Abstract:Controlling dissolved phosphorus (P) losses to surface waters is challenging as most conservation practices are only effective at preventing particulate P losses. As a result, P removal structures were developed to filter dissolved P from drainage water before reaching a water body. While many P removal structures with different P sorption materials (PSMs) have been constructed over the past two decades, there remains a need to evaluate their performances and compare on a normalized basis. The purpose of this … Show more
“…Much research is concerned with the effects of P removal by plants in wetlands [1,5,6], especially with the control of non-point source pollution [7]. However, plants can only absorb P in dissolved forms such as the free orthophosphate ions, H 2 PO 4 − and HPO 4 2− [8], while the available P in natural soil can be easily converted into insoluble complexes such as iron and aluminum hydrous oxides, crystalline and amorphous aluminum silicate, and calcium carbonate [9]. P can be dissolved by several mechanisms including Fe reduction [10], Ca removal and ligand exchange.…”
Inorganic phosphorus (P)-solubilizing bacteria (IPSB) and organic P-mineralizing bacteria (OPMB) were isolated from bacteria that were first extracted from the rhizosphere soil of a natural wetland and then grown on either tricalcium phosphate or lecithin medium. The solubilizing of inorganic P was the major contribution to P availability, since the isolated bacteria released much more available P from inorganic tricalcium phosphate than lecithin. IPSB No. 5 had the highest P release rate, that is, 0.53 mg·L −1 ·h −1 in 96 h, and R10 s release rate was 0.52 mg·L −1 ·h −1 in 10 days. The bacteria were identified as Pseudomonas sp. and Pseudomonas knackmussii, respectively. R10 released as much as 125.88 mg·L −1 dissolved P from tricalcium phosphate medium, while R4 released the most dissolved P from organic P medium among the isolates, with a concentration of 1.88 mg·L −1 and a releasing rate of 0.0078 mg·L −1 ·h −1 in ten days. P releasing increased with a pH decrease only when it was from inorganic P, not organic lecithin, and there was no significant correlation between the culture pH and P solubilizing. High-throughput sequencing analysis revealed that the dominant phylum in the studied wetland rhizosphere consisted of Acidobacteria, Proteobacteria, Bacteroidetes and Chloroflexi, accounting for 34.9%, 34.2%, 8.8% and 4.8%, respectively.
“…Much research is concerned with the effects of P removal by plants in wetlands [1,5,6], especially with the control of non-point source pollution [7]. However, plants can only absorb P in dissolved forms such as the free orthophosphate ions, H 2 PO 4 − and HPO 4 2− [8], while the available P in natural soil can be easily converted into insoluble complexes such as iron and aluminum hydrous oxides, crystalline and amorphous aluminum silicate, and calcium carbonate [9]. P can be dissolved by several mechanisms including Fe reduction [10], Ca removal and ligand exchange.…”
Inorganic phosphorus (P)-solubilizing bacteria (IPSB) and organic P-mineralizing bacteria (OPMB) were isolated from bacteria that were first extracted from the rhizosphere soil of a natural wetland and then grown on either tricalcium phosphate or lecithin medium. The solubilizing of inorganic P was the major contribution to P availability, since the isolated bacteria released much more available P from inorganic tricalcium phosphate than lecithin. IPSB No. 5 had the highest P release rate, that is, 0.53 mg·L −1 ·h −1 in 96 h, and R10 s release rate was 0.52 mg·L −1 ·h −1 in 10 days. The bacteria were identified as Pseudomonas sp. and Pseudomonas knackmussii, respectively. R10 released as much as 125.88 mg·L −1 dissolved P from tricalcium phosphate medium, while R4 released the most dissolved P from organic P medium among the isolates, with a concentration of 1.88 mg·L −1 and a releasing rate of 0.0078 mg·L −1 ·h −1 in ten days. P releasing increased with a pH decrease only when it was from inorganic P, not organic lecithin, and there was no significant correlation between the culture pH and P solubilizing. High-throughput sequencing analysis revealed that the dominant phylum in the studied wetland rhizosphere consisted of Acidobacteria, Proteobacteria, Bacteroidetes and Chloroflexi, accounting for 34.9%, 34.2%, 8.8% and 4.8%, respectively.
“…Monitoring and mitigation of stormwater from such developments should be treated as a priority water quality concern as well as a priority research topic. Practices such as the use of P sorbing materials in runoff detention/retention basins or P‐rich soils around poultry houses all show potential (Buda et al, 2012 Bryant et al, 2012; Penn et al, 2017). …”
Hennig Brandt's discovery of phosphorus (P) occurred during the early European colonization of the Chesapeake Bay region. Today, P, an essential nutrient on land and water alike, is one of the principal threats to the health of the bay. Despite widespread implementation of best management practices across the Chesapeake Bay watershed following the implementation in 2010 of a total maximum daily load (TMDL) to improve the health of the bay, P load reductions across the bay's 166,000‐km2 watershed have been uneven, and dissolved P loads have increased in a number of the bay's tributaries. As the midpoint of the 15‐yr TMDL process has now passed, some of the more stubborn sources of P must now be tackled. For nonpoint agricultural sources, strategies that not only address particulate P but also mitigate dissolved P losses are essential. Lingering concerns include legacy P stored in soils and reservoir sediments, mitigation of P in artificial drainage and stormwater from hotspots and converted farmland, manure management and animal heavy use areas, and critical source areas of P in agricultural landscapes. While opportunities exist to curtail transport of all forms of P, greater attention is required toward adapting P management to new hydrologic regimes and transport pathways imposed by climate change.
Core Ideas
At the midpoint of the Chesapeake TMDL, dissolved P is increasing in some tributaries.
Lingering concerns include legacy P, artificial drainage, animal heavy use areas.
Extreme events represent an acute risk to water quality.
“…Water‐control structures can reduce SRP loss from fields by affecting hydrology (Evans et al, 1991; Penn et al, 2017; Zhang et al, 2017). Evans et al (1991) found a net reduction in edge‐of‐field total P losses of 35% under controlled drainage.…”
Section: Implementing Conservation Practices That Reduce Agriculturalmentioning
confidence: 99%
“…Phosphorus sorbing materials offer the potential to trap edge‐of‐field P losses when used in off‐site stormwater treatment structures. Off‐site structures that contained PSMs were found by multiple researchers (Penn et al, 2017; Qin and Shober, 2018) to be effective at removing soluble P (and to some extent particulate P) from runoff. Additionally, several researchers have demonstrated that PSMs in drain tiles may be useful in reducing leached P (King et al, 2016; McDowell et al, 2008).…”
Section: Implementing Conservation Practices That Reduce Agriculturalmentioning
confidence: 99%
“…Many factors affect P reduction by off‐site structures, including structure material, resident time, and influent concentration. In their review, Penn et al (2017) determined that Fe‐containing PSMs performed better (∼35%) at reducing P concentrations in agricultural runoff than did nonslag and slag materials containing Al (∼25%). However, to be cost‐efficient, these structures must carefully balance the P adsorptive capacity of the material, as well as the flow dynamics of the system (i.e., containment structure or buffered filter).…”
Section: Implementing Conservation Practices That Reduce Agriculturalmentioning
Phosphorus (P) is essential for optimum agricultural production, but it also causes water quality degradation when lost through erosion (sediment‐attached P), runoff (soluble reactive P; SRP), or leaching (sediment‐attached P or SRP). Implementation of conservation practices (CP) affects P at the source (avoiding), during transport (controlling), or at the water resource edge (trapping). Trade‐offs often occur with CP implementation. For instance, multiple researchers have shown that conservation tillage reduces total P by over 50%, while increasing SRP by upward of 40%. Conservation tillage may increase water quality degradation as SRP is more bioavailable than is particulate P. Conservation practices must be implemented as a system of practices to increase redundancy and to address all loss pathways, such as P management with conservation tillage and a riparian buffer. Further, planning and adoption must be at a watershed scale to ensure practices are placed in critical source areas, thereby providing the most treatment for the least price. Farmers must be involved in watershed planning, which should include financial backstopping and educational outreach. It is imperative that CPs be used more effectively to reduce and retard off‐site P losses. New and innovative CPs are needed to improve control of P leaching, address legacy stores of soil test P, and mitigate increased P losses expected with climate change. Without immediate changes to CP implementation, P losses will increase due to climate change, with a concomitant degradation of water quality. These changes must be made at a watershed scale and in an intentional and transparent manner.
Core Ideas
Phosphorus‐reducing conservation practices must control all P pathways.
Phosphorus‐reducing conservation practices must be utilized as systems.
New and innovative conservation practices are needed to improve control of P.
Farmer decision‐making must be considered when implementing conservation practices.
Watershed planning and conservation practice implementation must be intentional.
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