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1 n and possible transformation to crystalline struvite.
2 d the first shell of As(5+) at the P site in struvite.
3 present in some wastes, may be removed with struvite.
4 ergy CT, 513-747 HU for high-energy CT), and struvite (1337-1530 HU for low-energy CT, 1007-1100 HU f
6 pe), one outlier), cystine (70-71 U(Slope)), struvite (56-60 U(Slope)), calcium oxalate and calcium p
9 ture spectroscopy confirmed that Zn added to struvite-bearing solutions at concentrations</=5 muM sor
13 crystalline composition (uric acid, cystine, struvite, calcium oxalate, calcium phosphate, brushite),
15 his metalloid during the transformation from struvite, can attenuate arsenic contamination from green
16 roscopy (SEM) revealed etch pit formation on struvite crystal surfaces, indicative of a surface inter
17 onance (EPR) spectra of gamma-ray-irradiated struvite disclose five [AsO3](2-) radicals and one [AsO4
18 bsequently inactivated to some degree during struvite drying, and the inactivation typically increase
23 y fluororescence (mu-SXRF) mapping show that struvite formed under ambient conditions contains up to
24 centralized systems, phosphorus recovered as struvite from the solids dewatering liquid resulted in a
25 ssed into market-attractive fertilizers like struvite; however, concerns regarding the microbial safe
26 occur in natural newberyite transformed from struvite in guano deposits and record the accumulation o
28 terial inactivation during the production of struvite, initial heating under moist conditions is reco
29 As(5+) is the predominant oxidation state in struvite, irrespective of Na2HAsO4.7H2O or NaAsO2 as the
30 e (CaOx) and calcium phosphate (CaP); 10% of struvite (magnesium ammonium phosphate produced during i
33 ry through the controlled crystallization of struvite (MgNH4PO4.6H2O), a potential slow-release ferti
34 structure, contributing to distortion of the struvite nu3 PO4(3-) band in the Fourier transform infra
35 e the heterogeneous nucleation and growth of struvite occurs via a particle-mediated process involvin
37 solids were lower when Zn was present during struvite precipitation compared to when Zn was added to
41 allowed for 43% more phosphate recovery via struvite precipitation in the acetic acid addition synth
43 results suggest that brucite dissolution and struvite precipitation were coupled at the mineral-fluid
44 al contaminants such as chromium (Cr) during struvite precipitation, however, requires consideration.
49 source for enrichment of the effluent of the struvite reactor, the phosphate flux was 16 mmol m(-2) h
51 the efficiency of phosphate recovery from a struvite reactor: SED was implemented in such a way that
53 (-1)) are consistent with those reported for struvite recovered from wastewater, suggesting that simi
58 ts, is an important decomposition product of struvite that is an increasingly popular green fertilize
59 Salmonella typhimurium during the drying of struvite under controlled temperature (from 5 to 35 degr
64 urvivor curves were typically nonlinear when struvite was dried at low relative humidity, indicating
65 and chemical composition (brushite, cystine, struvite, weddellite, whewellite, and uric acid) at 24 c
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