溢洪道上层开挖及支护施工

阐述溢洪道特大洞室上层开挖通过溶洞群地段的超前地质钻探、上下分部短台阶开挖，自钻式锚杆及小导管注浆结合钢格栅、喷锚支护等综合处理措施的施工技术，与各位同行共同探讨。     

地下储层建筑结构预测模型的建立

在露头研究、岩心分析的基础上 ,在双河油田建立了不同于 Miall划分方案的 6级界面系列 ,总结了 7种基本结构要素 (水下分流道、河口坝、水下溢岸、前缘席状砂、重力流、水下决口扇、湖相泥 )的特征及测井响应 .通过储层精细对比 ,建立了双河油田核三段 I- IV油组的储层建筑结构预测模型 ,总结了建立地下储层建筑结构模型的方法和基本步骤 .模型表明扇三角洲平面模型具有分带性 ,剖面模型则可分为分流河道型、分流河道与河口坝型、席状砂型、递变型 .建筑结构模型可用于建立储层精细流动单元模型或结合开发动态 ,据此可直接进行剩余油分布分析     

黔中地区岩溶洞穴翼手类的初步调查及部分生态观察

从 1995年 5月至 1999年 12月间对黔中地区的龙天洞、唐官大坡洞、和尚洞和大洞口等 2 1个洞穴的翼手类进行了初步调查 ,共捕获标本 2 0 0余号 ,经鉴定计 16种 ,隶属 3科 7属。此外 ,还对翼手类的部分生态进行了观察 ,共观察多种翼手类 10 0 0余只。分析了光和温度对翼手类活动的影响及湿度对翼手类分布的影响 ,翼手类的水平和空间分布、昼夜活动及在洞穴生态系统中的作用。还对翼手类的保护进行了探讨     

Downcutting and uplifting in the middle part of Qinling orogenic belt during the late Quaternary

Layered cave passages formed on the walls of the Qianyou River valley in the middle part of the Qinling Mountains since the Pleistocene due to the intermittent uplifts. 12 speleothem samples near ruins of palaeowater tables in 3 cave passages are dated by using the 230Th method. The results show that the 3 caves began to uplift (358±38) ka, (247±28) ka, (118±19) ka ago respectively. Given the differences of elevation between the caves, we could obtain the downcutting rates of the valley: (0.23(0.02) mm/a during 358-247 ka, (0.19(0.03) mm/a during 247-118 ka, and (0.51(0.08) mm/a since 118 ka. This implies that more andmore strong uplifting sustained in the middle part of Qinling since 358 k     

贵州喀斯特洞穴空间数据库建立与应用

贵州是我国沉积岩最发育的省份之一 ,从元古代的板溪群到第四纪均有发育 ,以浅海相碳酸盐岩沉积为主 ,除东南一角外 ,遍及全省和各地质时代 ,厚度 3 0 0 0～ 12 0 0 0m ,面积约占 70 %以上 ,洞穴特别发育。贵州岩溶洞穴空间信息数据库 ,是以GIS技术为基础的新型空间信息管理系统。     

特高含水期扇三角洲储集层剩余油分布及挖潜途径

综合分析岩芯、测井、生产资料等静态和动态资料，并在油藏三维两相模拟的基础上，多层次、多角度探讨了双河曲田北块Ⅳ1－3层系扇三角洲储集层油藏特高含水期剩余油分布规律、成因因互及潜力类型。研究表明：扇三角洲储集层油藏特高含水开发期后期，剩余油高度分散和隐蔽，不同储层砂体剩余油分布、潜力、水淹模式不同，前缘席状砂体、河口坝砂体是进一步挖潜的对象。层内、层面及平面非均质性控制了水驱油田的开发和剩余油的分布，层内及层间非均质性控制了油层的水淹厚度及垂向上剩余油的分布，平面非均质性控制了油层的水淹面积及剩余油平面分布。在完善井网的基础上，进行注采结构及注水合理调配是扇三角洲储集层油藏特高含水开发后期综合挖潜的途径。     

茂兰喀斯特森林洞穴蜘蛛初步调查

2014年至2017年对茂兰喀斯特森林的5个洞穴进行了蜘蛛标本的采集和调查;共采集到1000余号标本,隶属15科34属45种,常见科为园蛛科、漏斗蛛科和球蛛科,优势种有温室希蛛Achaeranea tepidariorum、阴暗隙蛛Coelotasluctrosus、狩猎巨蟹蛛Heteropodavenatoria、中华镂网蛛Psechrussinensis、山地艾蛛Cyclosa monticola、黑斑盖蛛Neriene nigripectoris等。洞穴蜘蛛群落组成分为有光带、弱光带、黑暗带群落。     

Application of Inductively Coupled Plasma Spectrometric Techniques and Multivariate Statistical Analysis in the Hydrogeochemical Profiling of Caves—Case Study Cloșani,Romania

The aim of the study was to develop the hydrogeochemical profiling of caves based on the elemental composition of water and silty soil samples and a multivariate statistical analysis. Major and trace elements, including rare earths, were determined in the water and soil samples. The general characteristics of water, anions content, inorganic and organic carbon fractions and nitrogen species (NO₃⁻ and NH₄⁺) were also considered. The ANOVA—principal component analysis (PCA) and two-way joining analysis were applied on samples collected from Cloșani Cave, Romania. The ANOVA-PCA revealed that the hydrogeochemical characteristics of Ca²⁺-HCO₃⁻ water facies were described by five factors, the strongest being associated with water-carbonate rock interactions and the occurrence of Ca, Mg and HCO₃⁻ (43.4%). Although organic carbon fractions have a lower influence (20.1%) than inorganic ones on water characteristics, they are involved in the chemical processes of nitrogen and of the elements involved in redox processes (Fe, Mn, Cr and Sn). The seasonal variability of water characteristics, especially during the spring, was observed. The variability of silty soil samples was described by four principal components, the strongest influence being attributed to rare earth elements (52.2%). The ANOVA-PCA provided deeper information compared to Gibbs and Piper diagrams and the correlation analysis.     

河南双河油田核三段Ⅰ—Ⅲ油组储层特征研究

通过研究区内大量铸体薄片及物性资料的分析,对双河油田核三段Ⅰ—Ⅲ油组储层的岩石学特征、孔隙结构及孔隙类型、储层物性特征进行研究。分析了影响储层储集性能的主要因素。研究表明,以扇三角洲前缘沉积为主的Ⅰ—Ⅲ油组储集层具有成分成熟度和结构成熟度均较低的特点。储层以粒间孔隙、溶蚀孔隙最为发育,属中孔中渗—高渗类型。储层物性主要受沉积相带的控制。     

不同等级石漠化地区洞穴滴水的物理化学特征对比研究

对贵州不同等级石漠化地区6个洞穴7月份的滴水物理指标(滴水滴率、电导率)和化学指标(p H值、Ca2+)进行了监测,并探讨了各指标的变化规律及环境意义,得出以下结论:1受地表植被影响,潜在石漠化地区洞穴滴水滴率较强度石漠化地区小,随着洞穴长度的加深,不同等级石漠化地区滴水滴率均趋于稳定;2各滴水点p H值并未表现出降雨的稀释效应,潜在石漠化地区不同洞穴的滴水p H值情况表现不一致,强度石漠化地区p H值普遍偏高;3潜在石漠化地区较强度石漠化地区滴水电导率偏大,不同等级石漠化地区洞穴滴水的电导率值正比于滴水Ca2+含量。