Spatial variability in soil water and salinity in Tamarix community in a semiarid saline region of the upper Yellow River北大核心CSCD

Tamarix is widely distributed in semiarid saline regions of the upper Yellow River. The community of Tamarix affects the spatial distribution of soil water and salinity. It is important to explore the dynamic response relationship of Tamarix community and spatial distribution of soil water and salinity in order to evaluate the effects of vegetation community construction and ecological restoration in this region. The natural Tamarix community in the secondary saline-alkali land of the Ningxia Yellow River Irrigation Area was investigated in July 2016. Classical statistics and geostatistics were used to analyze the spatial distribution characteristics of soil water and salinity. The results showed that the soil water content was relatively low (1.98%-7.55%), whereas the soil salinity was high (average conductivity 10.28-25.38 mS/cm) in the study area. The variability coefficient range of soil water and salinity was 36.1%-83.7%, both with moderate variations. Furthermore, the variation degree of soil salinity decreased with the increase in soil depth. The soil water and salinity had obvious spatial structure characteristics, which was mainly affected by structural factors or structural factors associated with stochastic factors. The coefficients of nugget were 0.04%-49.88%, indicating the strong spatial correlation. The spatial distribution of soil water and salinity in Tamarix community showed a patchy pattern; the soil water and salinity distribution in the areas with high Tamarix growing density were considerably high. The correlation analysis showed that there was a positive correlation between soil water and salinity in the study area. In conclusion, soil water and salinity restrict the distribution and growth of Tamarix. Furthermore, the distribution and growth of Tamarix enhanced the spatial variability of soil water and salinity. Keywords. © 2018 Science Press. All rights reserved.     

复杂地质低渗煤层水力压裂-割缝综合瓦斯增透技术研究

针对水力压裂区域化瓦斯增透盲区,提出了水力割缝局部化瓦斯增透技术措施,形成了复杂地质低渗煤层水力压裂-割缝综合瓦斯增透技术,并进行现场验证。研究结果表明:水力压裂区内的3个压裂钻孔平均瓦斯抽采纯流量较238底板道常规抽采钻孔单孔瓦斯抽采纯流量提高15.8倍,瓦斯抽采浓度提高4%,压裂区瓦斯抽采纯流量较对比区提高2.1倍,但水力压裂区域性措施受断层及煤层硬度等地质条件限制,存在盲区;水力割缝增透区内的抽采钻孔瓦斯浓度平均提高4.9倍,瓦斯纯流量平均提高3.3倍,对不同地质条件的适应性强,但是割缝影响范围小,抽采时效短;复杂地质低渗煤层水力压裂-割缝综合瓦斯增透技术综合了水力压裂与割缝的优点,对复杂地质煤层具有较强适应性,大幅提高了瓦斯治理水平。现场验证结果表明复杂地质低渗煤层水力压裂-割缝综合瓦斯增透技术在复杂地质条件下煤层强化抽采中有较好的实际应用价值。     

基于Box Behnken设计的煤导热系数分析与预测

为研究分析水分、固定碳及密度3个因素对煤导热系数的影响,选取多个矿井不同煤质的煤作为实验煤样,使用NETZSCH LFA457型激光导热系数测试仪进行测定,并引入二次响应曲面试验设计思想,采用Design Expert软件进行煤质指标的Box Behnken试验设计,按设计表筛选实验数据,构建了导热系数多因素、多水平影响下二次回归响应曲面模型,并对不同采样地点的煤导热系数进行了分析与预测。结果表明:二次回归方程P值小于0.000 1,极显著,失拟项为0.072 4,不显著,回归方程具有统计学意义;当水分在0.9%~10.9%,固定碳在49.3%~83.6%,密度在1.2~1.92 g·cm³之间,对煤的导热系数一次项影响程度为密度>固定碳>水分;二次项影响程度为固定碳和密度>水分和密度>水分和固定碳,且固定碳和密度之间存在交互作用,水分和密度、水分和固定碳之间无交互作用;应用响应曲面模型预测的煤导热系数误差为4.3%,满足精度要求。     

发泡注浆法合成莫来石轻质耐火材料

以工业废弃物粉煤灰和当地粘土为主要原料,十二烷基苯磺酸钠为发泡剂,采用发泡注浆法制备轻质莫来石耐火材料,研究了烧结温度对耐火材料晶相的影响以及发泡剂的种类、添加量和浆料固含量对轻质耐火材料常温物理性能的影响。结果表明,适当的烧结温度可改善耐火材料的晶相,同时对制品的孔隙率也有一定影响。选择适宜的发泡剂及添加量,在一定的浆料固含量范围内,可以制备容重小,孔隙率高,导热系数小,机械强度适中的轻质耐火材料。     

Reach‐Scale Geomorphic and Biological Effects of Localized Streambank Armoring

Armoring of streambanks is a common management response to perceived threats to adjacent infrastructure from flooding or erosion. Despite their pervasiveness, effects of reach‐scale bank armoring have received less attention than those of channelization or watershed‐scale hydromodification. In this study, we explored mechanistic ecosystem responses to armoring by comparing conditions upstream, within, and downstream of six stream reaches with bank armoring in Southern California. Assessments were based on four common stream‐channel assessment methods: (1) traditional geomorphic measures, (2) the California Rapid Assessment Method for wetlands, (3) bioassessment with benthic macroinvertebrates, and (4) bioassessment with stream algae. Although physical responses varied among stream types (mountain, transitional, and lowland), armored segments generally had lower slopes, more and deeper pools and fewer riffles, and increased sediment deposition. Several armored segments exhibited channel incision and bank toe failure. All classes of biological indicators showed subtle, mechanistic responses to physical changes. However, extreme heterogeneity among sites, the presence of catchment‐scale disturbances, and low sample size made it difficult to ascribe observed patterns solely to channel armoring. The data suggest that species‐level or functional group‐level metrics may be more sensitive tools than integrative indices of biotic integrity to local‐scale effects.     

吸能让位防冲支护结构与围岩协同作用体系研究*

为防治冲击地压危害,减小人员伤亡与经济损失,采用数值计算方法建立吸能让位防冲液压支架与围岩协同作用体系模型,计算支架和围岩组合体系在静载和冲击载荷作用下的受力状态。结果表明:静载条件下,受煤层影响巷道右侧拱肩位置应力值与塑性应变相对最大,此处最易发生破坏;吸能装置在静载条件下没有发生压缩变形,表明吸能装置不会影响支架正常工作;竖向冲击荷载条件下,受煤层结构影响巷道右侧拱肩处等效塑性应变值增大相对比较明显,吸能防冲支架中间液压柱与右侧液压柱水平位移变化相对最明显;冲击地压发生过程中,支架与围岩间相互作用力变化较大,总体可分为振动段、平稳段、上升段、波动段4个阶段。     

综合防尘技术在开元公司的应用

主要介绍了采煤机高压引射降尘系统、液压支架自动喷雾、粉尘浓度在线检测超限自动喷雾等综合防尘技术在开元公司矿井中的应用。通过对降尘系统效果监测和分析,降尘效率达到84．1％,降尘效果明显,改善了作业场所的劳动卫生条件。     

液压爬模在泰州大桥南塔施工中的安全控制

液压爬模具备自动爬升、操作简便、作业人员少、施工效率高、外观质量好等优点,其施工工艺和技术也比较成熟,在不少大中型工程建设项目中得到广泛应用。液压爬模的操作平台和爬升系统为一整体,液压驱动装置能实现整体均匀爬升,其安全性能有了明显提高。但液压爬模结构复杂且体积庞大,其安装、调位和脱模以及模板的收分等操作和使用环节的安全风险很大,容易出现模板坍塌、高处坠落、物体打击等事故,是施工中安全控制的重点。泰州大桥南塔工程引进了液压自动爬模系统来进行塔身浇注施工,施工中的安全控制措施取得了良好的效果。本研究将以泰州大桥南塔工程为背景,对液压爬模在塔柱施工过程中的危害因素进行分析并提出相应的控制措施,可供类似工程借鉴。     

Viscosities, thermal conductivities and diffusion coefficients of CO2 mixtures: Review of experimental data and theoretical models

Accurate experimental data on the thermo-physical properties of CO₂-mixtures are pre-requisites for development of more accurate models and hence, more precise design of CO₂ capture and storage (CCS) processes. A literature survey was conducted on both the available experimental data and the theoretical models associated with the transport properties of CO₂-mixtures within the operation windows of CCS. Gaps were identified between the available knowledge and requirements of the system design and operation. For the experimental gas-phase measurements, there are no available data about any transport properties of CO₂/H₂S, CO₂/COS and CO₂/NH₃; and except for CO₂/H₂O(/NaCl) and CO₂/amine/H₂O mixtures, there are no available measurements regarding the transport properties of any liquid-phase mixtures. In the prediction of gas-phase viscosities using Chapman–Enskog theory, deviations are typically <2% at atmospheric pressure and moderate temperatures. The deviations increase with increasing temperatures and pressures. Using both the Rigorous Kinetic Theory (RKT) and empirical models in the prediction of gas-phase thermal conductivities, typical deviations are 2.2–9%. Comparison of popular empirical models for estimation of gas-phase diffusion coefficients with newer experimental data for CO₂/H₂O shows deviations of up to 20%. For many mixtures relevant for CCS, the diffusion coefficient models based on the RKT show predictions within the experimental uncertainty. Typical reported deviations of the CO₂/H₂O system using empirical models are below 3% for the viscosity and the thermal conductivity and between 5 and 20% for the diffusion coefficients. The research community knows little about the effect of other impurities in liquid CO₂ than water, and this is an important area to focus in future work.     

水力割缝增透抽采煤层瓦斯原理及应用

煤层瓦斯抽采是避免煤矿瓦斯灾害发生的根本防治措施,水力割缝技术使煤体在割缝后应力松弛、卸压、破坏、破裂,以成倍或者十几倍地提高煤层的渗透性,继而对煤层瓦斯进行抽采,使瓦斯煤层变为低瓦斯或无瓦斯煤层,从根本上避免瓦斯灾害发生。从水力割缝技术切割煤层致煤层应力变化角度,将理论分析和数值模拟方法相结合,根据渗流力学平面径向流理论,分析给出水力割缝技术增透抽采瓦斯原理。以兖州东滩矿3号煤层为例,分析采用水力割缝技术前后煤层应力变化、渗透率变化规律。结果表明:大面积割缝后,应力重新分布,由均匀状态转变为非均匀状态分布,水平缝使煤层卸压,煤层应力普遍降低,在缝上部煤层局部形成拉应力区。割缝后渗透率是割缝前的4.34倍,渗透率大幅度增加,从而提高瓦斯抽采速度和最终抽采率。