松散煤岩体钻封注耦合注浆锚固机理与试验研究

针对松散煤岩体巷道钻孔成孔困难、锚固力低的问题,提出了钻封注分次注浆时空耦合加固方法,实现了钻孔内“全长封孔+带压注浆”,分析了钻封注分次注浆加固技术原理,研发了自钻锚杆、封孔及加固注浆材料,其封孔材料具有膨胀性大、强度大和凝固时间快等特点,注浆加固材料具有速凝早强、流动性好、固结效果好及强度较高等优点。研究结果表明:全长封孔后带压注浆,浆液扩散半径大,钻封注锚杆锚固力相对于数脂锚固提高1倍以上,表明钻封注分次注浆加固技术具有较高的应用价值。     

乡镇居民点规模—功能系统耦合协调发展研究——以重庆市潼南区为例

借鉴耦合理论,建立了乡镇居民点规模-功能耦合系统,以潼南区为案例,采用熵权法、耦合协调度评价和空间集聚分析等方法,对2014年潼南区22个乡镇居民点规模-功能的耦合协调发展状态进行评价。研究发现,经济规模是乡镇居民点规模的主要决定因素。第三产业是影响居民点生产功能的主要因素,教育医疗则是影响生活功能的主要因素,建成区绿化面积是影响居民点生态功能的主要因素。潼南区乡镇居民点规模-功能耦合协调发展水平在空间上具有明显的单核结构特征,区域发展具有较大的不平衡性。大部分乡镇规模-功能耦合处于拮抗状态,规模滞后状态,规模、功能建设发展都处于低水平状态。应当积极培育县城以外的区域次级增长中心,以缩小区域发展的不平衡性。在村镇居民点的规划中,应重视居民点经济规模的地位与作用,以求更为合理的预测居民点规模,并规划建设居民点功能。     

安徽省经济发展与生态环境耦合协调评价与趋势预测

本文遵循客观、科学、综合原则,运用熵值赋权法,对经济与生态环境系统进行了评价;采用动态耦合模型及剪刀差分析方法对经济发展与生态环境系统耦合协调状况进行了考察;借助Excel 2003软件,通过作散点图,比较拟合优度分析方法,对两者的协调前景进行了预测。结果表明:①经济发展与生态环境系统综合指数分别由2005年的0.2934、0.4198跃升至2015年的0.6236、0.4198,经济发展系统升幅明显高于生态环境系统。②2005—2015年,经济发展与生态环境系统动态耦合度均值为-6.95°,整体处于由低级协调向协调演进状态,而两者间演化速度夹角由2005年的18.56°扩展至2015年的82.4°。③若按既有惯性发展模式,2020年经济发展与生态环境系统耦合度将达155.74°,预期处于极限发展状态。基于研究结果,本文提出了相应的应对策略,可为新常态下安徽省制定经济与生态文明融动发展政策提供决策参考。     

地下储液罐抗爆炸地冲击作用的流固耦合有限元分析

储液罐的抗震性能虽然得到了较为深入的研究,但对其抗爆炸产生的地冲击作用的研究还十分罕见。本文通过建立流固耦合的数值分析模型,研究爆炸地冲击作用下地下立式储液罐的动力特性,包括储液晃动波高、罐壁的应力和应变、底板的提离和浮放储液罐的"象足"变形产生原因及破坏机理等。研究结果表明,储液罐在爆炸地冲击荷载和地震荷载作用下的动力响应有明显区别,地震荷载作用下的储液罐抗震验算方法不适用于爆炸地冲击荷载。     

Analysis of Coupling between Soil and Water Conservation and Economic-social Development

The coupling relation exists in water and soil conservation and economic-social development. The article analyses the relation of soil and water conservation and economic-social development stages as well as the coupling analytical method. Then calculates the expecting income by dispersing Markov decision and calculates the correlation coefficient and the relationship degree. The article obtains the relationship of soil and water conservation investments and all kinds of incomes. Finally, it analyzes the important meaning in socio-economic development of water and soil conservation.     

热-力耦合作用对建筑结构火灾安全的影响

结构火灾安全可以避免建筑物在火灾中坍塌.火灾热环境影响建筑结构的响应,传统的标准火灾环境有一定的局限性,不能完全适用于若干真实火灾场景.因此有必要开展真实火灾环境下建筑结构的热-力响应特性研究,发展有效的工程工具来设计经济安全的结构.近来,性能化的结构火灾安全设计评估方法和相应技术发展迅速,该文给出一种综合考虑热-力耦合作用的结构火灾安全设计评估方法及相应流程.首先通过建筑和燃料特性来预测可能的火灾热环境特性,然后再分析构件和结构的热响应和力学响应特性来判定结构是否会失效,以及可以降低热和力影响的预防失效措施.该文通过案例分析将该方法应用于某中庭钢结构屋顶的防火保护,得到经济合理的防火涂层设计,满足有关防火规范的安全等价要求.     

Comparison of Field Performance of Multiple Soil Moisture Sensors in a Semi‐Arid Rangeland1

Abstract:  Automated electronic soil moisture sensors, such as time domain reflectometry (TDR) and capacitance probes are being used extensively to monitor and measure soil moisture in a variety of scientific and land management applications. These sensors are often used for a wide range of soil moisture applications such as drought forage prediction or validation of large‐scale remote sensing instruments. The convergence of three different research projects facilitated the evaluation and comparison of three commercially available electronic soil moisture probes under field application conditions. The sensors are all installed in shallow soil profiles in a well instrumented small semi‐arid shrub covered subwatershed in Southeastern Arizona. The sensors use either a TDR or a capacitance technique; both of which indirectly measure the soil dielectric constant to determine the soil moisture content. Sensors are evaluated over a range of conditions during three seasons comparing responses to natural wetting and drying sequences and using water balance and infiltration simulation models. Each of the sensors responded to the majority of precipitation events; however, they varied greatly in response time and magnitude from each other. Measured profile soil moisture storage compared better to water balance estimates when soil moisture in deeper layers was accounted for in the calculations. No distinct or consistent trend was detected when comparing the responses from the sensors or the infiltration model to individual precipitation events. The results underscore the need to understand how the sensors respond under field application and recognize the limitations of soil moisture sensors and the factors that can affect their accuracy in predicting soil moisture in situ.     

大气中二甲硫等氧化的化学耦合作用

从遥远海洋到重污染地区在很宽的大气条件下,用灵敏度分析法研究了二甲硫（DMS）和SO2的氧化机理及其化学耦合作用,DMS最重要的氧化机理是OH自由基的摘氢反应,对SO2是SO2与OH自由基的反应。在DMS和SO2的氧化过程中,碳、氮、氧化合物的化学耦合作用起着根本性的作用,重要的化学耦合反应是OH自由基的生成反应、消耗反应和NOx等的光化学引发反应等。     

黄河(内蒙古段)水体中沉积物的表面特征

运用表面络合原理,研究了内蒙古清水河县喇嘛湾黄河干流沉积物的表面特征.根据酸碱滴定求得沉积物的零电点pH(PZC),表面质子电荷密度σH及总吸附位NS,运用恒定容量模式求定了样品的表面固有酸度常数.研究表明,应用恒定容量模式研究天然水体沉积物的表面特征是可行的,在一定程度上能较好地吻合实验数据.     

REAL-TIME SOIL WATER MONITORING FOR OPTIMUM WATER MANAGEMENT1

Abstract: Efficient water resource management is one of the most important policy issues facing agriculture in Hawaii in the years ahead. Soil water sensors, multisensor capacitance probes (MCP), have been successfully used for different water management projects. These MCPs monitor water content at multiple depths and at various locations in real-time. The objectives of this study were to determine the effect of water content on field soil bulk density of Wahiawa silty clay tropical soil; measure field saturated hydraulic conductivity of this tropical soil: calibrate MCP system for this soil: and monitor and evaluate real-time soil water content variations under a tomato crop using the calibrated MCP system. Sensor calibration was conducted under laboratory conditions. Soil bulk density at different water contents and saturated hydraulic conductivity were measured on the field. Bulk density increased with increasing water content: there was a 30 percent bulk density increase as a result of 0.25 cm³ cm^-3 water content variation. Compared with the manufacturer's calibration, site specific laboratory calibration of MCP gave a more accurate determination of soil water. Field determined saturated hydraulic conductivity was higher than laboratory determined values reported in the literature for the same soil type. Real-time soil water content monitoring within the root zone showed substantial variations due to water input (irrigation and rainfall) and water output (evapotranspiration and deep percolations). However, water content variations were much further reduced in the soil layer below the root zone.