湿地
土壤水分
环境科学
生物地球化学循环
营养物
富营养化
溶解有机碳
沼泽
盐度
环境化学
有机质
水文学(农业)
化学
生态学
海洋学
地质学
土壤科学
生物
岩土工程
作者
Havalend E. Steinmuller,Lisa G. Chambers
标识
DOI:10.2136/sssaj2017.05.0162
摘要
Core Ideas Ammonium that accumulated in the porewater following an influx of seawater took ∼1 wk to flux into the surrounding water. Soluble reactive P concentrations in both the porewater and surrounding water increased with salinity. Nutrient export was influenced by wetland soil type. Saltwater intrusion could catalyze the rapid export of nutrients from freshwater wetland soils into the coastal zone, especially in organic matter‐rich soils. Coastal wetlands are vulnerable to saltwater intrusion, which may alter soil biogeochemical processes, lead to the export of nutrients into the coastal zone, and contribute to eutrophication. Using intact soil cores from three different freshwater wetlands and subjecting them to control (0), 5, or 15 parts per thousand (ppt) seawater treatments, we investigated how different wetland soils (bayhead swamp, cypress dome, and mineral marsh) and salinities alter the export of soil nutrients [soluble reactive P (SRP), NH 4 + , and dissolved organic C (DOC)], as well as microbial biomass C and greenhouse gas emissions. The highest salinity treatment increased CO 2 production by 30% with no change in methane production. Porewater NH 4 + concentrations averaged 8× higher than the control in the 15‐ppt treatment and 5× greater than the control in the 5‐ppt treatment, with a ∼1‐wk lag period between porewater accumulation of NH 4 + and export into the surrounding water. The magnitude of NH 4 + export was mediated by wetland soil type. Soluble reactive P concentrations averaged 8× and 3.5× higher in the cypress dome and bayhead swamp 15‐ppt treatments respectively than in their controls, though no effect was observed within the mineral marsh. Dissolved organic C concentrations differed by wetland soil type but were unaffected by salinity treatment. This study demonstrates that saltwater intrusion could catalyze the rapid export of nutrients from freshwater wetland soils into the coastal zone, though nutrient export varies by wetland soil type.
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