Modeling diffuse phosphorus loads from land to freshwater using the sedimentary record

Research output: Contribution to journalArticle

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Abstract

Diffuse: phosphorus (P) loads to a small lake, Friary Lough, in a 1 km(2) agricultural subcatchment were quantified over 90 years using a palaeolimnological model. The model assumes that lake total phosphorus (TP) is lost to the sediments and to the lake outflow du(r)ing periods of steady-state or is also stored within the water column during periods of non-steady-state behavior. Reconstructed TP loads during the 1991-1995 time interval of 2.05-2.53 g m(-2) yr(-1) are verified by hydrochemical monitoring results from the lake inflow during 1997-1998. This provides evidence for the accuracy of the palaeolomnological model and also that TP loads to the lake dan be accounted for from external catchment runoff. An analysis of the TP load data in terms of-catchment exports shows that there was a linear rate of increase from ca. 1946 to 1995 of 1.20- 1.56 kg km(-2) yr(-1). The rate of increase is similar to river P load data in the larger 1480 km(2) catchment tal;en over 17 years, The; rate of TP increase to the lake is interpreted with regard to current soil P models that propose increasing and threshold soil P concentrations as the cause for increasing diffuse P loss-in runoff.
LanguageEnglish
Pages815-819
JournalENVIRONMENTAL SCIENCE & TECHNOLOGY
Volume35
Issue number5
Publication statusPublished - Mar 2001

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phosphorus
lake
modeling
catchment
runoff
land
inflow
outflow
soil
water column
monitoring
river
sediment
rate

Cite this

@article{043ad24c361e403881838299c3622b23,
title = "Modeling diffuse phosphorus loads from land to freshwater using the sedimentary record",
abstract = "Diffuse: phosphorus (P) loads to a small lake, Friary Lough, in a 1 km(2) agricultural subcatchment were quantified over 90 years using a palaeolimnological model. The model assumes that lake total phosphorus (TP) is lost to the sediments and to the lake outflow du(r)ing periods of steady-state or is also stored within the water column during periods of non-steady-state behavior. Reconstructed TP loads during the 1991-1995 time interval of 2.05-2.53 g m(-2) yr(-1) are verified by hydrochemical monitoring results from the lake inflow during 1997-1998. This provides evidence for the accuracy of the palaeolomnological model and also that TP loads to the lake dan be accounted for from external catchment runoff. An analysis of the TP load data in terms of-catchment exports shows that there was a linear rate of increase from ca. 1946 to 1995 of 1.20- 1.56 kg km(-2) yr(-1). The rate of increase is similar to river P load data in the larger 1480 km(2) catchment tal;en over 17 years, The; rate of TP increase to the lake is interpreted with regard to current soil P models that propose increasing and threshold soil P concentrations as the cause for increasing diffuse P loss-in runoff.",
author = "Philip Jordan and Brian Rippey and NJ Anderson",
year = "2001",
month = "3",
language = "English",
volume = "35",
pages = "815--819",
journal = "Environmental Science and Technology",
issn = "0013-936X",
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}

Modeling diffuse phosphorus loads from land to freshwater using the sedimentary record. / Jordan, Philip; Rippey, Brian; Anderson, NJ.

In: ENVIRONMENTAL SCIENCE & TECHNOLOGY, Vol. 35, No. 5, 03.2001, p. 815-819.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Modeling diffuse phosphorus loads from land to freshwater using the sedimentary record

AU - Jordan, Philip

AU - Rippey, Brian

AU - Anderson, NJ

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N2 - Diffuse: phosphorus (P) loads to a small lake, Friary Lough, in a 1 km(2) agricultural subcatchment were quantified over 90 years using a palaeolimnological model. The model assumes that lake total phosphorus (TP) is lost to the sediments and to the lake outflow du(r)ing periods of steady-state or is also stored within the water column during periods of non-steady-state behavior. Reconstructed TP loads during the 1991-1995 time interval of 2.05-2.53 g m(-2) yr(-1) are verified by hydrochemical monitoring results from the lake inflow during 1997-1998. This provides evidence for the accuracy of the palaeolomnological model and also that TP loads to the lake dan be accounted for from external catchment runoff. An analysis of the TP load data in terms of-catchment exports shows that there was a linear rate of increase from ca. 1946 to 1995 of 1.20- 1.56 kg km(-2) yr(-1). The rate of increase is similar to river P load data in the larger 1480 km(2) catchment tal;en over 17 years, The; rate of TP increase to the lake is interpreted with regard to current soil P models that propose increasing and threshold soil P concentrations as the cause for increasing diffuse P loss-in runoff.

AB - Diffuse: phosphorus (P) loads to a small lake, Friary Lough, in a 1 km(2) agricultural subcatchment were quantified over 90 years using a palaeolimnological model. The model assumes that lake total phosphorus (TP) is lost to the sediments and to the lake outflow du(r)ing periods of steady-state or is also stored within the water column during periods of non-steady-state behavior. Reconstructed TP loads during the 1991-1995 time interval of 2.05-2.53 g m(-2) yr(-1) are verified by hydrochemical monitoring results from the lake inflow during 1997-1998. This provides evidence for the accuracy of the palaeolomnological model and also that TP loads to the lake dan be accounted for from external catchment runoff. An analysis of the TP load data in terms of-catchment exports shows that there was a linear rate of increase from ca. 1946 to 1995 of 1.20- 1.56 kg km(-2) yr(-1). The rate of increase is similar to river P load data in the larger 1480 km(2) catchment tal;en over 17 years, The; rate of TP increase to the lake is interpreted with regard to current soil P models that propose increasing and threshold soil P concentrations as the cause for increasing diffuse P loss-in runoff.

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