Phosphorus runoff risk assessment in karstic regions of the United States
Abstract The Phosphorus (P) Index risk assessment tool has been widely adopted across the United States to identify and rank site vulnerability to P runoff as part of the Natural Resources Conservation Service nutrient management planning (NMP) process. However, limited success has been achieved in...
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Series: | Agricultural & Environmental Letters |
Online Access: | https://doi.org/10.1002/ael2.20001 |
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doaj-a4b5f64d05bd490786d219f43729da9e2021-02-05T06:02:44ZengWileyAgricultural & Environmental Letters2471-96252020-01-0151n/an/a10.1002/ael2.20001Phosphorus runoff risk assessment in karstic regions of the United StatesAndrew N. Sharpley0Phillip D. Hays1Karl W. VanDevender2Mike B. Daniels3Dep. of Crop, Soil, and Environmental Sciences Univ. of Arkansas 115 Plant Sciences Building Fayetteville AR 72701 USAU.S. Geological Survey, Lower Mississippi‐Gulf Water Science Center and Dep. of Geosciences Univ. of Arkansas 216 Ozark Hall Fayetteville AR 72701 USADep. of Biological and Agricultural Engineering Cooperative Extension Univ. of Arkansas 2301 South University Ave. Little Rock AR 72204 USADep. of Crop, Soil, and Environmental Sciences, Cooperative Extension Univ. of Arkansas 2301 South University Ave. Little Rock AR 72204 USAAbstract The Phosphorus (P) Index risk assessment tool has been widely adopted across the United States to identify and rank site vulnerability to P runoff as part of the Natural Resources Conservation Service nutrient management planning (NMP) process. However, limited success has been achieved in addressing the risk of P loss by subsurface flow pathways, despite its relative importance in certain areas of the United States, particularly in those U.S. states dominated by karst terrain. Here we review how states with varying land areas classified as having karst features address the risk of P runoff during the NMP process. Indices adopted in Illinois and Indiana require setbacks (widths 15–72 m) around surface karst features. The remaining states with karst address the risk of P loss in NMP development rather than the application of a P Index. Given the spatially variable hydrogeologic properties of karst, technically rigorous field‐scale factors are unlikely to be developed in the near future.https://doi.org/10.1002/ael2.20001 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Andrew N. Sharpley Phillip D. Hays Karl W. VanDevender Mike B. Daniels |
spellingShingle |
Andrew N. Sharpley Phillip D. Hays Karl W. VanDevender Mike B. Daniels Phosphorus runoff risk assessment in karstic regions of the United States Agricultural & Environmental Letters |
author_facet |
Andrew N. Sharpley Phillip D. Hays Karl W. VanDevender Mike B. Daniels |
author_sort |
Andrew N. Sharpley |
title |
Phosphorus runoff risk assessment in karstic regions of the United States |
title_short |
Phosphorus runoff risk assessment in karstic regions of the United States |
title_full |
Phosphorus runoff risk assessment in karstic regions of the United States |
title_fullStr |
Phosphorus runoff risk assessment in karstic regions of the United States |
title_full_unstemmed |
Phosphorus runoff risk assessment in karstic regions of the United States |
title_sort |
phosphorus runoff risk assessment in karstic regions of the united states |
publisher |
Wiley |
series |
Agricultural & Environmental Letters |
issn |
2471-9625 |
publishDate |
2020-01-01 |
description |
Abstract The Phosphorus (P) Index risk assessment tool has been widely adopted across the United States to identify and rank site vulnerability to P runoff as part of the Natural Resources Conservation Service nutrient management planning (NMP) process. However, limited success has been achieved in addressing the risk of P loss by subsurface flow pathways, despite its relative importance in certain areas of the United States, particularly in those U.S. states dominated by karst terrain. Here we review how states with varying land areas classified as having karst features address the risk of P runoff during the NMP process. Indices adopted in Illinois and Indiana require setbacks (widths 15–72 m) around surface karst features. The remaining states with karst address the risk of P loss in NMP development rather than the application of a P Index. Given the spatially variable hydrogeologic properties of karst, technically rigorous field‐scale factors are unlikely to be developed in the near future. |
url |
https://doi.org/10.1002/ael2.20001 |
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