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Title: (U) Introduction to Portage

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  1. Los Alamos National Laboratory
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Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
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Conference: NECDC ; 2016-10-10 - 2016-10-10 ; Livermore, California, United States
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United States

Citation Formats

Herring, Angela M., Certik, Ondrej, Ferenbaugh, Charles Roger, Garimella, Rao Veerabhadra, Jean, Brian Altom, Malone, Christopher M., and Sewell, Christopher Meyer. (U) Introduction to Portage. United States: N. p., 2017. Web.
Herring, Angela M., Certik, Ondrej, Ferenbaugh, Charles Roger, Garimella, Rao Veerabhadra, Jean, Brian Altom, Malone, Christopher M., & Sewell, Christopher Meyer. (U) Introduction to Portage. United States.
Herring, Angela M., Certik, Ondrej, Ferenbaugh, Charles Roger, Garimella, Rao Veerabhadra, Jean, Brian Altom, Malone, Christopher M., and Sewell, Christopher Meyer. Fri . "(U) Introduction to Portage". United States. doi:.
title = {(U) Introduction to Portage},
author = {Herring, Angela M. and Certik, Ondrej and Ferenbaugh, Charles Roger and Garimella, Rao Veerabhadra and Jean, Brian Altom and Malone, Christopher M. and Sewell, Christopher Meyer},
abstractNote = {},
doi = {},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Fri Feb 03 00:00:00 EST 2017},
month = {Fri Feb 03 00:00:00 EST 2017}

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  • Abstract not provided.
  • The Lower Silurian Clinton section (Ordovician Queenston Shale to Packer Shell/Brassfield Limestone) represents a deltaic sequence in Portage County where it occurs approximately 25 mi east of the delta edge and 50 mi east of the sandstone depositional limit. In Portage County, the Clinton section is approximately 190 ft thick. The mean sandstone thickness is 53 ft (range from > 100 to < 10 ft). The mean sandstone thickness is much greater than it is for the Clinton sandstone reservoir closer to the delta edge, where hydrocarbon production is comparable to, or surpasses that in Portage County. It is nowmore » evident that the occurrence of thick, clean Clinton sandstone is not the only primary geologic factor for high production from the reservoir. Two productive areas were studied to isolate controls on hydrocarbon occurrence and production. One area is structurally low, the other is structurally high, but both have about the same mean Clinton sandstone thickness.« less
  • Peat Bogs and wetlands represent unique environmental settings what are increasingly subjected to anthropogenic stresses involving inputs of water and chemicals. This study used geochemical and hydrologic monitoring to determine the inputs and fates of elements of the Kent-Brimfield bog located in Portage County, Ohio. Based on physical and chemical information collected over one year, a model is proposed here describing the hydrologic connection between a bog and shallow ground water surrounding the bog. The chemical composition of precipitation, soil water and ground water in the bog vicinity were monitored for one year. Field measurements included water levels, pH, Eh,more » alkalinity and temperature. Trace metal content of the peat, the pore waters, soil water and ground waters were determined by GFAA, ICP and LIC methods. This bog was found to function as part of a perched water table aquifer. Water in the upper 3 m of the bog is found to be chemically similar to precipitation, but modified by reactions involving dissolution of mineral matter and biologic processes. The chemistry of water deeper in the bog (> 3m) resembles shallow ground water surrounding the bog, modified by weathering of underlying geologic materials and sulfate reduction. This similarity, along with ground water elevations within and outside of the bog, supports that shallow ground water interacts with, and helps maintain water levels in the upper surface of the bog. From these results, a model is proposed for the seasonal variations in hydrologic processes operating in the wetland and surrounding basin, and describes how wetlands may change seasonally from being influent to effluent systems.« less
  • The research reported here extends source apportioment techniques by combining four air quality model types to establish multi-scale source/receptor relationships. The selected models are: Branching Atmospheric Trajectory (BAT) model for regional-scale contributors; Principal Component Analysis (PCA) receptor model for urban and regional-scale contributors; Chemical Mass Balance (CMB) receptor model for urban- and regional-scale contributors; Industrial Source Complex Short-Term (ISC-ST) dispersion model for urban-scale contributors. The framework in which these models are placed allows each one to be replaced with better ones when these new models have been demonstrated to be superior. The theoretical basis, previous applications, and the results ofmore » model evaluation studies are summarized by Chow in great detail and will not be presented here. The objectives of this research are: to develop a method for multi-scale composite modeling applications; to define the data requirements; and to apportion local and distract pollution sources using the composite modeling strategy. Results from the entire research effort are too lengthy to include here. This paper focuses on CMB portion of the method. Trajectory and Principal Component Analyses were reported earlier.« less
  • The Mississippian Berea Sandstone is a reservoir for shallow gas in Randolph and Suffield townships of Portage County, Ohio. The Berea Sandstone is well known in Ohio from its outcrops at the outskirts of Cleveland. It is among the more productive formations in Ohio where it yields gas, oil, or gas and oil at moderate to very shallow depths. The great differences in reservoir quality, sandstone distribution, and producibility in Berea oil and gas fields are partly related to the use of the term Berea for several sandstone bodies that produce from different structural and stratigraphic settings. In Portage County,more » the Berea Sandstone is up to 60 ft (18 m) thick and has a porosity in the 15-25% range. The sand is white, medium to fine-grained quartz, poorly cemented, and without substantial shale interbeds. The reservoir lies below the Cap Berea, a gray, cemented thin bed at the base of the Sunbury Shale (driller's Coffee shale). In Portage County, the sand is currently interpreted as fluvial or deltaic. Within the field, thickness of the reservoir and hydrocarbon saturated zone varies little. Natural gas is produced from the top 30 ft (9 m) of the reservoir. The reservoir energy is water drive. The gas fields lie just updip from a steep structural terrace interpreted as a fault zone. The trap for the fields is anticlinal and the Sunbury Shale is the seal. New wells drilled into the reservoir at 400-500 ft (122-152 m) in depth produce gas without water. Initial open flow tested up to 1.0 MMCFGD at an initial reservoir pressure of about 80 psig (552 kPa).« less