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Title: Surface reactions of synthetic, end-member analogues of monazite, xenotime and rhabdophane, and evolution of natural waters

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
 [1];  [2];  [3]
  1. McMaster Univ., Hamilton, Ontario (Canada)
  2. Univ. of Western Ontario, London (Canada)
  3. Oak Ridge National Laboratory, TN (USA)

Recently, evidence has accumulated that certain carbonate and sulfate minerals undergo selective surface ion-exchange reactions with aqueous solutions at low temperatures. Evidence obtained by powder XRD, SIMS and XPS is presented here indicating that synthetic rare earth element (REE) phosphate mineral analogues undergo similar reactions. Hydrous Ho-xenotime reacts with aqueous Nd{sup 3+} over a period of months to produce Nd-rhabdophane. Sm- and Nd-monazite crystals undergo detectable surface exchange reactions within 5 days at 65{degree}C. Ho- and Er-xenotime react similarly. Exchange of Y and Lu in the surface layers of Lu-xenotime is pH dependent, with lower pH favoring replacement. Clearly, such effects are relevant to the debate about REE concentrations and signatures in natural waters, particularly in view of the widespread occurrence of monazite in nature.

DOE Contract Number:
AC05-84OR21400
OSTI ID:
5254277
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Vol. 52:3; ISSN 0016-7037
Country of Publication:
United States
Language:
English