Optimization of well placement by combination of a modified particle swarm optimization algorithm and quality map method     

Shuaiwei Ding  Hanqiao Jiang  Junjian Li  Guoping Tang 《Computational Geosciences》2014,18(5):747-762

Determining the optimum placement of new wells in an oil field is a crucial work for reservoir engineers. The optimization problem is complex due to the highly nonlinearly correlated and uncertain reservoir performances which are affected by engineering and geologic variables. In this paper, the combination of a modified particle swarm optimization algorithm and quality map method (QM + MPSO), modified particle swarm optimization algorithm (MPSO), standard particle swarm optimization algorithm (SPSO), and centered-progressive particle swarm optimization (CP-PSO) are applied for optimization of well placement. The SPSO, CP-PSO, and MPSO algorithms are first discussed, and then the modified quality map method is discussed, and finally the implementation of these four methods for well placement optimization is described. Four example cases which involve depletion drive model, water injection model, and a real field reservoir model, with the maximization of net present value (NPV) as the objective function are considered. The physical model used in the optimization analyses is a 3-dimensional implicit black-oil model. Multiple runs of all methods are performed, and the results are averaged in order to achieve meaningful comparisons. In the case of optimizing placement of a single producer well, it is shown that it is not necessary to use the quality map to initialize the position of well placement. In other cases considered, it is shown that the QM + MPSO method outperforms MPSO method, and MPSO method outperforms SPSO and CP-PSO method. Taken in total, the modification of SPSO method is effective and the applicability of QM + MPSO for this challenging problem is promising  相似文献   

贵州习水县仙源煤矿煤层气赋存与开发前景     

徐文慧  唐显贵 《中国煤炭地质》2014,(6):22-25

根据仙源煤矿煤炭地质勘查、矿井地质及煤层气参数井资料,对仙源煤矿煤层气赋存特征进行分析,认为区内龙潭组4层目的煤层厚度较大,煤层间距较小,煤层埋藏深度适中,煤层含气量较高,煤层气富集和赋存条件较好。计算获得矿区煤层气推断资源量达27亿m3,煤层气资源潜力较大,具有较好的勘探开发前景。  相似文献   

贵州省六盘水煤田含煤地层特征分析     

杨瑞琴  ;唐显贵 《中国煤炭地质》2014,(7):28-32

六盘水煤田是贵州的主要产煤区之一,地处黔南坳陷六盘水断坳内,含煤地层主要为上二叠统龙潭组、长兴组,含煤层数多、厚度大,含煤性由中部向西北、南东方向逐渐变差。区内含煤地层的发育主要与含煤岩系基底构造和成煤期岩相古地理有关,晚二叠世早期西部峨眉山玄武岩喷发对含煤岩系基底起到填平补齐作用。盘县—水城古断裂控制着陆相与过渡相的分界,进而控制着两侧含煤地层的含煤性,沉积古地理自西向东由陆相逐渐向海陆交互相过渡,盘县、水城一带聚煤中心为多期次聚煤作用叠加所致。由聚煤中心向西北(陆相)、东南(海相)方向,含煤性逐渐变差。  相似文献   

Upper bound analysis of tunnel face stability in layered soils   总被引：3，自引：3，他引：0  

Xiao-Wu Tang  Wei Liu  Bettina Albers  Stavros Savidis 《Acta Geotechnica》2014,9(4):661-671

The working face of tunnel constructions has to be kept stable during tunneling to prevent large soil deformations or fatal failure. In layered soils with lower cohesion, failures happen more often and more abrupt than in cohesive soils. Therefore, the maintenance of a proper support pressure at the tunnel working face is of high importance. In this paper, an upper bound analysis is introduced to investigate the minimum support pressure for the face stability in layered soils. A three-dimensional kinematically admissible mechanism for the upper bound analysis is improved to model potential failure within different soil layers. An analytical solution for the support pressure assessment is achieved. The influence of the crossing and cover soil on the face stability is analyzed, respectively. This solution provides an analytical estimation of the minimum support pressure for the face stability. It may be used as a reference for projects under similar conditions.  相似文献   

Geochemical behavior of arsenic in reducing sulfidic sediments of reservoir contaminated by acid mine drainage     

C. P. Zhang  P. Wu  C. Y. Tang  H. H. Xie  Z. C. Zeng  S. Z. Yang 《Environmental Earth Sciences》2014,71(10):4341-4351

The sediment from an acid mine drainage affected reservoir of Guizhou province of China has the iron and arsenic concentration of about 400 and 2.6 g/kg, respectively. Sediment cores were collected, and were used to study the arsenic behavior in the seriously acidified reservoir from the viewpoint of chemical thermodynamics. The limestone neutralization and ferric iron hydrolysis regulated the porewater pH from about 2.9–5.8. The reductive dissolution of As–Fe-rich (hydr)oxides under the mild acidic conditions was the main mechanism for the release of absorbed arsenic into porewater. The maximum concentrations of iron, sulfate and arsenic reached to about 2,800, 9,000 and 1 mg/l, respectively. Arsenic speciation transformation and hydrous ferric oxide (HFO) crystallization enhanced the arsenic mobility in sediment. In addition, the iron sulfide minerals diagenesis could play a role in removing the dissolved arsenic from porewater. The actual distribution of arsenic concentration in porewater was well simulated using the model of surface complexation of arsenic to HFO. Although arsenic concentration in porewater could be above 100 times higher than that of reservoir water, it was not easy to release into the reservoir water through diffusion, because the shallow sediment had relatively strong arsenic adsorption capacity, and new HFO could be generated continuously at the sediment water interface.  相似文献   

A study of the interrelation between surface water and groundwater using isotopes and chlorofluorocarbons in Sanjiang plain,Northeast China   总被引：1，自引：0，他引：1  

Bing Zhang  Xianfang Song  Yinghua Zhang  Dongmei Han  Changyuan Tang  Lihu Yang  Zhongliang Wang  Tingyi Liu 《Environmental Earth Sciences》2014,72(10):3901-3913

Surface water and groundwater are the main water resources used for drinking and production. Assessments of the relationship between surface water and groundwater provide information for water resource management in Sanjiang plain, Northeast China. The surface water (river, lake, and wetland) and groundwater were sampled and analyzed for stable isotopic (δD, δ ¹⁸O) composition, tritium, and chlorofluorocarbons concentrations. The local meteoric water line is δD = 7.3δ ¹⁸O–6.7. The tritium (T) and chlorofluorocarbon (CFC) contents in groundwater were analyzed to determine the groundwater ages. Most groundwater were modern water with the ages <50 years. The groundwaters in mountain area and near rivers were younger than in the central plain. The oxygen isotope (δ ¹⁸O) was used to quantify the relationship between surface water and groundwater. The Songhua, Heilongjiang, and Wusuli rivers were gaining rivers, but the shallow groundwater recharged from rivers at the confluence area of rivers. At the confluence of Songhua and Heilongjiang rivers, 88 % of the shallow groundwater recharged from Songhua river. The combination of stable isotopes, tritium, and CFCs was an effectively method to study the groundwater ages and interrelation between surface water and groundwater. Practically, the farmlands near the river and under foot of the mountain could be cultivated, but the farmlands in the central plain should be controlled.  相似文献   

Fine description of structure and sedimentary microfacies of Li32 block of Lijin oilfield,Dongying depression,China     

Ding Fang  Zhang Jinliang  Xie Jun  Li Cunlei  Shi Chaoqun  Zhang Penghui  Zhang Ming  Tang Mingming 《Arabian Journal of Geosciences》2014,7(5):1693-1704

Considering that available data in Li32 block is limited, log phase method and core analysis were used to divide sedimentary facies and sequence, the former is principal, and two short-term cycles, five middle term cycles, and fifteen short-term cycles were divided. Combined seismic interpretation with fault point and fault rod, the instantaneous phase profile explained small fault more clearly and accurately. The sever faults were analyzed, and integrated structure was constructed. Lithofacies in cored wells were observed; the grain-size probability curves mainly are suspension and jumping transport; grain size is mainly for the siltstone and fine sandstone; the color of mud in the second segment of Shahejie formation (ES2) is mainly gray–green, gray to dark gray, these reflect that sediment environment is delta front, which included underwater distributary channel, mouth bar, distal bar, and so on. Well data and structural maps were integrated to build 3D structure model and sedimentary microfacies model of Li32 reservoirs using stochastic simulations with geometry data. The integrated 3D geological model is a valuable tool of reflecting geologic body with great reality and can accurately represent and describe the complex reservoir heterogeneity.  相似文献   

Effect of saltwater intrusion on groundwater environment in Weihe River downstream,Shandong Province,China     

MENG Yong-hui  WANG Ji-ning  YU De-Jie  ZHANG Li-xia  FENG Zai-min  YAN Tang  ZHOU Yong 《地下水科学与工程》2014,7(3):245-252

Based on the geological and hydrogeological conditions along with dynamic changes of groundwater level, this paper analyzes the hydrodynamic characteristics of saltwater intrusion in the study area. According to monitoring data of groundwater quality, the distribution characteristics of macro component are analyzed, and then fuzzy comprehensive evaluation method is adopted to evaluate the impact of saltwater intrusion on groundwater environment. Concerning the influence degree of groundwater environment, the study area is divided into brine area, seriously influenced area, moderately influenced zone, slightly influenced zone and uninfluenced zone. The results can offer references for prevention and control of saltwater intrusion as well as the protection of water resources.  相似文献   

电测深法在撒哈拉沙漠地区找水应用     

唐英杰 《地下水》2014,(3):107-109

撒哈拉沙漠地区气候干燥,水资源缺乏,相应的地质、水文地质工作研究程度低,为水源地勘探工作带来很大困难。结合实例,采用电测深法,遵循从已知到未知原则,经过点、线、面逐步开展工作,总结含水层物性特征,划定主要含水区域,为水文工作的开展提供重要的基础资料。  相似文献   

桂西北喀斯特山区人口分布特征及其与自然因素的关系   总被引：1，自引：0，他引：1  

史莎娜  谢炳庚  胡宝清  汤传勇  闫妍  李晓青 《地理科学》2019,39(9):1484-1495

选择第六次全国人口普查的最小行政单位——乡（镇）为基本单元,利用Lorenz曲线和空间相关分析方法分析桂西北喀斯特山区乡（镇）级尺度下的人口空间分布特征,运用地理探测器方法探测自然因素单独和叠加作用后对区域人口空间分布的影响强度。结果表明： 乡（镇）级研究尺度下的人口空间分布具有不均衡性特征,呈现一般显著正相关和一定的聚集性; 各自然因素空间分布对人口分布的影响呈现显著差异,研究区西北和中南部没有喀斯特分布的乡镇,人口密度随有利于人类居住因素的增加而增加,但平均人口密度仅79人/km ²。东部和南部有喀斯特分布的乡镇,人口密度与自然因素空间分布并非简单的增减关系,其随喀斯特分布面积的变化呈现起伏波动。 地理探测器的因子探测结果显示对人口空间分布的影响强度最大的为海拔高度,交互探测结果显示,任意两个自然因素叠加交互作用后的影响强度呈现非线性增强和双因子增强。可见,桂西北喀斯特山区与其他地区类似,海拔高度是影响人口空间分布的最主要因素之一,但喀斯特山区的河网密度及特有的地质地貌等因素对其人口的空间分布具有较强的催化作用,与其他因素叠加交互作用可进一步加强对人口分布的影响。  相似文献