Phosphorus retention and remobilization along hydrological pathways in karst terrain.
Environ Sci Technol
; 48(9): 4860-8, 2014 May 06.
Article
em En
| MEDLINE
| ID: mdl-24720609
ABSTRACT
Karst landscapes are often perceived as highly vulnerable to agricultural phosphorus (P) loss, via solution-enlarged conduits that bypass P retention processes. Although attenuation of P concentrations has been widely reported within karst drainage, the extent to which this results from hydrological dilution, rather than P retention, is poorly understood. This is of strategic importance for understanding the resilience of karst landscapes to P inputs, given increasing pressures for intensified agricultural production. Here hydrochemical tracers were used to account for dilution of P, and to quantify net P retention, along transport pathways between agricultural fields and emergent springs, for the karst of the Ozark Plateau, midcontinent USA. Up to â¼ 70% of the annual total P flux and â¼ 90% of the annual soluble reactive P flux was retained, with preferential retention of the most bioavailable (soluble reactive) P fractions. Our results suggest that, in some cases, karst drainage may provide a greater P sink than previously considered. However, the subsequent remobilization and release of the retained P may become a long-term source of slowly released "legacy" P to surface waters.
Texto completo:
1
Coleções:
01-internacional
Base de dados:
MEDLINE
Assunto principal:
Fósforo
/
Poluentes Químicos da Água
Idioma:
En
Revista:
Environ Sci Technol
Ano de publicação:
2014
Tipo de documento:
Article
País de afiliação:
Reino Unido