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Journal articles on the topic 'Geology – Georgia – Clay County'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Cook, Robert B. "Lazulite Graves Mountain, Lincoln County, Georgia." Rocks & Minerals 83, no. 4 (2008): 328–33. http://dx.doi.org/10.3200/rmin.83.4.328-333.

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2

Gordon, Jennings B. "A Gahnite Occurrence in Carroll County, Georgia." Rocks & Minerals 63, no. 6 (1988): 471–72. http://dx.doi.org/10.1080/00357529.1988.11761885.

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3

Cook, Robert B. "Connoisseur's Choice: Rutile, Graves Mountain, Lincoln County, Georgia." Rocks & Minerals 78, no. 2 (2003): 112–16. http://dx.doi.org/10.1080/00357529.2003.9926704.

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4

Barwood, Henry, and Robert B. Cook. "The Hogg Estate or Mineral Processing Mine, LaGrange, Troup County, Georgia." Rocks & Minerals 81, no. 3 (2006): 180–86. http://dx.doi.org/10.3200/rmin.81.3.180-186.

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5

Santamaria, Jose, and Jeff Deere. "Through the 'Scope: Baryte Microcrystals from the Cartersville Mining District, Bartow County, Georgia." Rocks & Minerals 96, no. 3 (2021): 270–76. http://dx.doi.org/10.1080/00357529.2021.1875753.

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6

Wight, Georgina Deweese, and Henri D. Grissino-Mayer. "Dendrochronological Dating of an Antebellum Period House, Forsyth County, Georgia, U.S.A." Tree-Ring Research 60, no. 2 (2004): 91–99. http://dx.doi.org/10.3959/1536-1098-60.2.91.

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7

Geffner, Paul. "The Treasure Chest Pockets: An Update on the Jacksons Crossroads Amethyst Mine Wilkes County, Georgia." Rocks & Minerals 83, no. 6 (2008): 550–52. http://dx.doi.org/10.3200/rmin.83.6.550-552.

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8

Turgut, Bülent, and Merve Ateş. "Factors of soil diversity in the Batumi delta (Georgia)." Solid Earth 8, no. 1 (2017): 1–12. http://dx.doi.org/10.5194/se-8-1-2017.

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Abstract. The aim of this study was to determine certain basic properties of soils in the Batumi delta (southwestern Georgia) to determine the relationships of studied properties and to identify differences with regards to these properties between different sampling sites in the delta that were selected based on the delta morphology. In this context, a total of 125 soil samples were collected from five different sampling sites, and the clay, silt and sand content of the samples were determined along with their mean weight diameter (MWD) values, aggregate stability (AS) values, amount of water

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9

Hower, James C., Dali Qian, Nicolas J. Briot, Madison M. Hood, and Cortland F. Eble. "Mineralogy of a rare earth element-rich Manchester coal lithotype, Clay County, Kentucky." International Journal of Coal Geology 220 (March 2020): 103413. http://dx.doi.org/10.1016/j.coal.2020.103413.

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10

Li, Xiao, Timothy Grey, William Vencill, et al. "Evaluation of Cotton Responses to Fomesafen-Based Treatments Applied Preemergence." Weed Technology 32, no. 4 (2018): 431–38. http://dx.doi.org/10.1017/wet.2018.31.

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AbstractFomesafen provides effective control of glyphosate-resistant Palmer amaranth in cotton. However, cotton seedlings can be injured when fomesafen is applied PRE. Therefore, greenhouse and field experiments were conducted at Athens, GA, and at six locations in Alabama and Georgia in 2013 and 2016 to evaluate cotton growth and yield response to fomesafen applied PRE at 70, 140, 280, 560, 1,120, or 2,240 g ai ha−1, and in combination with pendimethalin, diuron, acetochlor, and fluridone at 1×label rates. Greenhouse bioassays indicated that fomesafen reduced cotton height and dry weight with

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11

Fallaw, W., David Snipes, and Van Price. "Wandering With William Bartram: The Section At Silver Bluff, South Carolina." Earth Sciences History 13, no. 1 (1994): 52–57. http://dx.doi.org/10.17704/eshi.13.1.pw32124312286527.

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In his famous book, William Bartram (1791) described a stratigraphic section at Silver Bluff on the Savannah River in Aiken County, South Carolina, as dark, laminated clay containing belemnites, overlain by clays, sand, marl, and a shelly bed containing numerous oysters. There are now no known occurrences of marine megafossils in outcrops along the Savannah in Aiken County. The wording of Bartram's description of Cretaceous outcrops along the Cape Fear River in North Carolina indicates that the lower part of the Silver Bluff section was described from notes made on the Cape Fear and from his f

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12

Burley, Jon Bryan. "A vegetation productivity equation for reclaiming surface mines in Clay County, Minnesota." International Journal of Surface Mining, Reclamation and Environment 5, no. 1 (1991): 1–6. http://dx.doi.org/10.1080/09208119108944279.

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13

Hower, James C., Debora Berti, Michael F. Hochella, and Sarah M. Mardon. "Rare earth minerals in a “no tonstein” section of the Dean (Fire Clay) coal, Knox County, Kentucky." International Journal of Coal Geology 193 (June 2018): 73–86. http://dx.doi.org/10.1016/j.coal.2018.05.001.

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14

Sakulpitakphon, Tanaporn, James C. Hower, William H. Schram, and Colin R. Ward. "Tracking mercury from the mine to the power plant: geochemistry of the Manchester coal bed, Clay County, Kentucky." International Journal of Coal Geology 57, no. 2 (2004): 127–41. http://dx.doi.org/10.1016/j.coal.2003.09.004.

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15

Burley, J. B., and C. H. Thomsen. "Application of an agricultural soil productivity equation for reclaiming surface mines: Clay County, Minnesota." International Journal of Surface Mining, Reclamation and Environment 4, no. 3 (1990): 139–44. http://dx.doi.org/10.1080/09208119008944181.

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16

Medina, Daniel Alonso, and David Budd. "Critical Diagenetic Features Controlling Intergranular Flow Paths and Matrix Permeability in the Codell Sandstone, Northeastern Colorado." Mountain Geologist 57, no. 2 (2020): 95–120. http://dx.doi.org/10.31582/rmag.mg.57.2.95.

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The Codell Sandstone is a hydrocarbon-bearing, tight sand (permeability <0.1 mD) that is an active target for unconventional hydrocarbon production in the Denver-Julesburg Basin. In northeastern Colorado, the intergranular microporous drainage network within this clay-rich sandstone is poorly understood, with a strong diagenetic control suggested by the lack of correlation between permeability and depositional facies. Core samples from the Wattenberg Field and Redtail areas in Weld County were used to identify which diagenetic processes were most important in developing a connected pore net

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17

Doser, Diane I., Marc A. Ornelas, Isaac Martinez, Lixin Jin, Anna Ortiz, and Galen M. Kaip. "Using Geophysics to Investigate Texture and Salinity of Agricultural Soils and Their Impact on Crop Growth in El Paso County, Texas." Journal of Environmental and Engineering Geophysics 24, no. 3 (2019): 465–77. http://dx.doi.org/10.2113/jeeg24.3.465.

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Soil properties within the Rio Grande valley near El Paso are strongly linked to the types of fluvial deposits that serve as parent material. We used four geophysical techniques (DC resistivity, ground conductivity, capacitively coupled resistivity and magnetics) to distinguish between soil units in an alfalfa field. We combined these observations with geochemical characterization and particle size analysis in order to determine how these soils and irrigation practices influence salt buildup and water availability, and thus crop growth. Soils mapped at the site were derived from crevasse splay

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18

Matteson, A., J. P. Tomanic, M. M. Herron, D. F. Allen, and W. E. Kenyon. "NMR Relaxation of Clay/Brine Mixtures." SPE Reservoir Evaluation & Engineering 3, no. 05 (2000): 408–13. http://dx.doi.org/10.2118/66185-pa.

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Summary Effective interpretation of nuclear magnetic resonance (NMR) logs in shaly sands requires an understanding of the NMR contribution of clays. Of particular importance is the role of clays in the rapidly relaxing part of the NMR signal. In this study we measured the transverse relaxation time spectrum T2 of brine mixed with four clays (illite, smectite, kaolinite and glauconite) as a function of compaction. The Larmor frequency was 2 MHz and the echo spacing 0.16 ms. Mild compaction was achieved by centrifuging the clay slurry at three successive pressures ranging from 1 to 125 psi. High

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19

Hughes, Larry J. "Mapping contaminant-transport structures in karst bedrock with ground-penetrating radar." GEOPHYSICS 74, no. 6 (2009): B197—B208. http://dx.doi.org/10.1190/1.3223312.

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Ammonium perchlorate, a risk to human health, was used formerly to manufacture rocket fuel at the Naval Weapons Industrial Reserve Plant (NWIRP) McGregor, McLennon County, Texas. Perchlorate exists in several groundwater contaminant plumes, whose geometries were suspected to be influenced by transmissive bedrock structures. To identify these possible contaminant-transport pathways, a towed-array ground-penetrating radar (GPR) system was used to acquire 118 line-km of data across [Formula: see text] of the property. The shallow geology consists of bedrock limestone overlain by [Formula: see tex

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20

Yang, Ping, Yi-Qun Tang, Nian-Qing Zhou, Jian-Xiu Wang, Tian-Yu She, and Xiao-Hui Zhang. "Characteristics of red clay creep in karst caves and loss leakage of soil in the karst rocky desertification area of Puding County, Guizhou, China." Environmental Earth Sciences 63, no. 3 (2010): 543–49. http://dx.doi.org/10.1007/s12665-010-0721-1.

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21

Morris, T. F., and R. I. Kelly. "Origin and physical and chemical characteristics of glacial overburden in Essex and Kent counties, southwestern Ontario." Canadian Journal of Earth Sciences 34, no. 3 (1997): 233–46. http://dx.doi.org/10.1139/e17-022.

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The overburden of Essex and Kent counties, southwestern Ontario, has been described as consisting of a clayey silt to silty clay till overlying a gravelly unit resting on bedrock. Recent Quaternary geology mapping has identified additional materials and redefined the origin of others by determining the stratigraphic position and physical and geochemical properties of materials encountered in a sonic drilling program and field mapping. Catfish Creek Till was deposited on the bedrock surface during the Nissouri Stadial as ice advanced south over the area. As ice retreated during the Erie Interst

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22

Williams, G. M., A. Stuart, and P. Coulter. "Planning and engineering in relation to waste disposal: a case study of the Alkerton landfill." Geological Society, London, Engineering Geology Special Publications 4, no. 1 (1987): 495–502. http://dx.doi.org/10.1144/gsl.eng.1987.004.01.60.

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AbstractThe integration of planning with geology and engineering is essential in the successful location and development of landfill sites, particularly in areas which are not intrinsically safe for waste disposal without engineering improvements. Although technical matters often form the primary basis for site selection, planning constraints and political factors can be as important and yet may receive less emphasis by the developers. Selection of a site can arouse concern amongst local people who consider that they will be adversely affected, despite assurances from the developer, and the fo

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23

Glassmeyer, Michael P., and Abdul Shakoor. "Factors Contributing to Landslide Susceptibility of the Kope Formation, Cincinnati, Ohio." Environmental and Engineering Geoscience 27, no. 3 (2021): 307–18. http://dx.doi.org/10.2113/eeg-d-20-00077.

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ABSTRACT The objective of this study was to evaluate the factors that contribute to the high frequency of landslides in the Kope Formation and the overlying colluvial soil present in the Cincinnati area, southwestern Ohio. The Kope Formation consists of approximately 80 percent shale inter-bedded with 20 percent limestone. The colluvium that forms from the weathering of the shale bedrock consists of a low-plasticity clay. Based on field observations, LiDAR data, and information gathered from city and county agencies, we created a landslide inventory map for the Cincinnati area, identifying 842

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24

Johnson, Rebecca, Mark Longman, and Brian Ruskin. "Petrographic and Petrophysical Characteristics of the Upper Devonian Three Forks Formation, Southern Nesson Anticline, North Dakota." Mountain Geologist 54, no. 3 (2017): 181–201. http://dx.doi.org/10.31582/rmag.mg.54.3.181.

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The Three Forks Formation, which is about 230 ft thick along the southern Nesson Anticline (McKenzie County, ND), has four “benches” with distinct petrographic and petrophysical characteristics that impact reservoir quality. These relatively clean benches are separated by slightly more illitic (higher gamma-ray) intervals that range in thickness from 10 to 20 ft. Here we compare pore sizes observed in scanning electron microscope (SEM) images of the benches to the total porosity calculated from binned precession decay times from a suite of 13 nuclear magnetic resonance (NMR) logs in the study

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25

Handoo, Z. A., A. M. Skantar, and R. P. Mulrooney. "First Report of the Sting Nematode Belonolaimus longicaudatus on Soybean in Delaware." Plant Disease 94, no. 1 (2010): 133. http://dx.doi.org/10.1094/pdis-94-1-0133b.

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In late July of 2005, several, large, irregular areas of severely chlorotic, stunted, and dead soybean plants were observed in two fields of soybean (Glycine max), 8.05 km apart, in sandy soil (94% sand, 2% silt, and 4% clay) in southwestern Sussex County, DE. The grower also had observed stunted corn the previous year in the same areas and thought the fields had a fertility problem. The morphology of adults and molecular analyses of the juveniles isolated from soil samples established the identity of the species as the sting nematode, Belonolaimus longicaudatus (1–4). The population density w

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26

Zhang, Zhenping, Xiaodong Fu, Qian Sheng, Dawei Yin, Yongqiang Zhou, and Juehao Huang. "Effect of Rainfall Pattern and Crack on the Stability of a Red Bed Slope: A Case Study in Yunnan Province." Advances in Civil Engineering 2021 (January 13, 2021): 1–21. http://dx.doi.org/10.1155/2021/6658211.

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Red bed slopes in the southwest of China are associated with a grant number of geological hazards, such as landslides, mud-rock flows, and rock blocks falling, which are vital problems in geotechnical engineering. The damage can be induced or triggered due to a series of human and environmental activities, such as excavation, concentrated or long-term rainfall, earthquake, and fluctuation of groundwater level. According to the field observations and geological exploration results, a small-scale landslide was observed on January 10, 2016, after excavation along XiaoMo highway in Yunnan Province

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27

Grieser, William V., Robert F. Shelley, Bill J. Johnson, Eugene O. Fielder, James R. Heinze, and James R. Werline. "Data Analysis of Barnett Shale Completions." SPE Journal 13, no. 03 (2008): 366–74. http://dx.doi.org/10.2118/100674-pa.

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Summary The north Texas Barnett shale illustrates the successful commercialization of an unconventional reservoir. However, it took 17 years to evolve from pumping crosslinked gel (XLG) carrying more than 1 million lbm of proppant per job to sand waterfracs (SWFs) consisting of large volumes of water with friction reducer and small quantities of sand. This transition to SWF stimulation opened the door for widespread development that has advanced the Newark East (Barnett shale) to the largest producing gas field in Texas. This paper investigates Barnett completion strategy from 1993 to 2002. Th

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28

Tomson, Mason B., Amy T. Kan, Gongmin Fu, et al. "Mechanistic Understanding of Rock/Phosphonate Interactions and Effect of Metal Ions on Inhibitor Retention." SPE Journal 13, no. 03 (2008): 325–36. http://dx.doi.org/10.2118/100494-pa.

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Summary This paper discusses the effects of Ca2+, Mg2+, and Fe2+ on inhibitor retention and release. Better understanding of phosphonate reactions during inhibitor squeeze treatments has direct implication on how to design and improve scale inhibitor squeeze treatments for optimum scale control. Putting various amounts of metal ions in the inhibitor pill adds another degree of freedom in squeeze design, especially in controlling return concentrations and squeeze life. Phosphonate reactions during squeeze treatments involve a series of self-regulating reactions with calcite and other minerals.

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29

Gregory N. Bonn, David M. Patrick. "Clay Mineral Variations in Marginal Deltaic Plain, Coastal Hancock County, Mississippi: ABSTRACT." AAPG Bulletin 71 (1987). http://dx.doi.org/10.1306/703c7f43-1707-11d7-8645000102c1865d.

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30

Gregory McCrae, Jesse O. Snowden. "Clay-Mineral Segregation by Differential Flocculation: Jourdan River-St. Louis Bay Estuary, Hancock County, Mississippi: ABSTRACT." AAPG Bulletin 72 (1988). http://dx.doi.org/10.1306/703c98a2-1707-11d7-8645000102c1865d.

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31

Steven K. Henderson. "Clay Mineralogy and Reservoir Implications Within the Pennsylvanian Cross Cut Sandstone: TWP Field, Runnels County, Texas: ABSTRACT." AAPG Bulletin 79 (1995). http://dx.doi.org/10.1306/8d2b1d04-171e-11d7-8645000102c1865d.

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32

Tim W. Munson. "Clay Mineralogy and Its Controls on Production, Pennsylvanian Upper Morrow Sandstone, Farnsworth Field, Ochiltree County, Texas: ABSTRACT." AAPG Bulletin 73 (1989). http://dx.doi.org/10.1306/44b4aa7d-170a-11d7-8645000102c1865d.

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33

Michael M. Herron, James A. Grau. "Clay and Framework Mineralogy, Cation Exchange Capacity, Matrix Density, and Porosity from Geochemical Well Logging in Kern County, California: ABSTRACT." AAPG Bulletin 71 (1987). http://dx.doi.org/10.1306/948872c6-1704-11d7-8645000102c1865d.

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