ThuliumV1, PubMed, Corpus, bibRecord, 000394

Selected trace elements in the Sacramento River, California: occurrence and distribution.

Identifieur interne : 000394 ( PubMed/Corpus ); précédent : 000393; suivant : 000395

Selected trace elements in the Sacramento River, California: occurrence and distribution.

Auteurs : H E Taylor ; R C Antweiler ; D A Roth ; C N Alpers ; P. Dileanis

Source :

Archives of environmental contamination and toxicology [ 1432-0703 ] ; 2012.

RBID : pubmed:22193863

English descriptors

KwdEn :
- California, Colloids, Elements, Metals (analysis), Rivers, Water Pollutants, Chemical (analysis), Water Pollutants, Chemical (chemistry).
MESH :
- chemical , analysis : Metals, Water Pollutants, Chemical.
- chemical , chemistry : Water Pollutants, Chemical.
- chemical : Colloids, Elements.
- geographic : California.
- Rivers.

Abstract

The impact of trace elements from the Iron Mountain Superfund site on the Sacramento River and selected tributaries is examined. The concentration and distribution of many trace elements-including aluminum, arsenic, boron, barium, beryllium, bismuth, cadmium, cerium, cobalt, chromium, cesium, copper, dysprosium, erbium, europium, iron, gadolinium, holmium, potassium, lanthanum, lithium, lutetium, manganese, molybdenum, neodymium, nickel, lead, praseodymium, rubidium, rhenium, antimony, selenium, samarium, strontium, terbium, thallium, thulium, uranium, vanadium, tungsten, yttrium, ytterbium, zinc, and zirconium-were measured using a combination of inductively coupled plasma-mass spectrometry and inductively coupled plasma-atomic emission spectrometry. Samples were collected using ultraclean techniques at selected sites in tributaries and the Sacramento River from below Shasta Dam to Freeport, California, at six separate time periods from mid-1996 to mid-1997. Trace-element concentrations in dissolved (ultrafiltered [0.005-μm pore size]) and colloidal material, isolated at each site from large volume samples, are reported. For example, dissolved Zn ranged from 900 μg/L at Spring Creek (Iron Mountain acid mine drainage into Keswick Reservoir) to 0.65 μg/L at the Freeport site on the Sacramento River. Zn associated with colloidal material ranged from 4.3 μg/L (colloid-equivalent concentration) in Spring Creek to 21.8 μg/L at the Colusa site on the Sacramento River. Virtually all of the trace elements exist in Spring Creek in the dissolved form. On entering Keswick Reservoir, the metals are at least partially converted by precipitation or adsorption to the particulate phase. Despite this observation, few of the elements are removed by settling; instead the majority is transported, associated with colloids, downriver, at least to the Bend Bridge site, which is 67 km from Keswick Dam. Most trace elements are strongly associated with the colloid phase going downriver under both low- and high-flow conditions.

DOI: 10.1007/s00244-011-9738-z
PubMed: 22193863

Links to Exploration step

pubmed:22193863

Le document en format XML

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<author><name sortKey="Taylor, H E" sort="Taylor, H E" uniqKey="Taylor H" first="H E" last="Taylor">H E Taylor</name>
<affiliation><nlm:affiliation>United States Geological Survey, Boulder, CO 80303, USA. hetaylor@usgs.gov</nlm:affiliation>
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<author><name sortKey="Antweiler, R C" sort="Antweiler, R C" uniqKey="Antweiler R" first="R C" last="Antweiler">R C Antweiler</name>
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<author><name sortKey="Roth, D A" sort="Roth, D A" uniqKey="Roth D" first="D A" last="Roth">D A Roth</name>
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<author><name sortKey="Alpers, C N" sort="Alpers, C N" uniqKey="Alpers C" first="C N" last="Alpers">C N Alpers</name>
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<author><name sortKey="Dileanis, P" sort="Dileanis, P" uniqKey="Dileanis P" first="P" last="Dileanis">P. Dileanis</name>
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<sourceDesc><biblStruct><analytic><title xml:lang="en">Selected trace elements in the Sacramento River, California: occurrence and distribution.</title>
<author><name sortKey="Taylor, H E" sort="Taylor, H E" uniqKey="Taylor H" first="H E" last="Taylor">H E Taylor</name>
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<front><div type="abstract" xml:lang="en">The impact of trace elements from the Iron Mountain Superfund site on the Sacramento River and selected tributaries is examined. The concentration and distribution of many trace elements-including aluminum, arsenic, boron, barium, beryllium, bismuth, cadmium, cerium, cobalt, chromium, cesium, copper, dysprosium, erbium, europium, iron, gadolinium, holmium, potassium, lanthanum, lithium, lutetium, manganese, molybdenum, neodymium, nickel, lead, praseodymium, rubidium, rhenium, antimony, selenium, samarium, strontium, terbium, thallium, thulium, uranium, vanadium, tungsten, yttrium, ytterbium, zinc, and zirconium-were measured using a combination of inductively coupled plasma-mass spectrometry and inductively coupled plasma-atomic emission spectrometry. Samples were collected using ultraclean techniques at selected sites in tributaries and the Sacramento River from below Shasta Dam to Freeport, California, at six separate time periods from mid-1996 to mid-1997. Trace-element concentrations in dissolved (ultrafiltered [0.005-μm pore size]) and colloidal material, isolated at each site from large volume samples, are reported. For example, dissolved Zn ranged from 900 μg/L at Spring Creek (Iron Mountain acid mine drainage into Keswick Reservoir) to 0.65 μg/L at the Freeport site on the Sacramento River. Zn associated with colloidal material ranged from 4.3 μg/L (colloid-equivalent concentration) in Spring Creek to 21.8 μg/L at the Colusa site on the Sacramento River. Virtually all of the trace elements exist in Spring Creek in the dissolved form. On entering Keswick Reservoir, the metals are at least partially converted by precipitation or adsorption to the particulate phase. Despite this observation, few of the elements are removed by settling; instead the majority is transported, associated with colloids, downriver, at least to the Bend Bridge site, which is 67 km from Keswick Dam. Most trace elements are strongly associated with the colloid phase going downriver under both low- and high-flow conditions.</div>
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<Title>Archives of environmental contamination and toxicology</Title>
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<ArticleTitle>Selected trace elements in the Sacramento River, California: occurrence and distribution.</ArticleTitle>
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<Abstract><AbstractText>The impact of trace elements from the Iron Mountain Superfund site on the Sacramento River and selected tributaries is examined. The concentration and distribution of many trace elements-including aluminum, arsenic, boron, barium, beryllium, bismuth, cadmium, cerium, cobalt, chromium, cesium, copper, dysprosium, erbium, europium, iron, gadolinium, holmium, potassium, lanthanum, lithium, lutetium, manganese, molybdenum, neodymium, nickel, lead, praseodymium, rubidium, rhenium, antimony, selenium, samarium, strontium, terbium, thallium, thulium, uranium, vanadium, tungsten, yttrium, ytterbium, zinc, and zirconium-were measured using a combination of inductively coupled plasma-mass spectrometry and inductively coupled plasma-atomic emission spectrometry. Samples were collected using ultraclean techniques at selected sites in tributaries and the Sacramento River from below Shasta Dam to Freeport, California, at six separate time periods from mid-1996 to mid-1997. Trace-element concentrations in dissolved (ultrafiltered [0.005-μm pore size]) and colloidal material, isolated at each site from large volume samples, are reported. For example, dissolved Zn ranged from 900 μg/L at Spring Creek (Iron Mountain acid mine drainage into Keswick Reservoir) to 0.65 μg/L at the Freeport site on the Sacramento River. Zn associated with colloidal material ranged from 4.3 μg/L (colloid-equivalent concentration) in Spring Creek to 21.8 μg/L at the Colusa site on the Sacramento River. Virtually all of the trace elements exist in Spring Creek in the dissolved form. On entering Keswick Reservoir, the metals are at least partially converted by precipitation or adsorption to the particulate phase. Despite this observation, few of the elements are removed by settling; instead the majority is transported, associated with colloids, downriver, at least to the Bend Bridge site, which is 67 km from Keswick Dam. Most trace elements are strongly associated with the colloid phase going downriver under both low- and high-flow conditions.</AbstractText>
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Selected trace elements in the Sacramento River, California: occurrence and distribution.

Selected trace elements in the Sacramento River, California: occurrence and distribution.

Source :

English descriptors

Abstract

Links to Exploration step

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri

Pour générer des pages wiki