Further explanation of the sampling and testing procedures is included in Section 8.2.2. The most important rock mechanic properties obtained from these two lithology groups for stability analysis are summarized in Table 7-3 below. The clays include such rocks as lean clay, clayey ‐ sandstone, clayey ‐ siltstone and claystone, whereas the sands include siltstone, silty ‐ claystone, sandy siltstone, and sandstone. The results from this testing program show that lithology at NARM can be grouped into two broad classes from a strength standpoint: clays and sands. The rock testing program is designed to obtain the rock strength parameters for all major rock types encountered at NARM and the results are used for highwall stability analysis. ![]() These holes are spaced across the property to provide a comprehensive representation over the entire area. There are currently 59 geotechnical overburden cored locations completed as of December 31, 2021. Outside the fracture zone, the coal often does not yield enough water to be classified as an aquifer.Ī comprehensive rock mechanics testing program has been established at NARM. However, there are no stock or domestic wells completed in the coal in and adjacent to the permit area. In the fracture zone, the coal is classified as an aquifer. Coal seam hydraulic conductivity is higher in the area north of Porcupine Creek and Knapp Draw. The Porcupine Creek lineament (Denson, et al., 1978) is inferred to be a fracture system along Porcupine Creek Valley. Well yields in coal aquifers can range from zero in unfractured areas to greater than 100 GPM in highly fractured areas (Hodson, et al., 1973). Secondary permeability is dependent on fracturing and jointing in the coal, and the degree of fracturing and resulting permeability can vary greatly. Typically, the primary permeability for coal is low and secondary permeability controls the flow of groundwater. The Wyodak-Anderson coal seam is itself a low yield unit. (1981) postulate that this extensive and thick coal seam originated in a paludal subsystem of the Powder River intermountain basinal fluvial system. The main aquifer of the upper Fort Union is the Wyodak-Anderson coal seam, also locally referred to as the Roland coal seam. There are no known faults within the controlled coal area. The WA in the northern half and the WA1/WA2 in the southwest are the only seams mined at NARM. The rider seams are not mined due to poor quality. They are quite consistent throughout the eastern portions of the lease but become more sporadic west of the splitline. In conclusion, several thin rider seams (1-4 feet in thickness) occur within the overburden. Structurally, the WA2 seam remains relatively flat, whereas the WA1 rides up over the parting and has a dipping structure. The midburden between the WA1 and WA2 increases to a maximum of 120 ft thick. The WA splits into two nearly equally thick (30-35 ft) mineable seams: WA1 (upper split) and WA2 (lower split). The second geologic feature is a ribbon split occuring in the southwest portion of the lease and trending northwest to the southeast. The mineable WA coal thickness averages 80 feet in the west and 60 feet east of the monocline. ![]() The LWA seam is not mined because of poor quality and an increasingly high strip ratio. The lower 12-14 feet of the WA seam splits off as a hanger seam (Lower Wyodak-Anderson, or LWA) and has a steeply dipping gradient after it splits. ![]() The first is a monocline that exists in a northwest to southeast trend over the middle portion of the mine. ![]() There are two main geologic features at NARM. The coal is thickest on the northwest side of the lease. The WA seam is in the uppermost section of the Paleocene Fort Union Formation. The remaining coal is 50-87 ft thick and 180 to 460 ft deep within the leased area. Coal has been mined exclusively from the Wyodak-Anderson (WA) Seam. The Wasatch consists of alternating, lenticular deposits of sandstones, siltstones, claystones, coal, and carbonaceous shales. The Wasatch Formation and local Quaternary age deposits comprise all of the overburden lithologies at the mine site. National Pollution Discharge Elimination System American Society of the International Association for Testing and Materials
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RDBMS and MySQL are often thought to be the same because of MySQL’s popularity. MySQL is one of many RDBMS software options. Whenever they need to access data, they connect to the RDBMS server. Client-server modelĬomputers that install and run RDBMS software are called clients. The commercially licensed version is available if you need more flexible ownership and advanced support. However, The GPL ( GNU Public License) determines what you can do depending on conditions. You can also learn and customize the source code to better accommodate your needs. Open source means that you’re free to use and modify it. If the software doesn’t support the relational data model, just call it DBMS. The word “relational” means that the data stored in the dataset is organized as tables. A database is a place in which data is stored and organized. Your photo is data, and your phone’s gallery is the database. Think of taking a selfie: you push a button and capture an image of yourself. 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