NEW BOOKS     

Marvin Saines 《Ground water》1981,19(2):235-235

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GROUND WATER IN THE NEWS     

Marvin Saines 《Ground water》1972,10(3):47-47

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Geologic controls on movement of produced-water releases at US geological survey research Site A,Skiatook lake,Osage county,Oklahoma     

James K. Otton  Robert A. Zielinski  Bruce D. Smith  Marvin M. Abbott 《Applied Geochemistry》2007

Highly saline produced water was released from multiple sources during oil field operations from 1913 to 1973 at the USGS research Site A on Skiatook Lake in northeastern Oklahoma. Two pits, designed to hold produced water and oil, were major sources for release of these fluids at the site. Produced water spills from these and other features moved downslope following topography and downdip by percolating through permeable eolian sand and colluvium, underlying permeable sandstone, and, to a lesser extent, through shales and mudstones. Saline water penetrated progressively deeper units as it moved through the gently dipping bedrock to the north and NW. A large eroded salt scar north of the pits coincides with underlying fine-grained rocks that have retained substantial concentrations of salt, causing slow revegetation. Where not eroded, thick eolian sand or permeable sandstone bedrock is near the surface, and vegetation has been little affected or has reestablished itself after the introduced salt was flushed by precipitation. The extent of salt-contaminated bedrock extends well beyond existing surface salt scars. These results indicate that one of the legacies of surface salt spills can be a volume of subsurface salinization larger than the visible surface disturbance.  相似文献   

<Superscript>40</Superscript>Ar/<Superscript>39</Superscript>Ar ages of the<Emphasis Type="Italic"> AD</Emphasis> 79 eruption of Vesuvius,Italy     

Marvin Lanphere  Duane Champion  Leone Melluso  Vincenzo Morra  Annamaria Perrotta  Claudio Scarpati  Dario Tedesco  Andrew Calvert 《Bulletin of Volcanology》2007,69(3):259-263

The Italian volcano, Vesuvius, erupted explosively in AD 79. Sanidine from pumice collected at Casti Amanti in Pompeii and Villa Poppea in Oplontis yielded a weighted-mean ⁴⁰Ar/³⁹Ar age of 1925±66 years in 2004 (1σ uncertainty) from incremental-heating experiments of eight aliquants of sanidine. This is the calendar age of the eruption. Our results together with the work of Renne et al. (1997) and Renne and Min (1998) demonstrate the validity of the ⁴⁰Ar/³⁹Ar method to reconstruct the recent eruptive history of young, active volcanoes.  相似文献   

AN OCCURRENCE OF CALCIUM HYDROXIDE GROUND WATER IN JORDAN     

Marvin Saines  Hydrogeologist  Peter Dickson  Engineering Geologist  Paul Lambert  Environmental Chemist 《Ground water》1980,18(5):503-503

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Enriched H₂, CH₄, and He concentrations in hydrothermal plumes associated with the 1996 Gorda Ridge eruptive event     

Deborah S. Kelley  Marvin D. Lilley  John E. Lupton  Eric J. Olson 《Deep Sea Research Part II: Topical Studies in Oceanography》1998,45(12):2665-2682

The rapid field response in March and April 1996 to diking-eruptive events on the Northern Gorda Ridge allowed the first detailed co-measurement of ³He, H₂, and CH₄ in plumes associated with a submarine eruption, and examination of the chemical transformation of these volatile species during aging of the plumes. The diking-eruptive event generated extensive event plumes with a low ³He/heat ratio of ∼0.4×10^-12 cm³ STP gm^-1 °C^-1, while chronic plumes had ³He/heat ratios of 2.1–6.2×10^-12 cm³ STP gm^-1 °C^-1. Hydrogen concentrations in the initial event plume (EP96A) reached a maximum value of 47 nM, 235 times that of ocean background concentration (0.2 nM). In contrast, roughly one month later H₂ concentrations, although still elevated, had drastically dropped to 40 times background values. Methane concentrations in both event and chronic plume fluids were also elevated and similar to stable hydrothermal systems in unsedimented ridge environments, reaching a maximum value of 7 nM. The intense rapid interaction at very high temperatures of hydrothermal fluids with the host rock during dike intrusion or with seawater during extrusion of the basalt likely generated high, localized concentrations of H₂. The data indicate, however, that maximum rates of H₂ production during event plume formation could have lasted a few days at most.  相似文献   

NEWS NOTES     

Marvin Saines 《Ground water》1967,5(2):54-54

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THE HAVERÖ UREILITE: PETROGRAPHIC NOTES     

Ursula B. Marvin  John A. Wood 《Meteoritics & planetary science》1972,7(4):601-610

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NEW BOOKS     

Marvin Saines 《Ground water》1980,18(2):184-184

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NEWS NOTES     

Marvin Saines 《Ground water》1967,5(3):49-49

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