掘进巷道过断层漏顶区域的施工工艺研究

清水营煤矿岩体节理与裂隙发育,富水性较好,属于典型的＂三软＂煤层。工作面推进过程中顶板易碎、易冒;煤层开采中,软岩巷道稳定性控制与支护问题,严重制约了该矿井的安全生产。该矿在掘进巷道过断层时,发生突发性漏顶事故,致使巷道停掘。在分析了研究区岩性、构造、地球物理特征以及煤岩的物理力学参数的基础上,针对现场地质条件变化先后采取了两套施工方案对漏顶区进行加固。最终依靠方案二获得了成功,即采用对掘进迎头冒顶区采用水泥、水玻璃浆液加固冒顶区,并对冒空区采用马丽散泡沫充填。施工完成后从迎头退后36m起底,由冒顶区下部通过。现场实践证明,方案二具备安全性与经济性,可为＂三软＂条件下的巷道开采系统设计、岩层控制、安全回采提供地质保障与技术支持。     

济东煤田埠村煤矿瓦斯涌出量研究

煤矿瓦斯不仅关系到能否起到利用价值,同时也关系到众多矿工的安全问题,鲁中地区是山东重要的煤炭资源基地,埠村煤矿作为其中重要的一部分,其瓦斯研究价值不言而喻。运用沉积学、构造地质学、煤地质学,数学分析等相关学科和方法,从影响瓦斯涌出量的地质构造、顶底板岩性、岩浆岩、水文地质条件、上覆基岩厚度等地质因素进行综合分析,对埠村煤矿瓦斯涌出量进行量化预测,并作出其全井田瓦斯涌出量的等值线图。研究表明,埠村井田属低瓦斯矿井,瓦斯涌出量存在东高西低的趋势,主要受埠村向斜的控制,矿井瓦斯涌出量的预测分析可以对以后生产防治作出指导作用。     

建立留地安置制度是莱芜市“城中村”用地管理的有效途径

“城中村”是指位于城市规划区范围内、仍然保持村级建制的区域(包括以村为主改建的居委会)。“城中村”用地管理难,是多年来困扰各地土地管理工作的一个重要问题。如何加快“城中村”经济发展,维护“城中村”合法权益,规范“城中村”用地管理,是各级政府普遍关注的重大课题。笔者通过对莱芜地区“城中村”用地管理情况进行调查分析,认为建立“城中村”留地安置制度,是解决莱芜市“城中村”用地管理难,促进“城中村”经济发展、加快城市化进程、构建城市和谐的有效途径。1城中村留地安置制度的基本内容1.1总体思路根据留地安置指标和各“城…     

基于元模式的空间关联规则挖掘方法

空间关联规则可以从空间数据库中发现空间对象之间的隐含的、不明确的空间关系。空间数据库中空间关联规则挖掘研究是空间数据挖掘和知识发现(SDMKD)的主要内容,其主要问题是多层,多关系的规则发现问题。本文把元模式与空间关联规则挖掘相结合介绍了挖掘地理信息系统(GIS)中空间数据库关联规则的常用步骤方法。     

Features of climate change and their effects on glacier snow melting in Xinjiang,China

The features of climate change and their effects on glacier snow melting in the past 50 years (1961–2010) in Xinjiang were studied. Regional climate data for 49 meteorological stations in the Tianshan Mountains and the northern and southern areas of Xinjiang were collected with the aid of techniques such as climatological statistical diagnosis, regional climate models, remote sensing, and geographic information system. The annual average temperature displayed a rising trend across the Tianshan mountainous area and both areas of Xinjiang. The trend was particularly apparent in winter and autumn with the rate of increase in the annual average minimum temperature being significantly higher than that of the maximum temperature. Rainfall also tended to increase in all three areas over the 50-year period, with the magnitude of change being highest in the mountainous area followed by northern Xinjiang and then southern Xinjiang. As a result of the rising temperatures, there was a negative material balance among the region's glaciers, of which the year 1982/1983 was the key year for the development of Tianshan mountain glacier snow. After this date, glacial ablation intensified with an annual change increase in average temperature of 1 °C, leading to a glacier material balance change of about 300 mm. To establish rainfall and temperature sequences for three regional climate change scenarios in the 2011–2050 period, we adopted the delta method using actual measurements during the 1961–2000 period against corrected data from rainfall and temperature simulations. All three scenarios indicated that temperatures will continue to increase, that the increase in rainfall may decrease in mountainous regions but will increase in the basin, and that the speed of glacial ablation in Xinjiang will continue to accelerate.     

典型盆地煤与油页岩共生成矿物质及古气候分析

选取煤与油页岩共生典型盆地山东黄县盆地、辽宁抚顺盆地、黑龙江依兰盆地和内蒙古金宝屯盆地,综合分析了其成矿物质特点,认为共生背景下煤岩中的低等动植物和油页岩中的高等植物均比单一矿种下含量高。这一规律可用于勘探、开发煤或油页岩单一矿种时预测其共生矿种存在的可能性。对古气候的分析表明,气候变换在一定程度上制约着煤与油页岩的共生模式,这种共生模式可为古气候研究提供一定依据,反之,通过古气候的变迁也可帮助勘探、开发共生背景下的煤与油页岩。     

Aerodynamic roughness length of sandy beds and gravel beds

A physical model was developed for the aerodynamic roughness length of gravel beds and sandy beds under different atmospheric stability conditions based on Monin?CObukhov similarity theory and dimensional analysis. The relationship between the roughness length, the properties of the roughness elements, the characteristics of the airflow, and an atmospheric stability parameter (the bulk Richardson number) was then studied using the model. Results showed that the roughness length was not only functions of the shape, height, and coverage of the roughness elements and of the airflow, but also dependent upon atmospheric stability. These results were in agreement with results from wind tunnel experiments and field observations.     

濮阳小震集中区发震机理分析与讨论

综合小震精定位和震源机制解两方面的结果,对濮阳小震集中区小震丛集活动的发震机理进行了分析.双差定位结果显示,大部分地震震源位于聊考主干断裂上,与断层的产状吻合;5次ML≥3.5地震的震源机制显示,双力偶模型可以较好地解释观测波形,小震震源机制主要为走滑型,初动符号呈象限分布;在参考了油田地质构造背景资料后,对濮阳小震集中区中、小地震活动与油田采油作业之间是否存在注水诱发关系进行了讨论.     

Removal of Organic Dyes in Environmental Water onto Magnetic‐Sulfonic Graphene Nanocomposite

A magnetic‐sulfonic graphene nanocomposite (G‐SO₃H/Fe₃O₄) was synthesized and characterized by scanning electron microscopy, Fourier transform infrared spectroscopy, and X‐ray diffraction. It was used for removal of three cationic dyes: safranine T (ST), neutral red (NR), victoria blue (VB), and three anionic dyes: methyl orange, brilliant yellow, and alizarin red, from environmental water. The experimental conditions were optimized, including pH, amount of adsorbent, adsorption kinetics, adsorption isotherms, ionic strength, etc. The results show that G‐SO₃H/Fe₃O₄ can adsorb cationic dyes more efficiently and selectively than anionic dyes at pH 6.0. In the first 10 min of adsorption time, more than 93% of the cationic dyes were removed by the sorbent. Adsorption kinetics follow the pseudo‐second‐order kinetic model well. The adsorption isotherm coincided with Langmuir and Freundlich adsorption models. The maximum adsorption capacities of G‐SO₃H/Fe₃O₄ for ST, NR, and VB dyes were 199.3, 216.8, and 200.6 mg g^?1. The adsorbed cationic dyes were eluted by using different pH values of ethanol as the solvent. The established method was simple, sensitive, and rapid, and was suitable for the adsorption of cationic dyes in environmental water.