Petroleum Hydrocarbon Bioventing Kinetics Determined in Soil Core, Microcosm, and Tubing Cluster Studies   总被引：2，自引：0，他引：2  

Ellen E. Moyer  David W. Ostendorf  Robin J. Richards  Steve Goodwin 《Ground Water Monitoring & Remediation》1996,16(1):141-153

Aerobic biodegradation of vapor-phase petroleum hydrocarbons was evaluated in an intact soil core from the site of an aviation gasoline release. An unsaturated zone soil core was subjected to a flow of nitrogen gas, oxygen, water vapor, and vapor-phase hydrocarbons in a configuration analogous to a biofilter or an in situ bioventing or sparging situation. The vertical profiles of vapor-phase hydrocarbon concentration in the soil core were determined by gas chromatography of vapor samples. Biodegradation reduced low influent hydrocarbon concentrations by 45 to 92 percent over a 0.6-m interval of an intact soil core. The estimated total hydrocarbon concentration was reduced by 75 percent from 26 to 7 parts per million. Steady-state concentrations were input to a simple analytical model balancing advection and first-order biodegradation of hydrocarbons. First-order rate constants for the major hydrocarbon compounds were used to calibrate the model to the concentration profiles. Rate constants for the seven individual hydrocarbon compounds varied by a factor of 4. Compounds with lower molecular weights, fewer methyl groups, and no quaternary carbons tended to have higher rate constants. The first-order rate constants were consistent with kinetic parameters determined from both microcosm and tubing cluster studies at the field site.  相似文献   

Nant-y-moch grassland improvement study,A. M. Roberts,J. A. Hudson and G. Roberts,Institute of Hydrology,Report No. 104, 1990. No. of pages: 85. Price: £7.00. ISBN 0-948540-16-8     

Keith Richards 《地球表面变化过程与地形》1992,17(6):635-635

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LNAPL Retention in Sandy Soil     

David W. Ostendorf  Robin J. Richards  Frank P. Beck 《Ground water》1993,31(2):285-292

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A terrestrial shear pattern?     

T. Ll. Richards 《Pure and Applied Geophysics》1973,110(1):2012-2021

The concept of the strain ellipsoid is applied to indicate a possible regular shear pattern of earthquake distribution over the Earth's surface. A simple model of the Earth is assumed in the form of a rotating sphere with a plastic interior and a thin, fragile, crust. On this basis rotation of the Earth generates an internal radial pressure at the equator equivalent to 1/300g causing a proportionate distortion of the spherical shell. The system is in dynamic equilibrium with an increase in gravity at the equator. The ellipsoid representing the distortion, has orthogonal principal axes corresponding to the principal strains while radial directions at 54°44 from the poles are unchanged in length and are thus possible axes of shear generating the same distortion. The Alpide region of earthquakes extending from Lisbon to Tokyo and restriction of earthquakes mainly to the broad band between latitudes 55°N or S are in support of the proposed view.Four unique sets of orthogonal shear systems have been identified which form a regular pattern with a definite symmetry with respect to the plane of the ecliptic. This suggests that the hoop stress at the Equator associated with Earth rotation may be triggered off by tidal forces and that earthquake prediction may well be possible. Other implications of this new approach are also discussed.  相似文献   

AstroGrid: A place for your science     

Nicholas A Walton  Eduardo Gonzalez-Solarez  Silvia Dalla  Anita Richards  Jonathon Tedds 《Astronomy& Geophysics》2006,47(3):3.22-3.24

Nicholas A Walton, Silvia Dalla, Eduardo Gonzalez-Solarez, Anita Richards and Jonathan Tedds show off the fast-developing astronomical applications of the UK's virtual observatory service.  相似文献   

MERLIN observations of water maser proper motions in VY Canis Majoris     

A. M. S. Richards  J. A. Yates  & R. J. Cohen 《Monthly notices of the Royal Astronomical Society》1998,299(2):319-331

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Simulation of flow geometry in a riffle-pool stream     

K. S. Richards 《地球表面变化过程与地形》1978,3(4):345-354

The nature of the flow in most natural streams is gradually varied rather than uniform. This is particularly true of streams with coarse gravel bed material organized into relatively stable riffle and pool features. In spite of this, there are few applications of the gradually varied flow models (e.g. the Bernoulli equation) to such streams. This paper presents some initial results of a simulation of flow patterns in two riffle-pool reaches, using an open channel flow profile computation method based on an equation defining an energy balance between successive cross-sections separated by an incremental distance.  相似文献   

Compaction of Argillaceous Sediments — Developments in Sedimentology, 16: H.H. Rieke,III and G.V. Chilingarian. Elsevier,Amsterdam, 1974, 424 pp., Dfl.85.00     

A.F. Richards 《Precambrian Research》1975,2(1):94-95

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Problems in the calibration of an acoustic device for the observation of bedload transport     

K. S. Richards  L. M. Milne 《地球表面变化过程与地形》1979,4(4):335-346

Developments in theoretical and empirical modelling of bedload transport processes are hindered by the lack of an adequate data base for testing or establishing the models. Conventional methods of measuring bedload transport rates fail to provide the necessary continuous or frequent record of variations at a single section. Acoustic techniques have the potential to overcome this deficiency, but their application has been very limited. Some of the problems of calibrating an acoustic device in the field and in a laboratory flume are discussed, and a possible circuit design described which might minimize calibration difficulties by automatically subtracting the noise generated by flow turbulence.  相似文献   

Slope form and basal stream relationships: Some further comments     

K. S. Richards 《地球表面变化过程与地形》1977,2(1):87-92

The nature and strength of the correlation between stream gradient and valley side slope angle are seen to vary according to the order of the stream segment. In addition, it is suggested that the relationship will depend on the efficiency of slope processes, and that this may contribute to tye different from of relationship obtained in different regions.  相似文献