2015
DOI: 10.1080/01490451.2015.1048395
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Zinc Oxalate Crystal Formation byAspergillus nomius

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Cited by 8 publications
(6 citation statements)
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“…The XRD peaks recorded at 18.8°, 22.5°, 30.1°, 35.0°, and 40.5° 2θ were in agreement with those from previous XRD measurements of Zn-Ox dihdyrate (Fig. 3A) [8,27]. The XRD peaks of the crystals formed from Zn-Ca systems with Zn mole ratios less than 0.25 were attributable to Ca-Ox monohydrate (whewellite) or Ca-Ox dihydrate (weddellite) (Fig.…”
Section: Characterization Of Zn-ox and Ca-ox Precipitatessupporting
confidence: 90%
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“…The XRD peaks recorded at 18.8°, 22.5°, 30.1°, 35.0°, and 40.5° 2θ were in agreement with those from previous XRD measurements of Zn-Ox dihdyrate (Fig. 3A) [8,27]. The XRD peaks of the crystals formed from Zn-Ca systems with Zn mole ratios less than 0.25 were attributable to Ca-Ox monohydrate (whewellite) or Ca-Ox dihydrate (weddellite) (Fig.…”
Section: Characterization Of Zn-ox and Ca-ox Precipitatessupporting
confidence: 90%
“…The Ca-Ox precipitate is relatively insoluble, with the monohydrate (whewellite), dihydrate (weddellite), and trihydrate reported to have solubility product constants of 1.45 x 10 -9 , 3.80 x 10 -9 , and 4.68 x 10 -9 , respectively [5]. Other insoluble oxalates of trace metals including Cd and Zn can also be formed naturally, for example, by soil fungi [6][7][8]. The solubility product constants of these trace metal oxalates can be above or below that of Ca-Ox, with values of 1.42 x 10 -8 for Cd-oxalate (Cd-Ox) trihydrate [9] and 1.38 x 10 -9 [9] for Zn-oxalate (Zn-Ox) dihydrate.…”
Section: Introductionmentioning
confidence: 99%
“…A change in Zn minerals into Zn oxalates had been observed before, albeit the minerals were not nanoparticles [ 32 , 39 , 45 ]. When silicate and sulfide minerals containing Zn were transformed by fungal extracellular metabolites, the resulting crystals of zinc oxalates had various shapes and sizes, with most of the crystals measuring between 50 and 100 µm [ 39 ].…”
Section: Discussionmentioning
confidence: 89%
“…Minerals of zinc oxalate associated with a fungus have a different shape compared to both biomineral and abiotically formed Zn oxalate. However, the biominerals formed farther away from the fungal mycelium had a shape that was more similar to the abiotically formed Zn oxalate [ 32 ]. Since our experiment was only done with extracellular metabolites, the smaller change in the size and shape upon partial transformation may also result from the same processes that led to the increase in similarities between the biomineral formed further away from the mycelium and the abiotically formed mineral.…”
Section: Discussionmentioning
confidence: 99%
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