· Stratigraphy, Depositional Environments, and Reservoir Characteristics of the Tussy (Desmoinesian) Sandstones, Southeast Joiner City Field, Love and Carter Counties, Oklahoma* Jeffrey M. Cook1. Search and Discovery Article #20317 (2015) Posted July 27, 2015
· Poyang Lake is loed in Jiangxi and is the largest freshwater lake of China, 73km long longitudinally and wide latitudinally on average, with a lakeshore length of 1,200km, a surface area of 3,583 km2 (outlet level ), an average depth of, a maximum depth of and a volume of about billion m3.
Cornell Field Crops and Soils Handbook, 1987). SMG* c General Description CEC (cmol /kg soil) 1 Finetextured soils developed from clayey lake sediments and medium to finetextured soils developed from lake sediments. 25 2 Medium to finetextured soils developed from calcareous glacial till, mediumtextured to moderately
Novel foraging patterns by Siberian Cranes were associated with low densities of Vallisneria tubers across multiple sublakes within Poyang Lake National Nature Reserve (PLNR). Foraging success was higher in grasslands than in wetlands in winter 2010–2011, but higher in wetlands following a recovery of Vallisneria in 2011–2012.
· Poyang Lake, Dongting Lake and Shengjin Lake are three extremely important lakes for abundant waterbirds including species of conservation concern (Barter et al. Reference Barter, Chen, Cao and Lei 2004, Reference Barter, Lei and Cao 2006, Ji et al. Reference Ji, Zeng, Wang, Gong, Xu and Bao 2007, Lei et al. Reference Lei, Lei, Tao and Hearn 2011).
The origin and distribution of a sandstone reservoir for petroleum are controlled primarily by the processes by which the sand was deposited. Studies of modern environments of deposition and associated Holocene deposits provide a basis for understanding petroleum fields and predicting reservoir distribution and behavior.
Reservoir Properties Geol493K Porosity and Permeability • Porosity: ... • Effective Porosity = Interconnected pores Conventional View of Porosity • 05% Negligible • 510% Poor • 1015% Fair • 1520% Good • 2025% Very Good For gas, lower porosity is still viable Hydrofracturing makes low ... Sand Poorly Sorted Sand Porosity ...
· Such lakes support aquatic species who require welloxygenated, cold waters such as lake trout. Oligotrophic lakes are usually found in the cold regions of the world where mixing of nutrients is rare and slow due to the low temperatures of the lake waters. Mesotrophic: Lakes with an intermediate level of productivity are called mesotrophic lakes.
The soil and rock descriptions that are contained on the field logs should be based on ... size or smaller by normal hand pressure, should be classified as a soil. Soil Classifiion ... sand and gravel contained in the field sample. Tables 44 through 47 should be used in describing finegrained
· Sand mining in Poyang Lake quickly developed into an industry involving hundreds of large vessels (de Leeuw et al., 2010, Wu et al., 2007). In this paper, we argue that the major determinant of lower lake levels during the past decade is primarily because of sand mining increasing Poyang Lake's discharge ability into the Yangtze River.
· Reservoir Porosity. Porosity is the void space in a rock that can store the fluids. It is measured as either a volume percentage or a fraction (expressed as a decimal). In the subsurface this volume may be filled with petroleum (oil and gas), water, a range of non hydrocarbon gasses (CO2, H2S, N2), or some combination of these.
The conventional model involves a large tank buried in the ground near the home or building that it will service. Using gravity, the wastewater that comes from the home drains into the tank. The water line in and out continues to drain liquid out from the tank to the ground which is known as the drain field.
Sand mining and increasing Poyang Lake's discharge ability: A reassessment of causes for lake decline in China. Journal of Hydrology, 2014. Claire Huber.
Nine sand samples above represent nine different sand types. Row by row from left to right: 1. Glass sand from Kauai, Hawaii 2. Dune sand from the Gobi Desert, Mongolia 3. Quartz sand with green glauconite from Estonia 4. Volcanic sand with reddish weathered basalt from Maui, Hawaii 5. Biogenic coral sand from Molokai, Hawaii 6.