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Combination of drainage, water supply and environmental protection as well as rational distribution of water resource in zhengzhou mining district

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Science china Earth Sciences 2005年第10期48卷 1768-1779页

作者： WU Qiang1, LI Duo1,2, DI Zhiqiang3, MIAO Ying3, ZHAO Suqi4 & GUO Qiwen5.1. Resource Exploitation Engineering College, CUMT, Beijing 100083, china 2. Shijiazhuang Engineering College, University of Economics, Shijiazhuang 05.031, china 3. Shenyang Institute of Geology and mineral Resources, Shenyang 110032, china 4. State Adminstration of coal mine Safety, Beijing 100013, china 5. zhengzhou coal mine company (Group), zhengzhou 4523.1, china Resource Exploitation Engineering College CUMT Beijing China Shijiazhuang Engineering College University of Economics Shijiazhuang china Shenyang Institute of Geology and mineral Resources Shenyang china State Adminstration of coal mine Safety Beijing china zhengzhou coal mine company (Group) zhengzhou{5.

The geological condition of coalfield is much complex in china. With increasing in mining depth and drainage amount, the contradiction of drainage, water supply and environ-mental protection is becoming more and more serious. However, the contradiction can be solved by the scientific management of optimizing combination of drainage, water supply and environ-mental protection. The Philip multiple objectives simplex method used in this article has searched for a possible solution at the first step, and then it goes on searching to find out whether there is a weight number that can lead the solution to the biggest. It can reduce the randomness and diffi-culty of traditional weight method which determine the weight number artificially. Some beneficial coefficients are vague and the number is larger in the model of water resource dispatch. So the vague layer analysis method can consider these vague factors fully, combining the qualitative and quantitative analysis together. Especially, this method can quantify the experiential judge-ment of policy decider, and it will turn to be more suitable if the structure of objective factors is complex or the necessary data are absent. In the paper, the two methods above are used to solve the plans of drainage, water supply and optimizing distribution of water resource in the zhengzhou mining district.

关键词： combination of drainage, water supply and environmental protection, Philip multiple objective simplex method, vague layer analysis method, distribution of water resource.

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准噶尔盆地白家海地区西山窑组深部煤岩储层孔隙结构表征及发育主控因素

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中国石油大学学报（自然科学版） 2024年第4期48卷 12-23页

作者：胡鑫姚卫江胡正舟黄福成汪洋汪孝敬中国石油新疆油田分公司勘探开发研究院新疆乌鲁木齐830013 中国石油新疆油田分公司勘探事业部新疆克拉玛依834000

深部煤岩储层孔隙结构特征对深层煤层气勘探开发十分重要,为了明确深部煤岩储层孔隙结构特征及发育主控因素,以准噶尔盆地白家海凸起及周缘侏罗系西山窑组煤层为研究对象,运用覆压孔渗、扫描电镜、高压压汞、低温液氮吸附、二氧化碳等... 详细信息

深部煤岩储层孔隙结构特征对深层煤层气勘探开发十分重要,为了明确深部煤岩储层孔隙结构特征及发育主控因素,以准噶尔盆地白家海凸起及周缘侏罗系西山窑组煤层为研究对象,运用覆压孔渗、扫描电镜、高压压汞、低温液氮吸附、二氧化碳等温吸附等多种试验方法,对西山窑组煤岩储层特征进行研究。结果表明:西山窑组煤岩演化程度低,显微组分以镜质组和惰质组为主,具有低水分、特低灰和低挥发分的特点;西山窑组煤岩储层发育孔缝双重介质储集空间,储层物性好;西山窑组煤岩储层可以划分为3种类型,Ⅰ类储层储集性能好,但渗透性能差,Ⅱ类储层是研究区主要储层类型,进一步分为Ⅱ_(1)类和Ⅱ_(2)类,Ⅱ_(1)类储层具有中等储集性能和良好渗透性能,Ⅱ_(2)类储层与Ⅲ类储层均以微孔为主,物性较差;西山窑组煤层孔隙结构主要受灰分质量分数、镜质组体积分数、惰质组体积分数和埋深控制。

关键词：深部煤岩储层孔隙结构准噶尔盆地白家海凸起西山窑组

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Comprehensive Control on Microstructures and Properties of Medium Carbon V-N Microalloyed Steel Seamless Oil-Well Tubes of Hot-Rolling Non-Quenched/Tempered

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Journal of Iron and Steel Research International 2011年第S1期18卷 696-700页

作者： LIU Sheng-xin 1,2,LIU Guo-quan 2,CHEN Yong 1,ZHANG Yong-gang 3,HUANG Jian-kai 3 (1.School of Materials Science and Engineering,zhengzhou University,zhengzhou 45.002,Hennan china 2.School of Materials Science and Engineering,University of Science and Technology Beijing,100083,china 3.Wuxi Seamless Steel Tube company Ltd,Wuxi 214026,Jiangsu china) zhengzhou Univ Sch Mat Sci & Engn Zhengzhou 450002 Hennan Peoples R China Univ Sci & Technol Beijing Sch Mat Sci & Engn Beijing 100083 Peoples R China Wuxi Seamless Steel Tube Co Ltd Wuxi 214026 Jiangsu Peoples R China

The relationship between microstructures and mechanical properties of a medium carbon V-N microalloyed steel used for N80 seamless oil-well tubes of hot rolling non-quenched/tempered (non-Q and T) was *** results have shown that volume percentages of upper bainite,modified bainite and ferrite have a decisive influence on impact energies of steel *** the total volume percentage of bainite is larger than 5.,the impact energy of tubes can not satisfy with the industrial ***,if the total volume percentage of bainite is smaller than 5.,then the impact energy of steel tubes enhances with volume percentage of ferrite *** final microstructures have closely relation with tube billet quality,controlled cooling temperature after tube rolling and cooling method after *** quality of medium carbon V-N microalloyed steel for non-Q and T oil-well tubes can be produced through comprehensive control of microstructures and mechanical properties in sub-procedures,especially for tube billet quality and controlled cooling parameters.

关键词： medium carbon V-N microalloyed steel N80 grade seamless oil-well tube microstructure mechanical property

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准噶尔盆地侏罗系煤岩气成藏条件及勘探潜力

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中国石油勘探 2024年第4期29卷 31-43页

作者：毛新军李艳平梁则亮朱明姚卫江李树博潘拓胡正舟汪洋中国石油新疆油田公司勘探开发研究院中国石油新疆油田公司勘探事业部

准噶尔盆地侏罗系西山窑组、八道湾组两套煤层广覆式分布,煤系地层气资源十分丰富。但作为一个全新的天然气领域,盆地煤岩气基础研究薄弱、成藏特征、富集规律及资源规模不清。为探索深部煤岩的含气性,2020年钻探风险探井CT1H井,测试获... 详细信息

准噶尔盆地侏罗系西山窑组、八道湾组两套煤层广覆式分布,煤系地层气资源十分丰富。但作为一个全新的天然气领域,盆地煤岩气基础研究薄弱、成藏特征、富集规律及资源规模不清。为探索深部煤岩的含气性,2020年钻探风险探井CT1H井,测试获最高日产气5.7×10^(4)m^(3),试采日产气量稳定在2×10^(4)m^(3),证实煤岩气领域具备高产稳产能力。通过对深部煤岩岩石学特征、煤岩储集性能、演化特征、煤岩气成藏控制因素等系统研究,明确了盆地煤岩演化程度低,属于中—低阶煤,西山窑组煤岩以中—大孔为主,八道湾组煤岩以微—小孔为主;构建了盆地煤岩气古生中储与自生自储两类成藏模式;结合烃源岩、构造、煤岩储层特征及气测异常响应等多种控藏因素对盆地煤岩气潜在领域进行了分类评价,优选了滴南—白家海、齐古两大煤岩气勘探有利区,计算二者2000~4000m埋深煤岩气资源量超万亿立方米。

关键词：准噶尔盆地侏罗系煤岩气成藏模式勘探潜力

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Discovery of agglutinated foraminifers from the Longzhaogou Group in eastern Heilongjiang Province

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Science china Earth Sciences 2004年第2期47卷 122-127页

作者： LI Gang & YU Shanmao1. State Key Laboratory of Paleobiology Stratigraphy, Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences, Nanjing 210008, china 2.108th coal-prospecting Team of Geological Bureau, NE china and Inner Mongolia coal company, Jixi 15.100, china Correspondence should be addressed to Li Gang (email: gangli@***) 1. State Key Laboratory of Paleobiology Stratigraphy Nanjing Institute of Geology and Paleontology Chinese Academy of Sciences 210008 Nanjing China 2. 108th coal-prospecting Team of Geological Bureau NE China and Inner Mongolia Coal Company 158100 Jixi China

The low diversity agglutinated foraminifers are recovered from the Qihulin Formation of the Longzhaogou Group in eastern Heilongjiang, china. The foraminiferal fauna consists of 9 species of 5.genera. The common members are Cribrostomoides nonioninoides (Reuss), Haplophragmoides concavus (Chapman), H. gigas minor Nauss. Although the diagnostic zonal taxa are absent in the agglutinated fauna, according to the global stratigraphic distribution of the above-mentioned species, and the associated Pseudohaploceras ammonite fauna, the foraminiferal fauna may be of a Barremian-Aptian (Early Cretaceous) age.

关键词： Early Cretaceous, agglutinated foraminifers, Longzhaogou Group, eastern Heilongjiang, china.

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Geochemical characteristics and origin of gases from the Upper,Lower Paleozoic and the Mesozoic reservoirs in the Ordos Basin,china

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Science china Earth Sciences 2008年第S1期51卷 183-194页

作者： HU AnPing 1 ,Li Jian 2 ,ZHANG WenZheng 3 ,LI ZhiSheng 2 ,HOU Lu 4 &LIU QuanYou 5.1 Department of Earth Sciences,Zhejiang University,Hangzhou 310027,china 2 Langfang Branch,Reasearch Institute of Petroleum Exploration and Development,Petrochina,Langfang 065.07,china 3 Institute of Exploration and Development,Petrochina Changqing Oilfield company,Xi’an 710021,china 4 University of Petroleum,Beijing102249,china 5.Petrochina Research Institute of Petroleum Exploration and Development,Beijing 100083,china 1. Department of Earth Sciences Zhejiang University Hangzhou 310027 China2. Langfang Branch Reasearch Institute of Petroleum Exploration and Development PetroChina Langfang 065007 China3. Institute of Exploration and Development PetroChina Changqing Oilfield Company Xi’an 710021 China4. University of Petroleum Beijing 102249 China5. PetroChina Research Institute of Petroleum Exploration and Development Beijing 100083 China

The Ordos Basin,the second largest sedimentary basin in china,contains the broad distribution of natural gas *** far,several giant gas fields have been discovered in the Upper and Lower Paleozoic in this basin,each having over 1000×10 8 m 3 of proven gas reserves,and several gas pools have also been discovered in the *** paper collected the data of natural gases and elucidated the geochemical characteristics of gases from different reservoirs,and then discussed their *** hydrocarbons preserved in the Upper Paleozoic,the elevatedδ13C values of methane,ethane and propane indicate that the gases would be mainly coal-formed gases;the singular reversal in the stable carbon isotopes of gaseous alkanes suggests the mixed gases from humic sources with different *** the Lower Paleozoic,theδ13C 1 values are mostly similar with those in the Upper Paleozoic,but theδ13C 2 andδ13C 3 values are slightly lighter,suggesting that the gases would be mixing of coal-type gases as a main member and oil-type *** are multiple reversals in carbon isotopes for gaseous alkanes,especially abnormal reversal for methane and ethane(i.e.δ13C 1 >δ13C 2 ),inferring that gases would be mixed between high-mature coal-formed gases and oil-type *** the Mesozoic,the δ13Cvalues for gaseous alkanes are enriched in 12C,indicating that the gases are mainly derived from sapropelic sources;the carbon isotopic reversal for propane and butane in the Mesozoic is caused by microbial oxidation and mixing of gases from sapropelic sources with different *** contrast to the Upper Paleozoic gases,the Mesozoic gases are characterized by heavier carbon isotopes of iso-butane than normal butane,which may be caused by gases generated from different kerogen types. Finally,according toδ13C 1 -Ro relationship and extremely low total organic carbon contents,the Low Paleozoic gases would not be generated from the Ordovician source as a main gas source,bycontrast, the Upper Pale

关键词： Ordos Basin natural gas chemical composition carbon isotope genesis

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糠醛气相脱羰催化剂的制备

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石油化工 2002年第8期31卷 608-611页

作者：杨国玉赵玮刘金廷彭鸿杰聂燕平吉林工学院化工系吉林长春130012 沙隆达郑州农药有限公司河南郑州450009

采用固定床气相管式反应器研究了糠醛气相脱羰催化剂的制备条件 ,通过对载体、催化剂含量、pH、焙烧温度、还原温度及添加助剂的研究考察 ,找出了糠醛气相脱羰催化剂的最佳制备工艺参数 ,即载体为氧化铝、活性组分钯质量分数 0 3%、pH... 详细信息

采用固定床气相管式反应器研究了糠醛气相脱羰催化剂的制备条件 ,通过对载体、催化剂含量、pH、焙烧温度、还原温度及添加助剂的研究考察 ,找出了糠醛气相脱羰催化剂的最佳制备工艺参数 ,即载体为氧化铝、活性组分钯质量分数 0 3%、pH >9、焙烧温度 5.0 0℃、还原温度 30 0℃、助催化剂为Ni。通过扫描电镜观察催化剂的表面形貌 ,考察了不同焙烧温度对活性组分分散程度的影响。助催化剂Ni的添加提高了催化剂的选择性。

关键词：糠醛气相脱羰催化剂制备呋喃氧化铝肥催化剂

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双氯芬酸钠迟效制剂的药动学

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中国新药与临床杂志 2004年第6期23卷 342-345页

作者：李英谢冬玲周正王高峰高元勋郑州大学第二附属医院河南郑州450003 河南康利医药技术开发公司河南郑州450044 郑州大学癌症研究室河南郑州450052

目的 :以双氯芬酸钠普通肠溶片 (R)为对照 ,比较国产双氯芬酸钠迟效制剂 (T)的相对生物利用度和药动学。方法 :采用双交叉、自身对照的方法 ,将 2 4名受试者分为 2组 ,单剂量组分别口服T和R各 10 0mg ;多剂量组 ,每日分别口服T和R各10 0... 详细信息

目的 :以双氯芬酸钠普通肠溶片 (R)为对照 ,比较国产双氯芬酸钠迟效制剂 (T)的相对生物利用度和药动学。方法 :采用双交叉、自身对照的方法 ,将 2 4名受试者分为 2组 ,单剂量组分别口服T和R各 10 0mg ;多剂量组 ,每日分别口服T和R各10 0mg ,共 4d。结果 :单剂量组T和R的Cmax,Tmax,T1/2 ,MRT ,AUC0～τ分别为 (115.6±s 36 1)和(3910± 96 8) μg·L- 1,(3.0± 1.0 )和 (2 .3± 0 .5.)h ,(6 .6± 2 .3)和 (2 .9± 1.5.)h ,(12 .3± 2 .3)和 (4.4±1.0 )h ,(92 37± 994 )和 (874 5. 12 16 ) μg·h·L- 1,T的F为 (10 7± 12 ) %。多剂量口服T和R的Cav,FI分别为 (343± 4 6 ) μg·L- 1和 (333± 6 4) μg·L- 1,(2 5.4± 82 ) %和 (40 4± 97) %。结论 :2种制剂口服吸收相似 ,迟效制剂具有峰谷浓度差异小 ,血药浓度波动幅度小等缓释药动学特征。

关键词：双氯芬酸迟效制剂药动学色谱法高压液相

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Fe-Cu体系催化剂中铁比的测定及其对催化剂性能的影响

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石油化工 2002年第8期31卷 612-615页

作者：苏运来叶长明孙建伟王向宇郭益群郑州大学工业催化研究所山西煤炭化学研究所煤转化国家重点实验室山西太原030001

用一种比较简便、快捷的化学分析法对组分较为复杂的Fe-Cu体系低碳醇合成催化剂中的铁比进行了分析 ,即用磷酸保护Fe(Ⅲ )离子 ,用碳酸钠保护Fe(Ⅱ )离子。结果表明 ,该法可有效地排除其它组分的干扰 ,分析结果重复性好 ,相对标准偏差RS... 详细信息

用一种比较简便、快捷的化学分析法对组分较为复杂的Fe-Cu体系低碳醇合成催化剂中的铁比进行了分析 ,即用磷酸保护Fe(Ⅲ )离子 ,用碳酸钠保护Fe(Ⅱ )离子。结果表明 ,该法可有效地排除其它组分的干扰 ,分析结果重复性好 ,相对标准偏差RSD不高于 0 0 5.0 %。此外 ,将Fe -Cu体系催化剂的铁比与其催化性能关联后发现 ,铁比控制在 1 0 0～ 2 0 0内 ,催化剂显示出较好的生成醇活性和较高的C+2 醇选择性。

关键词： Fe-Cu体系催化剂铁比测定性能影响铁铜氨合成催化剂合成气低碳醇

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Formation mechanism of carbonate cemented zones adjacent to the top overpressured surface in the central Junggar Basin,NW china

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Science china Earth Sciences 2010年第4期53卷 529-540页

作者： YANG Zhi1,2,ZOU CaiNeng1,3,HE Sheng2,LI QiYan1,HE ZhiLiang3,WU HengZhi5.CAO Feng1,MENG XianLong4,WANG FuRong2 & XIAO Qilin21 State Key Laboratory of EOR,Research Institute of Petroleum Exploration & Development,Petrochina,Beijing 100083,china 2 Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education,china University of Geosciences,Wuhan 430074,china 3 State Key Laboratory of EOR,Research Institute of Petroleum Exploration & Development,Petrochina,Beijing 100083,china 4 Research Institute of Petroleum Exploration and Production,SINOPEC,Beijing 100083,china 5.Southwest Branch company,SINOPEC,Chengdu 61005.,china 1. State Key Laboratory of EOR Research Institute of Petroleum Exploration & Development PetroChina Beijing 100083 China2. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education China University of Geosciences Wuhan 430074 China3. State Key Laboratory of EOR Research Institute of Petroleum Exploration & Development Petrochina Beijing 100083 China5. Southwest Branch Company SINOPEC Chengdu 610051 China4. Research Institute of Petroleum Exploration and Production SINOPEC Beijing 100083 China

Carbonate cemented zones are normally adjacent to the top overpressured surface in the central Junggar Basin,NW *** carbon and oxygen isotopic compositions and petrological investigations of carbonate cements in the carbonate cemented zones indicate that:(1) carbonate cements are composed dominantly of ferrocalcite,ferroan dolomite,and ankerite;(2) carbonate cements are formed under a high temperature circumstance in the subsurface,and organic fluid migration has an important effect on the formation of them;and(3) carbon and oxygen ions in the carbonate cements migrate from the underlying overpressured *** suggests that the occurrence of carbonate cemented zones in this region results from multiple phases of organic fluid expulsion out of the overpressure compartment through geological *** study provides a plausible mechanism of the formation of carbonate cemented zones adjacent to the top overpressured surface in the clastic sedimentary basins,and has an important implication for understanding the internal correlation between the formation of carbonate cemented zones adjacent to top overpressured surface and geofluids expulsion out of overpressured system.

关键词： carbonate cemented zones formation mechanism stable carbon and oxygen isotopic top overpressured surface central Junggar Basin coal-bearing strata

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