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- W2023489117 abstract "Phosphorus (P) retention in wetlands is an important function of watershed nutrient cycling, particularly in drainage basins with significant nonpoint nutrient contributions from agriculture and urban sources. Phosphorus storage involves complex interrelated physical, chemical, and biological processes that ultimately retain P in organic and inorganic forms. Both short-term storage of P mediated by assimilation into vegetation, translocation within above- and below-ground plant tissues, microorganisms, periphyton, and detritus, and long-term storage (retention by inorganic and organic soil particles and net accretion of organic matter) need to be considered. Here, we review and synthesize recent studies on P cycling and storage in soils and sediments throughout the Greater Everglades Ecosystem and the influence of biotic and abiotic regulation of P reactivity and mobility as related to restoration activities in south Florida. Total P storage in the floc/detrital layer and surface soils (0–10 cm) is estimated to be 400,000 metric tons (mt) within the entire Greater Everglades Ecosystem, of which 40% is present in the Lake Okeechobee Basin (LOB), 11% in sediments of Upper Chain of Lakes, Lake Istokpoga, and Lake Okeechobee, 30% in the Everglades Agricultural Area (EAA), and 19% in the Stormwater Treatment Areas (STAs) and the Everglades. Approximately, 35% of the P stored is in chemically nonreactive (not extractable after sequential extraction with acid or alkali) pool and is assumed to be stable. Phosphorus leakage rates from LOB and EAA are approximately 500 and 170 mt P per year, respectively, based on long-term P discharges into adjacent ecosystems. The estimated reactive P in the LOB soils is 65% of the total P, of which only 10 –25% is assumed to leak out of the system. Under this scenario, legacy P in LOB would maintain P loads of 500 mt per year to the lake for the next 20– 50 years. Similarly, surface soils of the EAA are estimated to release approximately 170 mt P per year for the next 50–120 years. The role of the STAs in reducing loads to downstream regions is critical and requires effective management of P forms to ensure the P is stabilized in these systems by the addition of chemical amendments or by dredging of accumulated soils. Also, additional efforts to minimize leakage of the legacy P from the northern regions should also be evaluated to reduce external P loading loads to the STAs." @default.
- W2023489117 created "2016-06-24" @default.
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- W2023489117 date "2011-02-17" @default.
- W2023489117 modified "2023-10-17" @default.
- W2023489117 title "Phosphorous Cycling in the Greater Everglades Ecosystem: Legacy Phosphorous Implications for Management and Restoration" @default.
- W2023489117 cites W104676581 @default.
- W2023489117 cites W148316781 @default.
- W2023489117 cites W159113613 @default.
- W2023489117 cites W1964708268 @default.
- W2023489117 cites W1971211649 @default.
- W2023489117 cites W1971585579 @default.
- W2023489117 cites W1977457680 @default.
- W2023489117 cites W1977673682 @default.
- W2023489117 cites W1977674335 @default.
- W2023489117 cites W1978253934 @default.
- W2023489117 cites W1981238978 @default.
- W2023489117 cites W1984406508 @default.
- W2023489117 cites W1990588502 @default.
- W2023489117 cites W1990849819 @default.
- W2023489117 cites W1992666056 @default.
- W2023489117 cites W1993147494 @default.
- W2023489117 cites W1993705118 @default.
- W2023489117 cites W1995488709 @default.
- W2023489117 cites W1996772091 @default.
- W2023489117 cites W1997477998 @default.
- W2023489117 cites W1998615712 @default.
- W2023489117 cites W2003516363 @default.
- W2023489117 cites W2006732583 @default.
- W2023489117 cites W2007395770 @default.
- W2023489117 cites W2009889239 @default.
- W2023489117 cites W2009959856 @default.
- W2023489117 cites W2012253728 @default.
- W2023489117 cites W2017107152 @default.
- W2023489117 cites W2031146172 @default.
- W2023489117 cites W2031398995 @default.
- W2023489117 cites W2032158344 @default.
- W2023489117 cites W2032352195 @default.
- W2023489117 cites W2034591287 @default.
- W2023489117 cites W2038843115 @default.
- W2023489117 cites W2039007217 @default.
- W2023489117 cites W2039499438 @default.
- W2023489117 cites W2041383474 @default.
- W2023489117 cites W2045136634 @default.
- W2023489117 cites W2050936381 @default.
- W2023489117 cites W2051510604 @default.
- W2023489117 cites W2053464767 @default.
- W2023489117 cites W2053883820 @default.
- W2023489117 cites W2057464240 @default.
- W2023489117 cites W2060871989 @default.
- W2023489117 cites W2075539495 @default.
- W2023489117 cites W2078029680 @default.
- W2023489117 cites W2081652071 @default.
- W2023489117 cites W2092429901 @default.
- W2023489117 cites W2093822659 @default.
- W2023489117 cites W2099691715 @default.
- W2023489117 cites W2108862347 @default.
- W2023489117 cites W2109709661 @default.
- W2023489117 cites W2120818201 @default.
- W2023489117 cites W2124025477 @default.
- W2023489117 cites W2126325760 @default.
- W2023489117 cites W2129932536 @default.
- W2023489117 cites W2140108908 @default.
- W2023489117 cites W2145557466 @default.
- W2023489117 cites W2150225599 @default.
- W2023489117 cites W2153464255 @default.
- W2023489117 cites W2153721246 @default.
- W2023489117 cites W2158525702 @default.
- W2023489117 cites W2180710553 @default.
- W2023489117 cites W2315802781 @default.
- W2023489117 cites W2326796732 @default.
- W2023489117 cites W2330813965 @default.
- W2023489117 cites W2496620919 @default.
- W2023489117 cites W3015847851 @default.
- W2023489117 cites W4231313134 @default.
- W2023489117 cites W4233198016 @default.
- W2023489117 cites W4233804769 @default.
- W2023489117 cites W4237029002 @default.
- W2023489117 cites W4238864620 @default.
- W2023489117 cites W4245760120 @default.
- W2023489117 cites W4247448700 @default.
- W2023489117 cites W4248050389 @default.
- W2023489117 cites W4248797294 @default.
- W2023489117 cites W99323583 @default.
- W2023489117 doi "https://doi.org/10.1080/10643389.2010.530932" @default.
- W2023489117 hasPublicationYear "2011" @default.
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