Saltwater intrusion increases phosphorus abundance and alters availability in coastal soils with implications for future sea level rise

Chunhao Gu; Sunendra Joshi; Matthew H H Fischel; Elizabeth J Tomaszewski; Paul Northrup; Donald L Sparks

doi:10.1016/j.scitotenv.2024.172624

Saltwater intrusion increases phosphorus abundance and alters availability in coastal soils with implications for future sea level rise

Sci Total Environ. 2024 Apr 22:931:172624. doi: 10.1016/j.scitotenv.2024.172624. Online ahead of print.

Authors

Chunhao Gu¹, Sunendra Joshi², Matthew H H Fischel³, Elizabeth J Tomaszewski², Paul Northrup⁴, Donald L Sparks²

Affiliations

¹ Delaware Environmental Institute, Department of Plant and Soil Sciences, University of Delaware, Newark, DE 19716, USA. Electronic address: chunhaogu.biogeo@gmail.com.
² Delaware Environmental Institute, Department of Plant and Soil Sciences, University of Delaware, Newark, DE 19716, USA.
³ Sustainable Agricultural Systems Laboratory, USDA-Agricultural Research Service, Beltsville, MD 20705, USA.
⁴ Department of Geosciences, Stony Brook University, Stony Brook, NY 11794, USA.

PMID: 38657812
DOI: 10.1016/j.scitotenv.2024.172624

Abstract

Sea level rise (SLR) promotes saltwater intrusion (SWI) into coastal soils globally at an increasing rate, impacting phosphorus (P) dynamics and adjacent water quality. However, how SWI influences P molecular speciation and availability in coastal soils remains poorly understood. By using a space-for-time substitution strategy, we evaluated the SWI impacts on P transformation along a SWI gradient at the Rehoboth Inland Bay, which consists of five sampling locations along a transect representing different SWI degrees. Soils were analyzed at the macro- and micro-scale using X-ray absorption near edge spectroscopy (XANES) and the modified Hedley fractionation. With increasing distance from the Bay, soil salinity (29.3-0.07 mmhos cm^-1), the proportion of Fe³⁺ to total Fe, and P concentrations decreased. The fractionation showed that recalcitrant P was dominant (86.9-89.5% of total P). With increasing SWI, labile P increased gradually, reached a plateau, and then decreased sharply. Bulk XANES spectroscopy showed that soil P was likely dominated by iron and aluminum-associated P (Fe/Al-P), regardless of the SWI degree. Hence, with increasing SWI, P increasingly accumulated in a recalcitrant pool, mainly as Fe/Al-P. μ-XANES spectroscopy revealed that calcium-associated P (Ca-P) existed in P-rich spots of the greatest SWI soil while Al-P occurred in P-rich spots of the low SWI soil, consistent with the greater HCl-P (presumably Ca-P) in the former soil. Overall, results demonstrate that SWI impacts P availability and environmental risk in coastal soils depending on the degree of SWI. These findings have important implications for understanding soil P cycling and availability in SLR-impacted coastal areas.

Keywords: Climate change; Coastal soils; Flooding; Phosphorus; Redox; Saltwater intrusion; Sea level rise.