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101.
It has been known for many years that depositional method plays an important part in the results of laboratory testing of clean sands. In this paper, undrained triaxial compression tests were performed on specimens composed of Nevada sand with 20% non-plastic silt content using a variety of depositional methods that include slurry deposition, water sedimentation, air pluviation, mixed dry deposition, and dry funnel deposition. It was found that there was a marked difference in the undrained behavior even though the density and stress conditions were identical. The conclusion was that the soil fabric was responsible for this result. Using the scanning electron microscope, a method was developed to examine and quantify the microstructure of silty sand. These results appear to indicate that there are internal particle structures in sand with silt and their relative quantities correlate with the observed macroscopic undrained behavior. 相似文献
102.
Small diameter core samples were taken from outcrops of the Permian Phosphoria Formation and the Cretaceous Pierre Shale of the Western United States to determine the effects of weathering on organic matter in shale outcrops. While the Pierre Shale core showed no evidence of weathering, the Phosphoria Formation showed significant reduction of overall organic content and pronounced changes in organic composition over the near-surface interval of the core. Total organic carbon is lower by as much as 60% over the upper 2 ft of the core. Chloroform-soluble organic matter and total hydrocarbon (C15+) concentrations are 50% lower over this same interval. The ratio of saturated to aromatic hydrocarbons decreases steadily with core depth over the upper 2.6 ft of the core. Aromatic hydrocarbons are enriched in the stable carbon-13 isotope by an average of 1.7%. over this same interval. Shallow core samples also show a loss of n-paraffins relative to branched/cyclic compounds in the saturated C15+ fraction.Although the extent of weathering is variable, certain characteristic effects are recognizable and can be applied to the interpretation of outcrop data in organic geochemical studies. 相似文献
103.
3ew spectra of Titan centered at 7500 Å, at resolutions of 4 and 1 Å are presented. Weak absorptions coincident with features observed in the spectra of Uranus and Neptune are found. This observation suggests methane abundances in excess of 1 km-am, thereby emphasizing the complexity of line formation in Titan's atmosphere. The question of the total atmospheric pressure of Titan must be reexamined. 相似文献
104.
105.
Assessment of soil organic carbon in semi-arid Sudan using GIS and the CENTURY model 总被引:3,自引:0,他引:3
Using the UNFCCC as a basis, and the objectives of estimating soil organic carbon (SOC) changes during the period 1900–2100, a spatially explicit database of climate, land cover and soil texture was compiled for a 262,000 km2 region in semi-arid Sudan. The area is characterized by low input cultivation of millet, sorghum and sesamé combined with livestock grazing. By integrating the database with the CENTURY ecosystem model, we were able to estimate historical, current and future pools of SOC as a function of land management and climate.The SOC (upper 20 cm) decrease from 1900 to 2000 was estimated to be 6·8 Mt and the maximum potential carbon sink (SOC increase) for the period 2000 to 2100 was estimated to be 17 Mt. Cropland and grassland lost 293 and 152 t SOC km−2 respectively whereas the savannahs gained 76 t SOC km−2 from 1900 to 2000. The SOC sequestration scenario simulated during 2000–2100 recovered 94, 84 and 75 t km−2 for cropland, grassland and savannah respectively.In addition to climate and soils, cropping intensity, fallow periods, fire frequency and grazing intensity also influence cropland SOC variation. Grassland and savannah SOC variations depend on grazing intensity and fire return interval. Land management may affect future amounts of SOC in semi-arid areas thereby turning them from sources into sinks of carbon. SOC estimates were reasonably consistent with measurements (r2=0·70, n=13). 相似文献
106.
Jerry Shannon Mathew E. Hauer Alexis Weaver Sarah Shannon 《The Professional geographer》2018,70(1):84-93
Although general patterns of food insecurity in the United States are known, few studies have attempted to estimate small area food security or account for ongoing socioeconomic changes. Here we address these issues by producing small area estimates of food insecurity in the Atlanta metropolitan area using two methodologies: fixed effects modeling and demographic metabolism. In both cases, we use county-level data from the Current Population Survey to determine the association between food insecurity and demographic predictors. These associations are then applied to tract-level data from the 2009 to 2013 American Community Survey and projected data for 2020 to create small area estimates of food insecurity. We find broad consensus between our two methods. For both time periods, food insecurity is highest in southern sections of the city of Atlanta and its neighboring suburbs. Projections to 2020, however, show that food insecurity rates are projected to increase in outer-ring suburbs east and west of the city while decreasing in the urban core. These results highlight the need to further adapt antihunger efforts for often sprawling suburban communities, where poverty rates are increasing but spatial mismatch combined with poor transit access might hinder access to food assistance. 相似文献
107.
Olajide-Kayode Jerry O. Mustapha Shakirat O. Olatunji Akinade S. Okunlola Olugbenga A. 《Arabian Journal of Geosciences》2020,13(13):1-11
Tight conglomerate reservoirs have complex pore structure and strong heterogeneity which could bring great difficulties in the identification of oil and wa 相似文献
108.
109.
Distinguishing Carbonate Reservoir Pore Facies with Nuclear Magnetic Resonance Measurements 总被引:1,自引:0,他引:1
Characterization of carbonate rocks may involve identifying the important pore types which are present. In the past, this
task has required detailed petrographic analysis of many core samples. Here, we describe a method which uses nuclear magnetic
resonance (NMR) measurements to reduce the amount of petrographic analysis needed for porosity typing of carbonate reservoir
rocks.
For a rock sample which has been measured with NMR, our method decomposes the log(T2) spectrum into at most three Gaussian-shaped components and gives a set of nine parameters. Two characteristic quantities
having geological significance are extracted from the nine parameters. Values of the two quantities are compared with a reference
set, established from samples having both NMR and petrographic evaluations of porosity types. We use a Bayesian approach to
the classification of the dominant porosity type.
Tests of our method on 103 samples show a correct prediction in 60 to 90 percent of the samples. The lower success rate was
obtained for samples with five porosity types from three fields; the higher success rate obtained with samples with three
porosity types from one well. The use of geologically significant quantities extracted from the decomposition gives comparable
success rate to those obtained using a standard, non-geological approach such as canonical variates. 相似文献
110.
Jerry E. Mueller 《The Professional geographer》1979,31(3):306-311
Although stream length is a fundamental property of fluvially eroded landscapes, methods of obtaining this basic measure vary; therefore, data compiled from several sources are often not comparable. Not only are measurement methods inconsistent, but there is no standaid definition of stream length itself. Most measurements are taken directly from maps where accuracy may be questionable, and air photos have proven more reliable than topographic maps. Obtaining reliable stream-length data from published sources is perhaps the most perplexing problem of all. In investigations of stream length, therefore, it is imperative that data sources, measurement techniques, and methodology be clearly defined so that results may be studied in a meaningful context. 相似文献