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21.
岳伟民  史新慧  黄玉文  翁炜  赵志涛 《探矿工程》2013,40(10):46-48,63
转子是螺杆钻具的核心部件,与定子相配合,决定了螺杆钻具的工作效率和动力性能。主要研究不同泥浆固相含量和添加剂对螺杆钻具转子表面磨损的影响,并设计了专用试验装置以模拟近井下条件工作时螺杆钻具转子的表面磨损情况,对其磨损规律开展研究,探索了转子在不同泥浆条件下的磨损规律,并结合相关磨损机理进行了进一步分析。初步发现了对硬铬镀层损伤较大的因素是泥浆固相与盐类添加剂,进而确定了硬铬镀层磨损的主要形式是腐蚀磨损,从而形成了对转子的制造工艺及使用方法的有益建议。  相似文献   
22.
In the present study,humic acid was used as an adsorbent for the investigation of the adsorption kinetics,isotherms,and thermo-dynamic parameters of hexavalent chromium from aqueous solution at varying pH,temperatures,and concentrations.Adsorption isotherms and equilibrium adsorption capacities were determined by the fittings of the experimental data to three well-known iso-therm models:Langmuir,Freundlich,and Redlich-Peterson.The results showed that the Langmuir and Redlich-Peterson models appear to fit the adsorption better than did the Freundlich adsorption model for the adsorption of chromium onto humic acid.The equilibrium constants were used to calculate thermodynamic parameters such as the change of free energy,enthalpy,and entropy.The derived adsorption constants (logaL) and their temperature dependencies from Langmuir isotherm have been used to calculate the corresponding thermodynamic quantities such as the free energy of adsorption,heat,and entropy of adsorption.The thermo-dynamic data indicate that Cr (VI) adsorption onto humic acid is entropically driven and characterized by physical adsorption.  相似文献   
23.
24.
刘平  杨军红 《岩矿测试》2008,27(1):33-36
使用可见光谱数字化自动分析系统对铁基合金中铬元素可见光谱进行了分析测定。研究了铁基合金中铬元素的Cr 520.60 nm和Cr 534.58 nm分析谱线组的特征,并制作了数字化彩色图谱。探索了铁基合金中铬元素的数字化分析技术,结果可用于铁基合金中铬元素的定性、定量分析和牌号鉴别。  相似文献   
25.
Cr(III) sorbed at the solid/water interface of latex and hectorite was studied by ESR spectroscopy in the presence of different inorganic ligands. The ESR spectra of the surface obtained in the presence of selenite, phosphate and fluoride can be explained in terms of ternary surface complex formation. This is contrasted by the behaviour of sulfate and selenate ions which were found to have no effect on the ligand field of Cr(III), either in the adsorbed state or in solution.  相似文献   
26.
本工作使用一次培养法初步研究了Cr(VI)对菱形硅藻和隐藻的毒性,实验结果表明,当Cr(VI)浓度大于16ppb时,则对其生长率产生抑制作用,其72小时EC_(50)值分别为260ppb和230ppb.根据活性点位模式计算了Cr(VI)与藻体的结合常数,约为2×10~5藻体中Cr含量与培养液中Cr浓度有关,两者近似指数关系,根据藻体中Cr含量和溶液中Cr的浓度,估计每个硅藻细胞与Cr最大结合容量约为5×10~(-17)mol/cell.  相似文献   
27.
甲壳素对Cr(Ⅵ)的吸附研究   总被引:1,自引:0,他引:1  
采用正交实验法 ,使用甲壳素 (粗制壳聚糖 ) ,研究温度、时间、吸附剂用量、酸度、盐效应对甲壳素吸附水中溶解的 Cr( )离子的吸附过程的影响 ,将实验结果进行极差分析 ,得到较优的吸附条件。实验结果表明 :在 p H =2、30℃、离子强度 5 mmol/ L的条件下 ,甲壳素对 Cr( )的最大吸附量为 13.1mg/ g。根据化学平衡及红外光谱分析结果表明 :甲壳素对 Cr( )的吸附主要是游离氨基静电吸附 Cr2 O2 -7,吸附符合 L angmuir吸附等温式  相似文献   
28.
One pre-requisite for the construction of a global chromium isotope mass balance is detailed understanding of Cr isotope systematics in the critical zone where redox-processes can modify the isotope signature of geogenic Cr input into the hydrosphere. A Cr isotope inventory of bedrock, soil, and runoff was performed in a Central European headwater catchment underlain by amphibolite, situated in the vicinity of two previously studied catchments underlain by different bedrock types (serpentinite and leucogranite). Fresh bedrock in the amphibolite catchment NAZ contained ~300 mg/kg Cr, serpentinite at PLB contained ~800 mg/kg Cr, and leucogranite at LYS contained ~2 mg/kg Cr. Monthly hydrochemical monitoring at all three sites revealed higher Cr(VI) export fluxes in winter than in summer. NAZ was characterized by a distinct seasonality in the δ53Cr values, with minima during winter/spring snowmelts (−0.35‰) and maxima during dry summers (0.40‰). Similar seasonality in δ53Cr values had been reported from PLB and LYS. Bedrock at all three sites had similar Cr isotope composition close to −0.10‰, a value indistinguishable from the δ53Cr value of bulk silicate Earth (BSE). Positive mean δ53Cr value of NAZ runoff indicated Cr-isotope fractionations during weathering of geogenic Cr(III), combined with adsorption of the resulting Cr(VI) on soil particles during pedogenesis. However, the mass-weighted mean δ53Cr of NAZ runoff was lower (−0.08‰), indistinguishable from the Cr isotope signature of bedrock. The same pattern of lower mass-weighted mean δ53Cr values of runoff, compared to arithmetic mean δ53Cr values of runoff, were observed also at PLB and LYS. We suggest that elevated Cr runoff fluxes in winter remove some of the residual isotopically light Cr that accumulated in the soil during summer. Seasonality in runoff δ53Cr values appears to be a relatively widespread phenomenon, de-coupled from Cr availability for chemical weathering.  相似文献   
29.
本文以CdCl_2·2.5H_2O为反应剂,采用“下垫上滴”缓冲刺的装样形式,通过大量镉盐的蒸发控制电极温度,使被测元素预先分馏,有效地改善了它们的蒸发行为,同时,减小了基体效应、光谱背景。本法其有良好的精密度和准确度,各元素的检出限(×10~(-5))分别为:Pb(1),Sn(0.37),Cr(1.8),Ni(3.51,Mo(0.1)和Co(0.38),其相对标准偏差(RSD)为±3.7—9.5%  相似文献   
30.
Sukinda chromite valley is one of the largest chromite deposits of the country and produces nearly 8% of chromite ore. It greatly contributes towards the economic development but at the same time deteriorates the natural environment. It is generally excavated by opencast mining method. In the Sukinda mining area, around 7.6 million tons of solid waste have been generated in the form of rejected minerals, overburden material/waste rock and sub-grade ore that may be resulting in environmental degradation, mainly causing lowering in the water table vis-à-vis deterioration in surface and ground water quality. The study conducted in and around one of the chromite mine of the valley reveals that the concentration of hexavalent chromium is found in the water samples of ground and surface water, mine effluents and seepage water. Hexavalent Chromium (Cr+6) have been found varying between 0.02 mg/l and 0.12 mg/l in mine effluents and 0.03–0.8 mg/l in shallow hand pumps and 0.05 and 1.22 mg/l in quarry seepage. The concentration of Cr+6 in Damsal nalah, the main surface water source in the area, is found varying between 0.03 mg/l and 0.14 mg/l and a increasing trend, which is in the downstream of mining activities, has been observed. Leachate study clearly shows that the soil lying in the vicinity of mine waste dump shows highest concentration of Cr+6. Contaminant migration in ground water depends upon various geohydrological conditions of the area. The study shows that aquifer resistivity varies between 15 Ωm to 150 Ωm and aquifer depth varies from 4 m to 26 m below ground level. The ground water flow and mass transport models were constructed with the help of geo-hydrological and geophysical informations using Visual Modflow software. Contaminant migration and path lines for 20 years have been predicted in two layers model of ground water. The study provided an insight into the likely migration of contaminant in ground water due to leaching from overburden dump of chromite ore and will be helpful in making strategic planning for limiting the contaminant migration in the ground water regime in and around the mining areas.  相似文献   
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