The coupled release of REE and Pb to the soil labile pool with time by weathering of accessory phases, Wind River Mountains, WY

Yehudit Harlavan*, Yigal Erel, Joel D. Blum

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

49 Scopus citations

Abstract

Rare earth element (REE) distributions and Pb isotope compositions were explored in soils varying in age from ca. 0.4 to ≥300 ka, developed on moraines in the Wind River Mountains, Wyoming. Soil extracts (0.6 M HCl) were used to examine the soil labile pool while the major element distribution in soil profiles was used to determine the extent of weathering at different soil depths. The results show that the chondrite-normalized REE patterns of the deepest bulk soil within each profile reflects the composition of the moraine till, except for the oldest soil. Up to ca. 12 ka, the soil extract fraction is enriched in light REE, indicating early release of light REE to the soil labile pool while that of the two oldest soils are relatively enriched in heavy REE. In the soil extracts the La/Sm ratio normalized to the deepest soil (LaD/SmD) decreases systematically with soil age. Similarly, the Eu-anomaly in the deepest soil from each profile (EuD/EuD*) decreases slightly with soil age in the three young soils; however, EuD/EuD* increases with soil age in the older soils. The systematic trends of these two ratios indicate the depletion of light REE in young soils and the enrichment of Eu and heavy REE in the older soils. Based on the Pb isotope ratios, the relative contribution of Pb to the soil labile pool via mineral weathering of U- or Th-rich phases was assessed for the different stages of weathering. The whole-soil profile 208Pb/204Pb ratio was found to decrease with soil age and with LaD/SmD, whereas it increased with the EuD/EuD* ratio. In each horizon, Pb isotope ratios (206Pb/204Pb, 207Pb/204Pb, and 208Pb/204Pb) ratio generally decrease with soil age. In order to overcome possible effects from parent material heterogeneity, the amount of radiogenic Pb as compared to the whole-soil composition was calculated and this was found to decrease systematically with soil age.

Original languageAmerican English
Pages (from-to)320-336
Number of pages17
JournalGeochimica et Cosmochimica Acta
Volume73
Issue number2
DOIs
StatePublished - 15 Jan 2009

Bibliographical note

Funding Information:
The authors thank J.J. Braun, J. Schott, D. Vance and an anonymous reviewer for their in-depth comments which greatly improved the manuscript. Funding was provided by the US-Israel BSF Grant 95–30.

Fingerprint

Dive into the research topics of 'The coupled release of REE and Pb to the soil labile pool with time by weathering of accessory phases, Wind River Mountains, WY'. Together they form a unique fingerprint.

Cite this