煤矿高浓度胶结充填系统可靠性评价研究

煤矿充填系统可靠性受多种不确定因素影响.通过对影响东庞矿高浓度胶结充填系统可靠性主要因素的分析,综合考虑各因素随机性、模糊性特点,利用层次分析法(AHP)建立充填系统可靠性模糊综合评价模型并确定各指标因素权重,运用模糊数学理论确定隶属矩阵和模糊综合评价法得到充填系统可靠性综合评判向量,按照最大隶属度原则确定此充填系统可靠性为“较稳定”等级.经充填工业性试验开采验证,系统可靠性模糊评价模型的建立是合理有效、结果符合实际情况的.     

矿井避难硐室供氧系统研究

在矿山井下事故发生后的矿工自救中,设置避难硐室是十分必要的.供氧系统是避难硐室内避难人员生存的重要保障,避难硐室具有容载人数多、空间相对较大的特点.针对国内避难硐室采用的地面钻孔供氧、压风供氧、压缩气瓶供氧、化学氧供氧等供氧方式进行了研究,分别通过基本供风量、供氧量等参数的理论计算方法,密闭空间模拟试验的方法来对几种供氧方式进行比较,最终确定避难硐室设置多种供氧方式的必要性,为今后避难硐室供氧系统的构建奠定基础.     

中国地表水酸化敏感性的区划

地表水体的酸化与集水区的许多环境因子密切相关,如土壤对酸的缓冲能力、基岩中和酸沉降的能力以及土地利用方式等.其中,土壤的抗酸化能力是关键因素.因此可以根据集水区土壤、基岩和土地利用方式等信息来评估地表水在不同流量下发生酸化的可能性.本研究成功地应用已有资料和数据得到了我国地表水对酸沉降的敏感性等级,并绘制了地表水酸化敏感性区划图.结果表明,我国大部分地表水对酸化并不敏感.极易酸化和较易酸化的地表水主要分布在东北的北部地区,占所有国土面积的2.67%,是该地区强酸性漂灰土、酸性母岩和针叶林植被共同作用的结果.对酸化敏感性为中级和低级,即不易酸化的地表水主要分布在东北暗棕壤地区和南方富铝土区域,占所有国土面积的15.2%.其余82.11%国土面积上的地表水对酸化不敏感,完全不可能发生酸化.北方地区主要是由于土壤的强缓冲能力,而在南方,石灰质土壤以及耕作农田的广泛分布是最重要因素.南方重酸雨区由于土壤对酸化并不很敏感,因此在短期内不会出现大面积水体酸化现象.由于东北近年来频频出现酸雨,因此东北的酸沉降必须及早防治,以免出现大面积酸化水体.     

应用动态模型确定酸沉降临界负荷的探讨

任何一个天然生态系统都是一个稳定系统.在一定酸沉降量的作用下,生态系统最终会平衡在一个新的稳定状态.动态模型可以模拟不同酸沉降量下生态系统化学状态的变化趋势.根据信号与系统理论,这种趋势可以用一阶指数衰减函数进行模拟,以得到系统达到稳定状态时的化学指标值.根据不同酸沉降量和所对应的稳态化学指标值之间的剂量-响应曲线,可以求出当系统稳态化学指标值达到临界化学值时的酸沉降量,即为系统的酸沉降临界负荷.应用这种方法,以MAGIC模型为例,计算了四川峨眉山顶水和重庆南山湖泊的硫沉降临界负荷,分别为1.54和6.5     

基于高通量分析方法的长江干流重庆段抗生素种类特征及来源初探

采用高通量分析方法对长江干流重庆段11个流域断面、2个市政污水处理厂进水和6个养殖场废水的潜在抗生素进行筛查,并结合抗生素使用调查探讨其来源。结果表明,(1)共检出83种抗生素,其中流域内检出36种,污水处理厂和养殖场废水中检出70种;磺胺间甲氧嘧啶检出率最高,在流域水体和废水的检出率分别为91%和55%,喹诺酮类是检出抗生素的主要类型;(2)长江干流重庆段下游检出抗生素数量高于上游检出抗生素;(3)有20种抗生素可能由上游携带和重庆市内排放2种方式进入流域,7种抗生素可能由上游携带入境,9种抗生素可能由重庆市内排放引入长江。     

液化侧扩流场地桩基动力反应振动台试验数值模拟

针对已完成的振动台试验,采用OpenSees数值模拟计算平台,建立液化侧扩流场地群桩振动台试验数值模型。该模型中,采用线弹性梁柱单元模拟桩和挡墙,采用刚性连接单元和零长度单元模拟桩-土界面。自由水体通过施加节点孔压和节点力模拟。引入多屈服面塑性本构模拟饱和砂层,采用两相完全耦合的u—p形式模拟土体位移和孔压。通过对比振动台试验结果表明,建立的有限元数值模型能够可靠地再现砂层和桩基的动力响应,进而验证数值模型的可靠性。同时,针对两个代表性时刻,分析了桩-土体系的侧向变形响应。所采用的分析方法和相关结论也为同类桩-土体系数值模拟提供一般性分析方法和思路。     

缓倾斜煤层孤岛工作面巷道底鼓机制及控制

针对缓倾斜煤层孤岛工作面回采巷道底鼓严重的状况,以庞庞塔矿5煤107工作面运输顺槽为研究背景,测试了顶底板的矿物成分、微观结构,利用物理模拟研究了底鼓机制,结果表明:①107工作面运输顺槽底板以高岭石为主,膨胀性岩石成分较低,岩石内部空隙较少,结构致密,强度高;②107工作面运输顺槽底鼓属于挤压流动性底鼓,掘进期间发生的是浅部岩层整体弯曲,在采动超前支承压力影响阶段,底板上位坚硬岩层超过其抗弯强度而发生破断,下位软弱底板解除约束,变形急剧增加,帮角出现裂隙,底板变形出现剧烈变形区、受限变形区、变形过渡区;③107工作面运输顺槽底鼓机制为:坚硬底板在高应力下的挤压流动是造成底鼓的主要原因,缓倾斜煤层巷道底板存在三角煤和底板岩石中存在少量膨胀性岩石对底鼓影响较小。针对性提出了采用开挖卸压槽释放压力方式进行底鼓治理,现场实测表明所提措施可有效降低巷道底鼓量。     

Propagation characteristics of subaerial landslide-generated impulse waves

Environmental Fluid Mechanics - Subaerial landslide-generated impulse waves were investigated in a rectangular prismatic channel based on the Froude similarity criterion. Landslides were modeled...     

Reaction mechanism of arsenic capture by a calcium-based sorbent during the combustion of arsenic-contaminated biomass: A pilot-scale experience

Pilot-scale combustion is required to treat arsenic-enriched biomass in China. CaO addition to arsenic-enriched biomass reduces arsenic emission. CaO captures arsenic via chemical adsorption to form Ca₃(AsO₄)₂. Large quantities of contaminated biomass due to phytoremediation were disposed through combustion in low-income rural regions of China. This process provided a solution to reduce waste volume and disposal cost. Pilot-scale combustion trials were conducted for in site disposal at phytoremediation sites. The reaction mechanism of arsenic capture during pilot-scale combustion should be determined to control the arsenic emission in flue gas. This study investigated three Pteris vittata L. biomass with a disposal capacity of 600 kg/d and different arsenic concentrations from three sites in China. The arsenic concentration in flue gas was greater than that of the national standard in the trial with no emission control, and the arsenic concentration in biomass was 486 mg/kg. CaO addition notably reduced arsenic emission in flue gas, and absorption was efficient when CaO was mixed with biomass at 10% of the total weight. For the trial with 10% CaO addition, arsenic recovery from ash reached 76%, which is an ~8-fold increase compared with the control. Synchrotron radiation analysis confirmed that calcium arsenate is the dominant reaction product.     

Temporal trends in agricultural water use and the relationships to hydroclimatic factors in the High Plains aquifer region

The High Plains aquifer (HPA) is the primary water source for agricultural irrigation in the US Great Plains. The water levels in many locations of the aquifer have declined steadily over the past several decades because the rate of water withdrawals exceeds recharge, which has been a serious concern to the water resources management in the region. We evaluated temporal trends and variations in agricultural water use and hydroclimatic variables including precipitation, air temperature, reference evapotranspiration, runoff, groundwater level, and terrestrial water storage across the HPA region for different periods from 1985 to 2020 at the grid, county, or region scale. The results showed that water withdrawals decreased from 21.3 km³/year in 1985 to 18.2 km³/year in 2015, while irrigated croplands increased from 71,928 km² in 1985 to 78,464 km² in 2015 in the entire HPA. The hydroclimatic time-series showed wetting trends in most of the northern HPA, but drying and warming trends in the southern region from 1985 to 2020. The groundwater level time-series indicated flat trends in the north, but significant declining in the central and southern HPA. Trends in irrigation water withdrawals and irrigation area across the HPA were controlled by the advancement of irrigation systems and technologies and the management of sustainable water use, but also were affected by dynamical changes in the hydroclimatic conditions.