Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Paul R. Lear"'
Autor:
Paul E. Flathman, Jason R. Trausch, Paul Zottola, Ruji Yao, Paul R. Lear, Gregory J. Laird, Bryon J. Krupp, Douglas E. Jerger, John H. Carson, Patrick M. Woodhull
Publikováno v:
Remediation Journal. 6:57-79
In-situ biological solid-phase (or land) treatment was cost-effectively used to remediate 1,500 cubic yards (1,100 m3) of contaminated soil within three months of field operation following spillage of an estimated 12,000 gallons (45,000 L) of vinyl a
Publikováno v:
Clays and Clay Minerals. 38:203-208
The reduction and reoxidation of three nontronite samples, GAN (API H-33a, Garfield, Washington), SWa-1 (ferruginous Washington smectite), and NG-1 (Hohen Hagen, Federal Republic of Germany) were studied with visible absorption and Mossbauer spectros
Autor:
Joseph W. Stucki, Paul R. Lear
Publikováno v:
ACS Symposium Series ISBN: 9780841217164
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::096ce94b1810c8acf17df7293d06f63b
https://doi.org/10.1021/bk-1990-0415.ch017
https://doi.org/10.1021/bk-1990-0415.ch017
Autor:
Joseph W. Stucki, Paul R. Lear
Publikováno v:
Clays and Clay Minerals. 35:373-378
The effects of chemical reduction of structural Fe 3§ in nontronite SWa-1 (ferruginous smectite) on intervalence electron transfer (IT) and magnetic exchange were investigated. Visible absorption spectra in the region 800-400 nm of a chemical reduct
Autor:
Paul R. Lear, Joseph W. Stucki
Publikováno v:
Clays and Clay Minerals. 37:547-552
The effect of Fe oxidation state on the specific surface area, Sin, ofnontronite was studied using the < 2-tzm, Na§ fraction of the SWa-1 and Garfield nontronite reference clays. The reduction of structural Fe 3+ in the octahedral sheet of the nontr
Autor:
Paul R. Lear
Publikováno v:
Clays and Clay Minerals. 33:539-545
The effects of reduction and reoxidation of octahedral Fe 3+ on the exchange of structural hydrogen in nontronite were determined using tritium (all) as a label element. The uptake of H from the surrounding solution of nontronite suspensions increase
Publikováno v:
Journal of Agronomic Education. 15:104-106
Publikováno v:
Clays and Clay Minerals. 36:376-378
Iron impurities in the Hohen Hagen nontronite (NG-1) were identified as maghemite and goethite. The phase identified as maghemite was magnetically ordered at both room temperature and 87 K, with hyperfine magnetic fields of 48.6 and 50.7 tesla, respe
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