times larger than the dissolved inorganic phosphorus (DIP) flux. Thus, the transfer of fine particles to the open sea is most probably accompanied by BAPP release to the DIP and can support greater primary and secondary production. |
Databáze: | OpenAIRE |
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