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731.
山区高速公路挖方边坡的稳定性评价与安全防护技术 总被引:3,自引:3,他引:3
山区高速公路挖方边坡的稳定性对道路交通安全具有重要影响 ,阐述了进行挖方边坡的稳定性评价和安全防护的必要性 ,提出了评价原则、工作程序、评价方法及系列安全防护技术。得出了关于山区高速公路挖方边坡的稳定性评价和安全防护的几点认识。 相似文献
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733.
关于污水处理厂质量监理工作的探讨 总被引:2,自引:0,他引:2
污水处理已引起我国政府的高度重视。以此为契机,通过对阳江市第一净水厂工程监理工作的回顾,初步探讨了污水处理厂质量监理工作。 相似文献
734.
高炉料仓环境条件恶劣,而高炉生产又要掌握料位情况。比较了2种料位计,最终选择了SA—2型料位计。 相似文献
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736.
开展企业安全评价势在必行 总被引:2,自引:0,他引:2
安全评价是以实现工程、系统安全为目的。应用安全系统工程原理和方法,对危险和有害因素进行辨识与分析,判断发生事故和职业危害的可能性及其严重程度,从而为制定防范措施和管理决策提供科学依据。本文从六个方面阐述了企业开展安全评价的必要性。 相似文献
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739.
Ian H. McBeth Katta J. Reddy Quentin D. Skinner 《Journal of the American Water Resources Association》2003,39(3):575-585
ABSTRACT: The Powder River Basin in Wyoming has become one of the most active areas of coalbed methane (CBM) development in the western United States. Extraction of methane from coalbeds requires pumping of aquifer water, which is called product water. Two to ten extraction wells are manifolded into one discharge point and product water is released into nearby unlined holding ponds. The objective of this study was to evaluate the chemistry, salinity, and sodicity of CBM product water at discharge points and associated holding ponds as a function of watershed. The product water samples from the discharge points and associated holding ponds were collected from the Cheyenne River (CHR), Belle Fourche River (BFR), and Little Powder River (LPR) watersheds during the summers of 1999 and 2000. These samples were analyzed for pH, electrical conductivity (EC), total dissolved solids (TDS), alkalinity, sodium (Na), calcium (Ca), magnesium (Mg), potassium (K), sulfate (SO42‐), and chloride (C1‐). From the chemical data, practical sodium adsorption ratio (SARp) and true sodium adsorption ratio (SARt) were calculated for the CBM discharge water and pond water. The pH, EC, TDS, alkalinity, Na, Ca, Mg, K, SARp, and SARt of CBM discharge water increased significantly moving north from the CHR watershed to the LPR watershed. CBM discharge water in associated holding ponds showed significant increases in EC, TDS, alkalinity, Na, K, SARp, and SARt moving north from the CHR to the LPR watershed. Within watersheds, the only significant change was an increase in pH from 7.21 to 8.26 between discharge points and holding ponds in the LPR watershed. However, the LPR and BFR exhibited larger changes in mean chemistry values in pH, salinity (EC, TDS), and sodicity (SAR) between CBM product water discharges and associated holding ponds than the CHR watershed. For instance, the mean EC and TDS of CBM product water in LPR increased from 1.93 to 2.09 dS/m, and froml,232 to 1,336 mg/L, respectively, between discharge and pond waters. The CHR exhibited no change in EC, TDS, Na, or SAR between discharge water and pond water. Also, while not statistically significant, mean alkalinity of CBM product water in BFR and LPR watersheds decreased from 9.81 to 8.01 meq/L and from 19.87 to 18.14 meq/L, respectively, between discharge and pond waters. The results of this study suggest that release of CBM product water onto the rangelands of BFR and LPR watersheds may precipitate calcium carbonate (CaCO3) in soils, which in turn may decrease infiltration and increase runoff and erosion. Thus, use of CBM product water for irrigation in LPR and BFR watersheds may require careful planning based on water pH, EC, alkalinity, Na, and SAR, as well as local soil physical and chemical properties. 相似文献
740.
Marty D. Matlock Kevin Ray Kasprzak G. Scott Osborn 《Journal of the American Water Resources Association》2003,39(2):267-275
ABSTRACT: The lower reaches of the Arroyo Colorado have historically failed to meet their use under subsection 303(b) of the U.S. Clean Water Act due to fecal coliform bacteria and low dissolved oxygen (DO). Fish kills, especially at the tidal confluence at the Port of Harlingen, Texas, have been reported. Oxygen demand from sediment (SOD) for a river typically has two states‐diffusion limited SOD (SOD) and potential SOD (pSOD), expressed when sediment is resuspended through increased flow or other disturbances. The objective of this research was to measure SOD in the Arroyo Colorado River in situ, estimate pSOD ex situ, and evaluate the relationship between SOD and the depositional environment. We measured SOD and pSOD in the Arroyo Colorado River at up to eight sites over three sampling events. We identified the sample sites based on a modified Rosgen geomorphic index for streambed stabilization. Sites with high sediment deposition potential had high SOD. The average values of SOD between sites were 0.62 g/m2/day (standard deviation 0.38 g/m2/day) and ranged from 0.13 to 1.2 g/m2/day. Potential SOD values ranged from as low as 19.2 to as high as 2,779 g/m3 sediment/ day. Potential SOD can serve as an indicator of the possible impact of SOD from resuspended sediment in stream systems. 相似文献