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Articoli di riviste sul tema "Coal mine soils"

1

Singer, David, Elizabeth Herndon, Laura Zemanek, Kortney Cole, Tyler Sanda, John Senko e Nicolas Perdrial. "Biogeochemical Controls on the Potential for Long-Term Contaminant Leaching from Soils Developing on Historic Coal Mine Spoil". Soil Systems 5, n. 1 (30 dicembre 2020): 3. http://dx.doi.org/10.3390/soilsystems5010003.

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Coal mine spoil is widespread in US coal mining regions, and the potential long-term leaching of toxic metal(loid)s is a significant and underappreciated issue. This study aimed to determine the flux of contaminants from historic mine coal spoil at a field site located in Appalachian Ohio (USA) and link pore water composition and solid-phase composition to the weathering reaction stages within the soils. The overall mineralogical and microbial community composition indicates that despite very different soil formation pathways, soils developing on historic coal mine spoil and an undisturbed soil are currently dominated by similar mineral weathering reactions. Both soils contained pyrite coated with clays and secondary oxide minerals. However, mine spoil soil contained abundant residual coal, with abundant Fe- and Mn- (oxy)hydroxides. These secondary phases likely control and mitigate trace metal (Cu, Ni, and Zn) transport from the soils. While Mn was highly mobile in Mn-enriched soils, Fe and Al mobility may be more controlled by dissolved organic carbon dynamics than mineral abundance. There is also likely an underappreciated risk of Mn transport from coal mine spoil, and that mine spoil soils could become a major source of metals if local biogeochemical conditions change.
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Zhang, Jian, Yinghe Xie, Ying Wei, Huisheng Meng, Yanzhuan Cao, Junmei Qin e Jianping Hong. "Effects of fertilisation on microbial communities in short-term coal mine reclamation". Soil Research 58, n. 8 (2020): 779. http://dx.doi.org/10.1071/sr19262.

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The recovery of the belowground microbial community structure and diversity that occurs in long-term coal mining reclamation is critical to reclamation success. However, long-term coal mining reclamation can take ~10–30 years. Therefore, finding an effective method for promoting coal mine soil restoration in the short-term is necessary to minimise reclamation time. This study investigated the response of soil bacterial communities to fertilisation along a chronosequence of short-term reclamation. Fertilised and unfertilised soils with three short-term reclamation stages were examined to characterise soil properties, as well as bacterial structure and diversity. Fertilisation promoted available nitrogen, phosphate, potassium, and soil organic matter, as well as benefits in bacterial community diversity across the three stages, with the most beneficial effects at 7 years. 16S rRNA sequencing data showed that the predominant phyla across all soils were Proteobacteria, Actinobacteria, Acidobacteria, Bacteroidetes, Chloroflexi, and Gemmatimonadetes. Abundance of each phylum was altered by reclamation time and fertilisation. Clustering and functional analysis indicated that the bacterial community structure in soils with a longer reclamation time was more similar to that in natural soils, suggesting that longer reclamation resulted in increased soil activity and bacterial community diversity, which is likely also true for fertilisation. Our results demonstrate that reclamation duration is the main driving force to recover soil properties and bacterial communities, and fertilisation could enhance the beneficial effects with longer reclamation duration. Therefore, short-term reclamation, combined with fertiliser, is a potential strategy to improve soil conditions in coal mine areas and shorten the recovery time of reclaimed soils.
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Seybold, C. A., R. B. Grossman, H. R. Sinclair, K. M. McWilliams, G. R. Struben e S. L. Wade. "EVALUATING SOIL QUALITY ON RECLAIMED COAL MINE SOILS IN INDIANA". Journal American Society of Mining and Reclamation 2004, n. 1 (30 giugno 2004): 1644–63. http://dx.doi.org/10.21000/jasmr0401644.

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Herndon, Elizabeth, Brianne Yarger, Hannah Frederick e David Singer. "Iron and Manganese Biogeochemistry in Forested Coal Mine Spoil". Soil Systems 3, n. 1 (8 febbraio 2019): 13. http://dx.doi.org/10.3390/soilsystems3010013.

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Abandoned mine lands continue to serve as non-point sources of acid and metal contamination to water bodies long after mining operations have ended. Although soils formed from abandoned mine spoil can support forest vegetation, as observed throughout the Appalachian coal basin, the effects of vegetation on metal cycling in these regions remain poorly characterized. Iron (Fe) and manganese (Mn) biogeochemistry were examined at a former coal mine where deciduous trees grow on mine spoil deposited nearly a century ago. Forest vegetation growing on mine spoil effectively removed dissolved Mn from pore water; however, mineral weathering at a reaction front below the rooting zone resulted in high quantities of leached Mn. Iron was taken up in relatively low quantities by vegetation but was more readily mobilized by dissolved organic carbon produced in the surface soil. Dissolved Fe was low below the reaction front, suggesting that iron oxyhydroxide precipitation retains Fe within the system. These results indicate that mine spoil continues to produce Mn contamination, but vegetation can accumulate Mn and mitigate its leaching from shallow soils, potentially also decreasing Mn leaching from deeper soils by reducing infiltration. Vegetation had less impact on Fe mobility, which was retained as Fe oxides following oxidative weathering.
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Tang, Mei Zhen, Min Yuan, Jian Li Ma, Jun Feng Chen e Hai Li Fu. "Studies on Soil Enzymatic Activities in Areas around Coal Mine". Advanced Materials Research 518-523 (maggio 2012): 1986–93. http://dx.doi.org/10.4028/www.scientific.net/amr.518-523.1986.

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Soil enzymatic activities such as urease and invertase, were determined in areas polluted by Nesslers reagent colorimentric method and Mo-Phosphate colorimentric method in Yu Long coal mine, Shandong Province. The index of heavy metal pollution and the relationship between the activities of soil enzymes were analyzed. The results showed that the contents of heavy metals in contaminated soils were higher than those in unpolluted soils and the enzyme activities were decreased significantly with increasing contamination. The results of multivariate regression model test indicated that the elements of soil heavy metals have different influence on the soil enzymatic activities. It is feasible to use this index as a primary biochemical parameter to evaluate compound heavy metals pollution.
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Masto, R. E., S. Sheik, G. Nehru, V. A. Selvi, J. George e L. C. Ram. "Assessment of environmental soil quality around Sonepur Bazari mine of Raniganj coalfield, India". Solid Earth 6, n. 3 (8 luglio 2015): 811–21. http://dx.doi.org/10.5194/se-6-811-2015.

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Abstract. Assessment of soil quality is one of the key parameters for evaluation of environmental contamination in the mining ecosystem. To investigate the effect of coal mining on soil quality, opencast and underground mining sites were selected in the Raniganj coalfield area, India. The physical, chemical, and biological parameters of the soils, and trace metals and PAHs (polycyclic aromatic hydrocarbons) in the soils were evaluated. Soil dehydrogenase (+79 %) and fluorescein (+32 %) activities were significantly higher in underground mine (UGM) soil, whereas peroxidase activity (+57 %) was higher in opencast mine (OCM) soil. Content of As, Be, Co, Cr, Cu, Mn, Ni, and Pb was significantly higher in OCM soil, whereas Cd was higher in UGM. In general, the PAHs contents were higher in UGM soils, probably due to the natural coal burning at these sites. The observed values for the above properties were converted into a unitless score (0–1.00) and the scores were integrated into an environmental soil quality index (ESQI). In the unscreened index (ESQI-1) all the soil parameters were included and the results showed that the quality of the soil was better for UGM (0.539) than the OCM (0.511) soils. Principal component analysis was employed to derive ESQI-2 and accordingly, total PAHs, loss on ignition, bulk density, Be, Co, Cr, Ni, Pb, and microbial quotient (respiration: microbial biomass ratio) were found to be the most critical properties. The ESQI-2 was also higher for soils near UGM (+10.1 %). The observed indicators and the ESQI results revealed that soil quality assessment for these coal mining soils is largely depended on soil PAHs and potentially toxic trace metals. The proposed ESQI may be further refined by incorporating specific parameters related to human exposure risks and exposure pathways.
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Sena, Kenton L., Kevin M. Yeager, Christopher D. Barton, John M. Lhotka, William E. Bond e Kimberly J. Schindler. "Development of Mine Soils in a Chronosequence of Forestry-Reclaimed Sites in Eastern Kentucky". Minerals 11, n. 4 (16 aprile 2021): 422. http://dx.doi.org/10.3390/min11040422.

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Surface mining for coal has contributed to widespread deforestation and soil loss in coal mining regions around the world, and particularly in Appalachia, USA. Mined land reforestation is of interest in this and other regions where forests are the dominant pre-mining land use. This study evaluated mine soil development on surface-mined sites reforested according to the Forestry Reclamation Approach, representing a chronosequence of time ranging from 0 to 19 years after reclamation. Soils were sampled in depth increments to 50 cm and analyzed for a suite of soil physical and chemical characteristics. Overall, soil fines (silt + clay) tended to increase over time since reclamation (17% silt at year 0 increasing to 35% at year 11; 3.2% clay at year 0 increasing to 5.7% at year 14) while concentrations of metals (e.g., Al, Mg, Mn, Na) demonstrated varied relationships with time since reclamation. Concentrations of organic carbon (OC) tended to increase with time (0.9% OC at year 0 increasing to 2.3% at year 14), and were most enriched in near-surface soils. Some soil characteristics (e.g., Na, OC, Ca) demonstrated patterns of increasing similarity to the forest control, while others were distinct from the forest control throughout the chronosequence (e.g., Al, clay, Mn, gravel). Future surveys of these soils over time will elucidate longer-term patterns in soil development, and better characterize the time scales over which these soils might be expected to approximate forest soil conditions.
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Pajak, M., e W. Krzaklewski. "Selected physical properties of initial soils on the outside spoil bank of the Belchatow brown coal mine". Journal of Forest Science 53, No. 7 (7 gennaio 2008): 308–13. http://dx.doi.org/10.17221/2077-jfs.

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The purpose of the study was to assess, in respect of selected physical properties, the reclamation of the northern slope of the outside spoil bank of the Belchatów brown coal mine by reforestation carried out 20 years ago. Investigations were carried out on 55 permanent research plots. This study confirmed the efficiency of reclamation of strip-mine spoils, and its results allowed to point out the properties of initial soils as the most useful characteristics for the assessment of land reclamation by reforestation.
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Thomas, C., A. Sexstone e J. Skousen. "Soil biochemical properties in brown and gray mine soils with and without hydroseeding". SOIL 1, n. 2 (16 settembre 2015): 621–29. http://dx.doi.org/10.5194/soil-1-621-2015.

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Abstract. Surface coal mining in the eastern USA disturbs hundreds of hectares of land every year and removes valuable and ecologically diverse eastern deciduous forests. Reclamation involves restoring the landscape to approximate original contour, replacing the topsoil, and revegetating the site with trees and herbaceous species to a designated post-mining land use. Re-establishing an ecosystem of ecological and economic value as well as restoring soil quality on disturbed sites are the goals of land reclamation, and microbial properties of mine soils can be indicators of restoration success. Reforestation plots were constructed in 2007 using weathered brown sandstone or unweathered gray sandstone as topsoil substitutes to evaluate tree growth and soil properties at Arch Coal's Birch River mine in West Virginia, USA. All plots were planted with 12 hardwood tree species and subplots were hydroseeded with a herbaceous seed mix and fertilizer. After 6 years, the average tree volume index was nearly 10 times greater for trees grown in brown (3853 cm3) compared to gray mine soils (407 cm3). Average pH of brown mine soils increased from 4.7 to 5.0, while gray mine soils declined from 7.9 to 7.0. Hydroseeding doubled tree volume index and ground cover on both mine soils. Hydroseeding doubled microbial biomass carbon (MBC) on brown mine soils (8.7 vs. 17.5 mg kg−1), but showed no effect on gray mine soils (13.3 vs. 12.8 mg kg−1). Hydroseeding also increased the ratio of MBC to soil organic C in both soils and more than tripled the ratio for potentially mineralizable nitrogen (PMN) to total N. Brown mine soils were a better growth medium than gray mine soils and hydroseeding was an important component of reclamation due to improved biochemical properties and microbial activity in mine soils.
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Olumuyiwa, Amosu Cyril. "Reclamation of the Enugu Coal Mine Site at Abandonment". Indian Journal of Environment Engineering 1, n. 2 (10 novembre 2021): 18–24. http://dx.doi.org/10.35940/ijee.a1812.111221.

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Mining of coal (fossil fuel) resources in Enugu resulted in groundwater pollution/depletion and left the mine site with the potentials of air pollution, loss of landscape/aesthetic degradation and soil contamination. Other Environmental impacts were extensive soil damage, alteration in microbial communities and affecting vegetation leading to destruction of vast amounts of land and displacement of dwellers. Reclamation is the process to restore the ecological integrity of these disturbed mine land areas. It includes the management of all types of physical, chemical and biological disturbances of soils such as soil pH, fertility, microbial community and various soil nutrient cycles that makes the degraded land soil productive. Mining does not mean permanent loss of land for other use. On the other hand it holds potential for altered and improved use apart from restoring for agriculture, forestry and irrigation. This paper attempts to view the best practices for reclaiming the abandoned Enugu coal mine site which ceased production since 2002.
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Tesi sul tema "Coal mine soils"

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Thomas, Kevin A. "Characterization and quality of soils developing on a mountaintop removal coal mine". Morgantown, W. Va. : [West Virginia University Libraries], 2001. http://etd.wvu.edu/templates/showETD.cfm?recnum=2152.

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Thesis (M.S.)--West Virginia University, 2001.
Title from document title page. Document formatted into pages; contains 149 p. : ill. (some col.), map (part col.). Vita. Includes abstract. Includes bibliographical references (p. 66-71).
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Day, A. D., e K. L. Ludeke. "Reclamation and Fertilization of Coal Mine Soils in the Southwestern Desert". University of Arizona (Tucson, AZ), 1986. http://hdl.handle.net/10150/609071.

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A 5 -year experiment was conducted from 1978 through 1982 on the Black Mesa Coal Mine, Kayenta, Arizona, to study plant species best suited for coal mine reclamation and the effects of fertilizer on selected species. Five plant species were broadcast seeded on coal mine soil (spoils) and unmined soil. Prior to planting, 560 kg /ha of 16-20-0 fertilizer were applied on one -half of each site while the other half received no fertilizer. Immediately after planting, sprinkler irrigation water was applied on all plots, as needed, for the first two years. After two years, fertilizer and irrigation were discontinued on both soil materials and all plant species received only natural rainfall for the following three years. Coal mine soil contained more total soluble salts, nitrogen, potassium, sodium, and organic matter than did unmined soil; however, unmined soil had a higher pH and contained more phosphorous than did coal mine soil. Plant growth measurements were recorded for each plant species in October of each year. In general, plants grew better and produced more forage in unmined soil than they did in coal mine soil. All plant species grew better, yielded more forage, and produced a more satisfactory ground cover when they were fertilized than they did when they were not fertilized. Plant species differed greatly in general growth, forage yield, and percent ground cover within soil materials and within fertilizer treatments. Crested wheatgrass (Agropyron cristaturn L.), western wheatgrass (Agropyron smithii Rydb.), and vernal alfalfa (Medicago sativa L.) grew better, yielded more forage, and produced a more complete ground cover than did Indian ricegrass (Oryzopsis hymenoides Ricker) or fourwing saltbrush (Atriplex canescens Pursh). In general, the reclamation of unmined soil with fertilizer and a combination of natural rainfall and sprinkler irrigation during the first two years and with perennial grasses was more successful than the reclamation of coal mine soil with no fertilizer and with legumes or shrubs in the semiarid environment in the southwestern United States.
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Shah, Syed Sabir Hussain. "Transformations of nitrogen and its availability to plants in coal mine soils". Thesis, University of Glasgow, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.293383.

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Wood, Daniel L. "Lime Treatment of Coal Mine Spoil Impacted Soils in the Huff Run Watershed of Northeast Ohio". Kent State University / OhioLINK, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=kent1532101439596856.

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Craig, Nina Genevieve. "Properties and Potentials of Coal Mine Soils in Southwest Virginia 29 Years After Establishment". Thesis, Virginia Tech, 2013. http://hdl.handle.net/10919/19255.

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Current reclamation research following surface mining in the Appalachian coal region seeks to measure carbon (C) and nutrient accumulation and retention under forest vegetation to better understand the role of reforestation in the re-establishment of these ecosystem services. This study capitalized on the Controlled Overburden Placement Experiment (COPE), a 29-year-old reclamation research installation in southwestern Virginia, to estimate long-term mine soil C sequestration potentials and nutrient capitals after different reclamation strategies. The COPE includes two studies, a rock mix study (RM) comparing topsoil substitutes created from different ratios of local overburden [pure sandstone (SS), pure siltstone (SiS), 2:1 SS to SiS, 1:1 SS to SiS, and 1:2 SS to SiS], and a surface amendment study (SA) comparing organic amendments [control (CON), natural topsoil (TS), sawdust (SD), and 22 Mg ha-1 (22B), 56 Mg ha-1 (56B), 112 Mg ha-1 (112B) and 224 Mg ha-1 (224B) of biosolids] on a common 2:1 SS to SiS topsoil substitute. In the RM, overburden selection significantly affected soil nitrogen (N) and C concentrations as well as many other soil chemical [e.g., available phosphorus (P), pH, and other macro- and micronutrients) and physical (e.g., sand, silt and clay contents) properties.    C sequestration rates were also significantly different and ranged from 0.13 to 0.47 Mg C ha-1 yr-1. Many of the differences demonstrated relationships with the mineral make-up of the RM treatment. The SA mine soils also differed significantly in many properties after 29 years, including N, C, and many other nutrient concentrations and contents. C sequestration rates were also significantly different with the SD and 224B treatments having negative sequestration rates, and the remaining treatments ranging from 0.23 to 0.80 Mg C ha-1 yr-1. Collectively, the results demonstrate that topsoil substitutes and surface amendments show divergent trends in soil C and nutrient dynamics after nearly three decades of development and stress the importance of post- mining reclamation based on available materials and reclamation goals.
Master of Science
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Hardiputra, Bingah Astuti. "Properties of rehabilitated coalmine soils at Collie". University of Western Australia. Soil Science and Plant Nutrition Discipline Group, 2004. http://theses.library.uwa.edu.au/adt-WU2005.0041.

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[Truncated abstract] Many soil properties are involved in supporting the growth of plants and in limiting soil degradation. The present study was carried out to provide a basis for minimising environmental impact by providing a firm understanding of the soil properties that affect plant growth for soils developed from mining waste from the Wesfarmers Premier coalmine at Collie. The purpose of this study was to provide an understanding of the soil materials and to identify the potential interactions between soil properties and plants for soils developed on coalmine materials at the Premier mine, Collie. This research was to identify the nature of the manmade soils so as to determine if soil forming processes are active, to determine soil acidity including pH buffering capacity and the lime requirement of soils, to measure water retention characteristics and soil available water for plant growth, to relate soil properties to possible effects on plant growth, and to identify management strategies to improve soil conditions and overcome plant growth constraints. Seventy-seven manmade horizons from pits in 18 constructed soils, ranging from 9 to 21-years old, were analyzed throughout this study. These samples are classified based on soil depth, layer (topsoil and subsoil), and age of soil since rehabilitation. The methods for doing most of the analyses follow the Australian Soil and Land Survey handbook by Rayment and Higginson (1992). The results are presented quantitatively and soil properties are compared to provide information on pedogenic processes, the extent of soil development, the ability of the soils to resist degradation and to provide an indication of soil parent materials
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Barone, Jessica Lynn. "Petrological and geochemical analysis of coal mine spoil to determine the source of magnesium-rich groundwater, Star Fire Mine, Eastern Kentucky". Virtual Press, 2000. http://liblink.bsu.edu/uhtbin/catkey/1189406.

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The Star Fire Coal Mine is a large strip mining operation (10,000 acre permit) that produces mine spoil consisting of sandstones, shales, siltstones, and underclays of the Pennsylvanian Breathitt Formation. Chemical analysis of groundwater from the saturated mine spoil show unusually high magnesium concentrations, with magnesium constituting between 27 and 47 percent of the major cations. Excess magnesium in water is detrimental to plant metabolism, and its content in groundwater may limit its use for irrigation and other uses during a post-mining land use plan. Petrological methods (thin section point count analysis and x-ray diffraction) and geochemical methods (electron microprobe analysis and water extraction experiments) were performed to determine the source of magnesium in sandstone and shale samples of the Breathitt Formation. Based on mineral percents and concentrations of magnesium found in samples used for waterrock interaction samples, magnesium-rich siderite was found as the primary contributor of magnesium to the groundwater.
Department of Geology
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Turney, Douglas C. "Hydrologic investigation of coal mine spoil near Howard Williams Lake, Perry County, Ohio". Ohio : Ohio University, 1996. http://www.ohiolink.edu/etd/view.cgi?ohiou1177703503.

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Van, Blerk Gerhardus Nicolas. "Microbial community structure and dynamics within sulphate- removing bioreactors". Diss., Pretoria : [s.n.], 2009. http://upetd.up.ac.za/thesis/available/etd-08122009-132505.

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Beletse, Yacob Ghebretinsae. "The environmental impact and sustainability of irrigation with coal-mine water". Pretoria : [s.n.], 2008. http://upetd.up.ac.za/thesis/available/etd-05242009-125253.

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Libri sul tema "Coal mine soils"

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Gitt, M. J. Abandoned coal refuse reclamation in the northern plains. Bozeman, Mont: Reclamation Research Unit, Montana State University, 1987.

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Francis, Richard E. Vegetation establishment on reclaimed coal mine spoils in northwestern New Mexico. Fort Collins, Colo: USDA Forest Service, Rocky Mountain Forest and Range Experiment Station, 1991.

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Chugh, Yoginder P. In situ strength characteristics of coal mine floor strata in Illinois. Champaign, Ill. (615 E. Peabody Dr., Champaign 61820): Illinois Mine Subsidence Research Program, 1988.

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Chugh, Yoginder P. In situ strength characteristics of coal mine floor strata in Illinois. Champaign, IL: Illinois State Geological Survey, 1988.

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Chugh, Yoginder P. In situ strength characteristics of coal mine floor strata in Illinois. Champaign, Ill: Illinois State Geological Survey, 1987.

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Fresquez, Philip R. Number of fungal colonies required to describe species differences on reclaimed coal mine areas in New Mexico. [Fort Collins, Colo.]: Rocky Mountain Forest and Range Experiment Station, 1989.

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Norland, Michael R. Soil characterization and soil amendment use on coal surface mine lands: An annotated bibliography. [Washington, DC]: U.S. Dept. of the Interior, Bureau of Mines, 1991.

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Norland, Michael R. Soil characterization and soil amendment use on coal surface mine lands: An annotated bibliography. Washington, DC: U.S. Dept. of the Interior, Bureau of Mines, 1990.

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Saini, Pradeep. Nitrogen transformations and nitrate leaching in mine soils reclaimed with sewage sludge and coal combustion residues. Morgantown, WV: College of Agriculture and Forestry, West Virginia University, 1994.

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Hetzler, R. T. Coal mine subsidence mitigation: effects on soil and crop yields. S.l: s.n, 1992.

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Capitoli di libri sul tema "Coal mine soils"

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Haigh, Marting J. "Slope evolution on coal-mine disturbed land". In Environmental Geotechnics and Problematic Soils and Rocks, 3–13. London: CRC Press, 2021. http://dx.doi.org/10.1201/9781003211051-2.

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Semmens, Kenneth J., e James A. Jacobs. "Sustainable Aquaculture Using Treated and Untreated Mine Water from Coal Mines". In Acid Mine Drainage, Rock Drainage, and Acid Sulfate Soils, 419–29. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2014. http://dx.doi.org/10.1002/9781118749197.ch36.

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Marcos, M. L. Fernández, E. Alvarez Rodríguez e C. Monterroso. "Phosphorus sorption of coal-mine soils in Galicia, NW Spain". In Plant-Soil Interactions at Low pH: Principles and Management, 125–28. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0221-6_17.

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Vangronsveld, J., A. Ruttens e H. Clijsters. "The Use of Cyclonic Ashes of Fluidized Bed Burning of Coal Mine Refuse for Long-Term Immobilization of Metals in Soils". In Biogeochemistry of Trace Elements in Coal and Coal Combustion Byproducts, 223–33. Boston, MA: Springer US, 1999. http://dx.doi.org/10.1007/978-1-4615-4155-4_13.

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Skousen, Jeff, W. Lee Daniels e Carl E. Zipper. "Soils on Appalachian Coal-Mined Lands". In Appalachia's Coal-Mined Landscapes, 85–109. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-57780-3_4.

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Barton, Christopher D., Kenton Sena, Teagan Dolan, Patrick Angel e Carl Zipper. "Restoring Forests on Surface Coal Mines in Appalachia". In Spoil to Soil, 123–45. Taylor & Francis Group 6000 Broken Sound Parkway NW, Suite 300 Boca Raton, FL 33487-2742: CRC Press, 2017. http://dx.doi.org/10.1201/9781351247337-12.

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Bhumbla, Devinder K., Rabindar N. Singh e Robert F. Keefer. "Effect of Rock Phosphate on Arsenic Uptake from Fly Ash Treated Mine Soil". In Biogeochemistry of Trace Elements in Coal and Coal Combustion Byproducts, 279–92. Boston, MA: Springer US, 1999. http://dx.doi.org/10.1007/978-1-4615-4155-4_18.

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Sloan, John J., e Don Cawthon. "Mine Soil Remediation Using Coal Ash and Compost Mixtures". In Chemistry of Trace Elements in Fly Ash, 309–18. Boston, MA: Springer US, 2003. http://dx.doi.org/10.1007/978-1-4757-4757-7_21.

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Li, XiaoLong, DuoXi Yao e JinXiang Yang. "Soil Environmental Quality Analysis and Evaluation of Coal Mine Reclamation Area". In Advances in Computer Science, Intelligent System and Environment, 701–4. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-23753-9_113.

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Lottermoser, Bernd, Ewald Schnug e Silvia Haneklaus. "Coca-Cola® for Determining Bioaccessible Uranium in Contaminated Mine Soils". In The New Uranium Mining Boom, 493–98. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-22122-4_57.

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Atti di convegni sul tema "Coal mine soils"

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Baumgartl, Thomas, J. Chan, F. Bucka e E. Pihlap. "Soil organic carbon in rehabilitated coal mine soils as an indicator for soil health". In 14th International Conference on Mine Closure. QMC Group, Ulaanbaatar, 2021. http://dx.doi.org/10.36487/acg_repo/2152_121.

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2

Keefer, Michael, Alison Kennedy, R. Moody e P. Gibeau. "Comparative inventory of vegetation and soils surrounding Teck Coal Ltd.’s coal mountain operations – 2010". In Sixth International Conference on Mine Closure. Australian Centre for Geomechanics, Perth, 2011. http://dx.doi.org/10.36487/acg_rep/1152_04_keefer.

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3

Spain, Alister, e Ian Hollingsworth. "Selected properties of the incipient soils developing on coal mining wastes, Bowen Basin, Australia". In Mine Closure 2016. Australian Centre for Geomechanics, Perth, 2016. http://dx.doi.org/10.36487/acg_rep/1608_11_spain.

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Paterson, D. G. "Mapping rehabilitated coal mine soils in South Africa using GPR". In 8th International Conference on Ground Penetrating Radar, a cura di David A. Noon, Glen F. Stickley e Dennis Longstaff. SPIE, 2000. http://dx.doi.org/10.1117/12.383580.

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Nie, Jinsuo, Jim Xu, Charles H. Hofmayer e Syed A. Ali. "An Approach for Assessing Structural Uplifting Using Blast Motions". In ASME 2008 Pressure Vessels and Piping Conference. ASMEDC, 2008. http://dx.doi.org/10.1115/pvp2008-61278.

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Abstract (sommario):
When a nuclear power plant (NPP) structure is subjected to beyond-design-basis seismic motions, a localized nonlinear effect on the soil-structure system is attributed to separations between the structure and the surrounding soils such as basemat uplift. Experiments involving field tests for real seismic events are usually difficult because of the low probability for large earthquakes at any particular site. To this end, the magnitudes of blast-induced ground motions at a coal mine have been found to be predicatable and can reach very large values. An approach has been developed to investigate whether the strong ground motions recorded at this coal mine can be used to evaluate the basemat uplift effect. This approach involves the use of a scaled ground motion to establish the relationship between the basemat uplift and the peak ground acceleration (PGA). This paper summarizes the field measurements for the ground motions at a coal mine by the Japan Nuclear Safety Organization (JNES) and a method using large scale finite element analyses for basemat uplift assessment performed by Brookhaven National Laboratory for the US Nuclear Regulatory Commission.
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Corcoran, Kyle, J. P. Gannon, J. P. Gannon, Thomas Martin, Thomas Martin, Jerry R. Miller e Jerry R. Miller. "BIOGEOCHEMICAL CHARACTERISTICS OF SUBSURFACE WATERS IN RECLAIMED SOILS AT PT BUKIT ASAM COAL MINE, SOUTH SUMATRA, INDONESIA". In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-312210.

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Tindal, Miles, David Brand, Ben Ludwig e Douglas Hackbarth. "Risk-based soil remediation guidelines in coal mine closure". In Sixth International Conference on Mine Closure. Australian Centre for Geomechanics, Perth, 2011. http://dx.doi.org/10.36487/acg_rep/1152_23_tindal.

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Wen, Bin, Jianwei Zhou e Liming Zhang. "Appropriate thickness and medium of covering soil on land reclamation in a coal mining subsidence area". In Mine Closure 2016. Australian Centre for Geomechanics, Perth, 2016. http://dx.doi.org/10.36487/acg_rep/1608_10_wen.

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Dickinson, Andrew, Richard Humphries, Mark Pawlett e Mark Tibbett. "Ecological and soil development of 19th Century iron and coal mine wastes at Bryn Defaid, South Wales". In Mine Closure 2016. Australian Centre for Geomechanics, Perth, 2016. http://dx.doi.org/10.36487/acg_rep/1608_12_dickinson.

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Paquin, Leo, e Curtis Brinker. "Soil salvage and placement – breaking new ground at Teck’s Cheviot open pit coal mine". In Sixth International Conference on Mine Closure. Australian Centre for Geomechanics, Perth, 2011. http://dx.doi.org/10.36487/acg_rep/1152_15_brinker.

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Rapporti di organizzazioni sul tema "Coal mine soils"

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Soil-water hydrology and geochemistry of a coal spoil at a reclaimed surface mine in Routt County, Colorado. US Geological Survey, 1988. http://dx.doi.org/10.3133/wri864350.

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