Premium
Phosphorus storage, transport and export dynamics in the Foron River watershed
Author(s) -
Dorioz J. M.,
Cassell E. A.,
Orand A.,
Eisenman K. G.
Publication year - 1998
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/(sici)1099-1085(199802)12:2<285::aid-hyp577>3.0.co;2-h
Subject(s) - surface runoff , phosphorus , environmental science , hydrology (agriculture) , watershed , soil water , nonpoint source pollution , eutrophication , nutrient , environmental chemistry , chemistry , soil science , ecology , geology , biology , geotechnical engineering , organic chemistry , machine learning , computer science
Phosphorus (P) export from the Foron River watershed was intensively monitored. Water was analysed for total P, soluble total P, soluble orthophosphate and suspended solids. Watershed soils and river sediments were sampled and the size fraction <0·2 mm analysed for total P, water extractable P, bioavailable P, 1 minute exchangeable P and P fixation capacity. Interstitial waters were analysed for soluble total P. Four hydrological conditions recurred, two during low river flows and two during increased flow. The first occurs in dry weather with a constant or decreasing flow over at least seven days and when there is no surface runoff. Exported phosphorus, predominately soluble and bioavailable, is from point sources. Phosphorus inputs exceed P export so P accumulates in the river. The second condition occurs when a small storm flow increases the average seven‐day flow to exceed the preceding weekly average. Phosphorus export exceeds P inputs and originates from urban runoff, point sources and release of P stored in the river. Exported P is largely particulate but highly bioavailable. The third condition is when substantial runoff follows at least a seven‐day period of constant or decreasing flow. Phosphorus export is from diffuse urban runoff. All the P stored is exported. Exported P is highly bioavailable. High concentrations and fluxes of P export are often seen. The fourth condition happens when the soils are wet and increased flow is from both urban and agricultural runoff. Phosphorus export from diffuse agricultural runoff predominates and is largely not bioavailable. Phosphorus concentrations are low but export fluxes are high when flows are high. These hydrological conditions, when integrated with concepts of mass balance define a phosphorus export typology comprising four regimes. These regimes explain total phosphorus (TP) storage, transport and export patterns, changes in P speciation and allow identification of probable sources of TP in the Foron river watershed. © 1998 John Wiley & Sons, Ltd.