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Enrichment model and major controlling factors of below-source tight oil in Lower Cretaceous Fuyu reservoirs in northern Songliao Basin,NE China
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作者 WANG Xiaojun BAI Xuefeng +9 位作者 LI Junhui JIN Zhijun WANG Guiwen CHEN Fangju ZHENG Qiang HOU Yanping YANG Qingjie LI Jie LI Junwen CAI Yu 《Petroleum Exploration and Development》 SCIE 2024年第2期279-291,共13页
Based on the geochemical,seismic,logging and drilling data,the Fuyu reservoirs of the Lower Cretaceous Quantou Formation in northern Songliao Basin are systematically studied in terms of the geological characteristics... Based on the geochemical,seismic,logging and drilling data,the Fuyu reservoirs of the Lower Cretaceous Quantou Formation in northern Songliao Basin are systematically studied in terms of the geological characteristics,the tight oil enrichment model and its major controlling factors.First,the Quantou Formation is overlaid by high-quality source rocks of the Upper Cretaceous Qingshankou Formation,with the development of nose structure around sag and the broad and continuous distribution of sand bodies.The reservoirs are tight on the whole.Second,the configuration of multiple elements,such as high-quality source rocks,reservoir rocks,fault,overpressure and structure,controls the tight oil enrichment in the Fuyu reservoirs.The source-reservoir combination controls the tight oil distribution pattern.The pressure difference between source and reservoir drives the charging of tight oil.The fault-sandbody transport system determines the migration and accumulation of oil and gas.The positive structure is the favorable place for tight oil enrichment,and the fault-horst zone is the key part of syncline area for tight oil exploration.Third,based on the source-reservoir relationship,transport mode,accumulation dynamics and other elements,three tight oil enrichment models are recognized in the Fuyu reservoirs:(1)vertical or lateral migration of hydrocarbon from source rocks to adjacent reservoir rocks,that is,driven by overpressure,hydrocarbon generated is migrated vertically or laterally to and accumulates in the adjacent reservoir rocks;(2)transport of hydrocarbon through faults between separated source and reservoirs,that is,driven by overpressure,hydrocarbon migrates downward through faults to the sandbodies that are separated from the source rocks;and(3)migration of hydrocarbon through faults and sandbodies between separated source and reservoirs,that is,driven by overpressure,hydrocarbon migrates downwards through faults to the reservoir rocks that are separated from the source rocks,and then migrates laterally through sandbodies.Fourth,the differences in oil source conditions,charging drive,fault distribution,sandbody and reservoir physical properties cause the differential enrichment of tight oil in the Fuyu reservoirs.Comprehensive analysis suggests that the Fuyu reservoir in the Qijia-Gulong Sag has good conditions for tight oil enrichment and has been less explored,and it is an important new zone for tight oil exploration in the future. 展开更多
关键词 northern Songliao Basin Cretaceous Quantou Formation Qingshankou Formation upper generation and lower storage Fuyu reservoir tight oil main control factor enrichment model
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Enrichment factors of movable hydrocarbons in lacustrine shale oil and exploration potential of shale oil in Gulong Sag,Songliao Basin,NE China 被引量:5
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作者 ZHAO Wenzhi BIAN Congsheng +9 位作者 LI Yongxin ZHANG Jinyou HE Kun LIU Wei ZHANG Bin LEI Zhengdong LIU Chang ZHANG Jingya GUAN Ming LIU Shijul 《Petroleum Exploration and Development》 SCIE 2023年第3期520-533,共14页
The geological characteristics and production practices of the major middle-and high-maturity shale oil exploration areas in China are analyzed.Combined with laboratory results,it is clear that three essential conditi... The geological characteristics and production practices of the major middle-and high-maturity shale oil exploration areas in China are analyzed.Combined with laboratory results,it is clear that three essential conditions,i.e.economic initial production,commercial cumulative oil production of single well,and large-scale recoverable reserves confirmed by the testing production,determine whether the continental shale oil can be put into large-scale commercial development.The quantity and quality of movable hydrocarbons are confirmed to be crucial to economic development of shale oil,and focuses in evaluation of shale oil enrichment area/interval.The evaluation indexes of movable hydrocarbon enrichment include:(1)the material basis for forming retained hydrocarbon,including TOC>2%(preferentially 3%-4%),and typeⅠ-Ⅱkerogens;(2)the mobility of retained hydrocarbon,which is closely related to the hydrocarbon composition and flow behaviors of light/heavy components,and can be evaluated from the perspectives of thermal maturity(Ro),gas-oil ratio(GOR),crude oil density,quality of hydrocarbon components,preservation conditions;and(3)the reservoir characteristics associated with the engineering reconstruction,including the main pore throat distribution zone,reservoir physical properties(including fractures),lamellation feature and diagenetic stage,etc.Accordingly,13 evaluation indexes in three categories and their reference values are established.The evaluation indicates that the light shale oil zones in the Gulong Sag of Songliao Basin have the most favorable enrichment conditions of movable hydrocarbons,followed by light oil and black oil zones,containing 20.8×10^(8) t light oil resources in reservoirs with R_(0)>1.2%,pressure coefficient greater than 1.4,effective porosity greater than 6%,crude oil density less than 0.82 g/cm^(3),and GOR>100 m/m^(3).The shale oil in the Gulong Sag can be explored and developed separately by the categories(resource sweet spot,engineering sweet spot,and tight oil sweet spot)depending on shale oil flowability.The Gulong Sag is the most promising area to achieve large-scale breakthrough and production of continental shale oil in China. 展开更多
关键词 Gulong Sag continental shale oil movable hydrocarbon enrichment factor enrichment zone/interval evaluation material basis component flow engineering-associated factor
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Controlling factors and models of shale oil enrichment in Lower Permian Fengcheng Formation,Mahu Sag,Junggar Basin,NW China 被引量:2
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作者 JIANG Fujie HU Meiling +8 位作者 HU Tao LYU Jiahao HUANG Liliang LIU Chenglin JIANG Zhenxue HUANG Renda ZHANG Chenxi WU Guanyun WU Yuping 《Petroleum Exploration and Development》 SCIE 2023年第4期812-825,共14页
Based on the combination of core observation,experimental analysis and testingand geological analysis,the main controlling factors of shale oil enrichment in the Lower Permian Fengcheng Formation in the Mahu Sag of th... Based on the combination of core observation,experimental analysis and testingand geological analysis,the main controlling factors of shale oil enrichment in the Lower Permian Fengcheng Formation in the Mahu Sag of the Junggar Basin are clarified,and a shale oil enrichment model is established.The results show that the enrichment of shale oil in the Fengcheng Formation in the Mahu Sag is controlled by the organic abundance,organic type,reservoir capacity and the amount of migration hydrocarbon in shale.The abundance of organic matter provides the material basis for shale oil enrichment,and the shales containing typesⅠandⅡorganic matters have good oil content.The reservoir capacity controls shale oil enrichment.Macropores are the main space for shale oil enrichment in the Fengcheng Formation,and pore size and fracture scale directly control the degree of shale oil enrichment.The migration of hydrocarbons in shale affects shale oil enrichment.The shale that has expelled hydrocarbons has poor oil content,while the shale that has received hydrocarbons migrated from other strata has good oil content.Lithofacies reflect the hydrocarbon generation and storage capacity comprehensively.The laminated felsic shale,laminated lime-dolomitic shale and thick-layered felsic shale have good oil content,and they are favorable lithofacies for shale oil enrichment.Under the control of these factors,relative migration of hydrocarbons occurred within the Fengcheng shale,which leads to the the difference in the enrichment process of shale oil.Accordingly,the enrichment mode of shale oil in Fengcheng Formation is established as"in-situ enrichment"and"migration enrichment".By superimposing favorable lithofacies and main controlling factors of enrichment,the sweet spot of shale oil in the Fengcheng Formation can be selected which has great significance for the exploration and development of shale oil. 展开更多
关键词 Junggar Basin Mahu Sag Permian Fengcheng Formation shale oil enrichment controlling factors enrichment model lithofacies
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Factors Controlling Organic Matter Enrichment in Alkaline Lacustrine Source Rocks:A Case Study of the Late Paleozoic Fengcheng Formation in the Junggar Basin,NW China
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作者 HUANG Renda JIANG Fujie +7 位作者 HU Tao CHEN Di HUANG Liliang LIU Zheyu WANG Xiaohao ZHANG Chenxi LU Jiahao WU Yuping 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2023年第6期1744-1755,共12页
The late Paleozoic Fengcheng Formation shale(LPF shale)in the Junggar Basin,NW China,is the oldest alkaline source rock discovered in the world,providing a unique perspective with which to explore organic matter(OM)en... The late Paleozoic Fengcheng Formation shale(LPF shale)in the Junggar Basin,NW China,is the oldest alkaline source rock discovered in the world,providing a unique perspective with which to explore organic matter(OM)enrichment in alkaline lake environments.Combined with the organic carbon isotope profile and paleoenvironmental proxies,this study reveals that the LPF shale was deposited in an arid climate with high salinity and a strong reducing environment,accompanied by frequent volcanic activity.High TOC values are concentrated in two intervals with frequent fluctuations in OM types.A negative excursion due to changes in sedimentary OM source is found in the δ^(13)C_(org) profile.The excursion corresponds to the OM enrichment interval and is accompanied by abnormally high values of Sr/Ba and Sr/Cu.This implies that the extreme arid climate has led to high salinity,resulting in strong reducibility and changes in paleontological assemblages,which in turn controlled the differential enrichment of OM.The Fengcheng Fm.high-quality source rocks are the result of the combined action of climatic events,volcanism,high-salinity water environment and superior hydrocarbon-generating organisms.The results provide new insights into the formation conditions of terrestrial alkaline high-quality source rocks and the factors controlling alkaline OM enrichment. 展开更多
关键词 organic matter enrichment control factors alkaline lake source rocks Fengcheng Formation Junggar Basin
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Assessment of Axial Power Peaking Factors in GHARR-1 LEU Core: A Decadal Simulation Analysis
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作者 Emmanuel Kwame Ahiave Emmanuel Ampomah-Amoako +1 位作者 Rex Gyeabour Abrefah Mathew Asamoah 《World Journal of Nuclear Science and Technology》 CAS 2024年第1期72-85,共14页
This study aims to thoroughly investigate the axial power peaking factors (PPF) within the low-enriched uranium (LEU) core of the Ghana Research Reactor-1 (GHARR-1). This study uses advanced simulation tools, like the... This study aims to thoroughly investigate the axial power peaking factors (PPF) within the low-enriched uranium (LEU) core of the Ghana Research Reactor-1 (GHARR-1). This study uses advanced simulation tools, like the MCNPX code for analysing neutron behavior and the PARET/ANL code for understanding power variations, to get a clearer picture of the reactor’s performance. The analysis covers the initial six years of GHARR-1’s operation and includes projections for its whole 60-year lifespan. We closely observed the patterns of both the highest and average PPFs at 21 axial nodes, with measurements taken every ten years. The findings of this study reveal important patterns in power distribution within the core, which are essential for improving the safety regulations and fuel management techniques of the reactor. We provide a meticulous approach, extensive data, and an analysis of the findings, highlighting the significance of continuous monitoring and analysis for proactive management of nuclear reactors. The findings of this study not only enhance our comprehension of nuclear reactor safety but also carry significant ramifications for sustainable energy progress in Ghana and the wider global context. Nuclear engineering is essential in tackling global concerns, such as the demand for clean and dependable energy sources. Research on optimising nuclear reactors, particularly in terms of safety and efficiency, is crucial for the ongoing advancement and acceptance of nuclear energy. 展开更多
关键词 GHARR-1 Power Peaking factor Nuclear Reactor Safety Low Enriched Uranium Core Operational Longevity Thermal Hydraulics
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Differential Hydrocarbon Enrichment and its Main Controlling Factors in Depressions of the Bohai Bay Basin Differential Hydrocarbon Enrichment and its Main Controlling Factors in Depressions of the Bohai Bay Basin 被引量:15
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作者 JIANG Youlu LIU Hua +4 位作者 SONG Guoqi WANG Yongshi LIU Jingdong ZHAO Kai LYU Xueying 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2017年第5期1855-1872,共18页
Significant differential hydrocarbon enrichment occurs in depressions in a petroliferous basin.There are multiple depressions in the Bohai Bay Basin, and each depression as a relatively independent unit of hydrocarbon... Significant differential hydrocarbon enrichment occurs in depressions in a petroliferous basin.There are multiple depressions in the Bohai Bay Basin, and each depression as a relatively independent unit of hydrocarbon generation, migration and accumulation, contains significantly different hydrocarbon generation conditions and enrichment degree. On the basis of previous documents and a large number of statistical data, this work comparatively analyzed the differential hydrocarbon enrichment and its major controlling factors in depressions of the Bohai Bay Basin. The results show that depressions in the Bohai Bay Basin have various hydrocarbon enrichment degrees, and can be categorized into four types, namely enormously oil-rich, oil-rich, oily and oil-poor depressions. In general, the enormously oil-rich and oil-rich depressions are distributed in the eastern part of the basin along the Tan-Lu and Lan-Liao faults, whereas depressions in the western part of the basin are poor in hydrocarbons. Moreover, the vertical distribution of hydrocarbons is also highly heterogeneous, with Pre-Paleogene strata rich in hydrocarbons in the northern and western depressions, Paleogene strata rich in hydrocarbons in the entire basin, and Neogene strata rich in hydrocarbons in the off-shore areas of the Bohai Bay Basin. From early depressions in onshore areas to the late depressions in offshore areas of the Bohai Bay Basin, the source rocks and source-reservoir-cap rock assemblages gradually become younger and shallower, and the hydrocarbon resource abundance gradually increases. Hydrocarbon supplying condition is the key factor constraining the hydrocarbon enrichment for different depressions,while the main source-reservoir-cap rock assemblage, sufficient hydrocarbons and the transportation capacity of faults control the vertical distribution of hydrocarbons. The main factors controlling hydrocarbon enrichment are different for different layers. The hydrocarbon supplying condition of source rocks is the key controlling factor, whereas the source-reservoir configuration, the main sourcereservoir-cap rock assemblages, and the fault transportation are the main factors of hydrocarbon enrichment in the Paleogene, Paleogene and Neogene, respectively. 展开更多
关键词 differential hydrocarbon enrichment hydrocarbon distribution hydrocarbon-rich depression fault transportation main controlling factors Bohai Bay Basin
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An Assessment of Heavy-Metal Contamination in Soils within Auto-Mechanic Workshops Using Enrichment and Contamination Factors with Geoaccumulation Indexes 被引量:4
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作者 Isaac A. Ololade 《Journal of Environmental Protection》 2014年第11期970-982,共13页
Soil characterization and heavy metals in different layers (0 - 15 cm;15 - 30 cm and 30 - 45 cm depth) of automobile mechanic waste dumps were studied. The soils showed remarkably high levels of all the metals above b... Soil characterization and heavy metals in different layers (0 - 15 cm;15 - 30 cm and 30 - 45 cm depth) of automobile mechanic waste dumps were studied. The soils showed remarkably high levels of all the metals above background concentrations with most (Ni, Cu, Fe, Cr and Cd) decreasing with soil depth. The distribution pattern were in the following order Fe > Cu > Zn > Pb > Cr > Ni > Cd. Across all the sampling locations and profiles, Fe and Cd showed the highest (476.4 μg·g-1) and least (37.5 μg·g-1) mean concentrations respectively. Pollution load index (PLI) and index of geoaccumulation (Igeo) revealed overall high and moderate contamination respectively but the enrichment factors (EFs) for Pb Ni and Cd are severe. The inter-element relationship revealed the identical source of elements in the soils of the studied area. The accuracy of the results has been cheeked using the standard reference material;SRM (PACS-2). The mechanic waste dumps represent potential sources of heavy metal pollution to environment. The elevated levels of heavy metals in these soil profiles constitute a serious threat to both surface and groundwater. 展开更多
关键词 HEAVY Metals SOIL CONTAMINATION SOIL Profiles Automobile MECHANIC enrichment factor Geoaccumulation Index
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Enrichment of tight oil and its controlling factors in central and western China 被引量:5
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作者 SONG Yan LUO Qun +2 位作者 JIANG Zhenxue YANG Wei LIU Dongdong 《Petroleum Exploration and Development》 CSCD 2021年第2期492-506,共15页
Taking the tight oil of the Zhongnan sag in the Ordos Basin,Jimusar sag in the Junggar Basin and Qingxi sag in the Jiuquan Basin as study objects,based on field survey,dissection of tight oil reservoirs,sample test,mo... Taking the tight oil of the Zhongnan sag in the Ordos Basin,Jimusar sag in the Junggar Basin and Qingxi sag in the Jiuquan Basin as study objects,based on field survey,dissection of tight oil reservoirs,sample test,modeling experiment and comprehensive analysis,this study reveals that the tight oil accumulates at start-up pressure,advances under differential pressure,diffuses at alternating fast and low speeds,charges in stepped large area and migrates rapidly through fractures,and enriches in dominant fractures and pores.The root cause of ladder-like charge is the multiple scales of pores.The widespread source rock with high hydrocarbon generation intensity is the material basis for tight oil enrichment;the dominant source reservoir assemblage is the basic unit for tight oil enrichment;fractures and beddings are conducive to local rapid migration of tight oil;fractures and pores work together to control the enrichment of tight oil.Two typical accumulation models of tight oil are established,namely"source reservoir in coexistence,four optimal factors controlling enrichment around central area,and large-scale continuous distribution"for a large freshwater lake clastic rock basin and"source reservoir integration,four optimal factors controlling enrichment,central area distribution,small in size but high in enrichment degree"for a small saline lake diamictite depression. 展开更多
关键词 tight oil enrichment mechanism main control factor enrichment model central and western China
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Coalbed Methane Enrichment Regularity and Major Control Factors in the Xishanyao Formation in the Western Part of the Southern Junggar Basin 被引量:2
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作者 YUAN Yuan SHAN Yansheng +1 位作者 TANG Yue CAO Daiyong 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2020年第2期485-500,共16页
There are abundant coal and coalbed methane(CBM)resources in the Xishanyao Formation in the western region of the southern Junggar Basin,and the prospects for CBM exploration and development are promising.To promote t... There are abundant coal and coalbed methane(CBM)resources in the Xishanyao Formation in the western region of the southern Junggar Basin,and the prospects for CBM exploration and development are promising.To promote the exploration and development of the CBM resources of the Xishanyao Formation in this area,we studied previous coalfield survey data and CBM geological exploration data.Then,we analyzed the relationships between the gas content and methane concentration vs.coal seam thickness,burial depth,coal reservoir physical characteristics,hydrogeological conditions,and roof and floor lithology.In addition,we briefly discuss the main factors influencing CBM accumulation.First,we found that the coal strata of the Xishanyao Formation in the study area are relatively simple in structure,and the coal seam has a large thickness and burial depth,as well as moderately good roof and floor conditions.The hydrogeological conditions and coal reservoir physical characteristics are also conducive to the enrichment and a high yield of CBM.We believe that the preservation of CBM resources in the study area is mainly controlled by the structure,burial depth,and hydrogeological conditions.Furthermore,on the basis of the above results,the coal seam of the Xishanyao Formation in the synclinal shaft and buried at depths of 700-1000 m should be the first considered for development. 展开更多
关键词 coalbed methane enrichment REGULARITY MAJOR control factors Xishanyao Formation western area of the southern JUNGGAR Basin
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Controlling factors of marine shale gas differential enrichment in southern China 被引量:5
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作者 JIANG Zhenxue SONG Yan +8 位作者 TANG Xianglu LI Zhuo WANG Xingmeng WANG Guozhen XUE Zixin LI Xin ZHANG Kun CHANG Jiaqi QIU Hengyuan 《Petroleum Exploration and Development》 2020年第3期661-673,共13页
Based on the exploration and development practice of marine shale gas in Fuling, Weiyuan, Changning, Luzhou and Southeast Chongqing in southern China, combined with experiments and analysis, six factors controlling di... Based on the exploration and development practice of marine shale gas in Fuling, Weiyuan, Changning, Luzhou and Southeast Chongqing in southern China, combined with experiments and analysis, six factors controlling differential enrichment of marine shale gas are summarized as follows:(1) The more appropriate thermal evolution and the higher the abundance of organic matter, the higher the adsorption and total gas content of shale will be.(2) Kerogen pyrolysis and liquid hydrocarbon cracking provide most of the marine shale gas.(3) The specific surface area and pore volume of organic matter rich shale increased first and then decreased with the increase of thermal evolution degree of organic shale. At Ro between 2.23% and 3.33%, the shale reservoirs are mainly oil-wet, which is conducive to the enrichment of shale gas.(4) The thicker the roof and floor, the higher the shale gas content. The longer the last tectonic uplift time and the greater the uplift amplitude, the greater the loss of shale gas will be.(5) The buried depth and dip angle of the stratum have different controlling and coupling effects on shale gas in different tectonic positions, resulting in two differential enrichment models of shale gas.(6) The effective and comprehensive matching of source, reservoir and preservation conditions determines the quality of shale gas accumulation. Good match of effective gas generating amount and time, moderate pore evolution and good preservation conditions in space and time is essential for the enrichment of shale gas. 展开更多
关键词 southern China shale gas differential enrichment main controlling factors factors matching accumulation effect
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Evaluation of Nutrients and Trace Metals and Their Enrichment Factors in Soil and Sugarcane Crop Irrigated with Wastewater 被引量:1
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作者 Mohammed Abdullah Alghobar Sidduraiah Suresha 《Journal of Geoscience and Environment Protection》 2015年第8期46-56,共11页
The study was conducted to investigate enrichment factor of wastewater (WW) irrigation to agricultural soils and the bioconcentration factor of trace metals uptake by sugarcane and to determine the concentrations of n... The study was conducted to investigate enrichment factor of wastewater (WW) irrigation to agricultural soils and the bioconcentration factor of trace metals uptake by sugarcane and to determine the concentrations of nutrients in sugarcane by growing the same on a contaminated soil, during the growth period of crop in Vidyaranyapuram area in the South West of Mysore, Karnataka. The concentrations of macronutrients and trace metals in the soil sampled sugarcane crop were found highly significant in Ca, Mg, K, Na, N, Mn, Cu, Ni and Cr. The enrichment factor was maximum for N and Na, and the values of N and Na were in the significant enrichment category. Whereas the values of following elements (K, P, Ca, SO4, Cu, Cr, Mg, Mn, Ni, Cd, Fe, Pb, Cl, Co and Zn) in soil irrigated with WW were in moderate enrichment category. The mean concentrations of N, P, K, Ca, Na, Fe, Mn, and Pb in sugarcane leaves in wastewater treatment crops were significantly higher than those with ground water (GW) treated which showed the lowest concentrations. Calculation of the bioconcentration factor (BCF) indicated that the accumulation of heavy metals in sugarcane crop was in the order Cd > Zn > Co > Pb > Mn > Ni > Cu > Cr > Fe. Pearson’s correlation coefficient indicated the relationship between different elements content in soil and plant. The results showed that the elements, Ca, Mg, Na, K, N, P, Mn, Zn and Cr, were significantly positively correlated, between the soil and the plant. 展开更多
关键词 Heavy Metals WASTEWATER SUGARCANE enrichment factor
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Distribution, Enrichment and Accumulation of Heavy Metals in Soil and <i>Trigonella foenum-graecum</i>L. (Fenugreek) after Fertigation with Paper Mill Effluent 被引量:1
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作者 Vinod Kumar Ashok Kumar Chopra 《Open Journal of Metal》 2013年第2期8-20,共13页
The aim of the study was to investigate distribution, enrichment and accumulation of heavy metals in soil and Trigonella foenum-graecum (var. Pusa Early Bunching) after fertigation with paper mill effluent. Doses of p... The aim of the study was to investigate distribution, enrichment and accumulation of heavy metals in soil and Trigonella foenum-graecum (var. Pusa Early Bunching) after fertigation with paper mill effluent. Doses of paper mill effluent viz. 5%, 10%, 25%, 50%, 75% and 100% were used for fertigation of T. foenum-graecum along with bore well water (control). The results revealed that paper mill effluent had significant (P +, K+, Ca2+, Mg2+, Fe2+, TKN, PO3-4, SO2-4, Cd, Cr, Cu, Mn and Zn of the soil in both seasons. Insignificant (P > 0.05) changes in WHC and bulk density of the soil were observed after irrigation with paper mill effluent. The agronomical performance of T. foenum-graecum was increased from 5% to 25% concentration and decreased from 50% to 100% concentration of paper mill effluent as compared to control in both seasons. The heavy metals concentration was increased in T. foenum-graecum from 5% to 100% concentrations of paper mill effluent in both seasons. Biochemical components like crude proteins, crude fiber and crude carbohydrates were found maximum with 25% paper mill effluent in both seasons. The enrichment factor (Ef) of various heavy metals was in order of Cd > Mn > Cr > Cu > Zn > Fe for soil and Mn > Cu > Cr > Cd > Zn > Fe for T. foenum-graecum plants after fertigation with paper mill effluent. Therefore, paper mill effluent can be used as a biofertigant after appropriate dilution to improve yield of T. foenum-graecum. 展开更多
关键词 TRIGONELLA foenum-graecum Agronomical Characteristics enrichment factor FERTIGATION Heavy Metals Paper Mill efFLUENT
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Molecular mechanisms underlying the neuroprotection of environmental enrichment in Parkinson’s disease 被引量:4
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作者 Tamara Andrea Alarcón Sarah Martins Presti-Silva +2 位作者 Ana Paula Toniato Simões Fabiola Mara Ribeiro Rita Gomes Wanderley Pires 《Neural Regeneration Research》 SCIE CAS CSCD 2023年第7期1450-1456,共7页
Parkinson’s disease is the most common movement disorder,affecting about 1%of the population over the age of 60 years.Parkinson’s disease is characterized clinically by resting tremor,bradykinesia,rigidity and postu... Parkinson’s disease is the most common movement disorder,affecting about 1%of the population over the age of 60 years.Parkinson’s disease is characterized clinically by resting tremor,bradykinesia,rigidity and postural instability,as a result of the progressive loss of nigrostriatal dopaminergic neurons.In addition to this neuronal cell loss,Parkinson’s disease is characterized by the accumulation of intracellular protein aggregates,Lewy bodies and Lewy neurites,composed primarily of the proteinα-synuclein.Although it was first described almost 200 years ago,there are no disease-modifying drugs to treat patients with Parkinson’s disease.In addition to conventional therapies,non-pharmacological treatment strategies are under investigation in patients and animal models of neurodegenerative disorders.Among such strategies,environmental enrichment,comprising physical exercise,cognitive stimulus,and social interactions,has been assessed in preclinical models of Parkinson’s disease.Environmental enrichment can cause structural and functional changes in the brain and promote neurogenesis and dendritic growth by modifying gene expression,enhancing the expression of neurotrophic factors and modulating neurotransmission.In this review article,we focus on the current knowledge about the molecular mechanisms underlying environmental enrichment neuroprotection in Parkinson’s disease,highlighting its influence on the dopaminergic,cholinergic,glutamatergic and GABAergic systems,as well as the involvement of neurotrophic factors.We describe experimental pre-clinical data showing how environmental enrichment can act as a modulator in a neurochemical and behavioral context in different animal models of Parkinson’s disease,highlighting the potential of environmental enrichment as an additional strategy in the management and prevention of this complex disease. 展开更多
关键词 ACETYLCHOLINE brain-derived neurotrophic factor DOPAMINE environment enrichment gamma-aminobutyric acid glial cell line-derived neurotrophic factor GLUTAMATE molecular mechanisms Parkinson’s disease
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The enrichment characteristics and geological controlling factors of coalbed methane occurrence in Laochang area, Yunnan Province
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作者 WU Cai-fang CHEN Zhao-ying +1 位作者 WANG Cong JIANG Wei 《Journal of Coal Science & Engineering(China)》 2012年第4期355-361,共7页
The enriched characters of methane content in the main coal seam of Yunnan's Laochang coal mine was analyzed through combined with the geologic conditions of the research area: structure type, hydrogeology condition... The enriched characters of methane content in the main coal seam of Yunnan's Laochang coal mine was analyzed through combined with the geologic conditions of the research area: structure type, hydrogeology condition, coal reservoir's macerals, ash, water content, and so on. The geology factors of controlling gas in Laochang coal mine were illustrated; and the different geology models of controlling gas of geologic condition coupling were posed. Research shows that, in the region, the methane contents of the main coal seams decrease gradually from middle to all around it; the northeast and southeast is higher than the west. In the local area, the methane content of anticline axis is higher, and the gas content is reduced to both wings and plunging crown. On macroscopic view, the distribution of methane content in coal-beds was controlled by structural type. On microscopic view, the methane content in coal-beds is mainly involved in coal reservoir's macerals, ash content, and water content. The enriched characters of CBM in the research area are mainly the result of structure-hydrogeology-petrophysics coupling controls of CBM. On the basis of above analysis, according to the distribution character of methane content in coalbeds, the research area was divided into low gas area, middle gas area, and high gas area. 展开更多
关键词 coalbed methane enrichment characteristics cotrolling factor Laochang area gas content geological condition
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四川盆地下寒武统筇竹寺组海相页岩气高产井突破与富集模式 被引量:3
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作者 何骁 梁峰 +4 位作者 李海 郑马嘉 赵群 刘勇 刘文平 《中国石油勘探》 CAS CSCD 北大核心 2024年第1期142-155,共14页
多年来下寒武统筇竹寺组页岩气勘探开发进展缓慢,资201井获高产气流大大增加了该套页岩气规模商业化开发的信心,不同区域及层段富集规律差异及下一步勘探开发方向是筇竹寺组页岩开发面临的首要问题。以四川盆地57口钻井资料为基础,对多... 多年来下寒武统筇竹寺组页岩气勘探开发进展缓慢,资201井获高产气流大大增加了该套页岩气规模商业化开发的信心,不同区域及层段富集规律差异及下一步勘探开发方向是筇竹寺组页岩开发面临的首要问题。以四川盆地57口钻井资料为基础,对多口重点井的古生物、沉积、储层等特征进行分析,详细剖析资201井的部署理论依据、筇竹寺组页岩气富集条件及下一步勘探开发方向。从地层研究入手,建立了筇竹寺组地层划分标准,明确筇竹寺组主体发育4套深水陆棚相的富有机质页岩(①至④号层段),其分布受裂陷槽发育控制,裂陷槽内厚度最大。分析了页岩储层发育特征,指出储层压力、孔隙度、含气饱和度从下向上、从裂陷槽外到内呈现增大趋势,储层超压对页岩孔隙保存起到重要作用;基于此结合保存条件等建立了“多层异相、超压保孔”的页岩气超压差异富集模式,指出远离散失通道的超压孔隙发育区(层段)是页岩气富集有利区(层段)。文章指出资201井及周边是未来筇竹寺组页岩气增储上产的主要区域,资源量为8.06×10^(12)m^(3);川西地区具有相当的开发潜力,资源量为0.72×10^(12)m^(3);川南长宁及黔北一带受石墨化及构造活动影响,以寻找远离风化壳及地表露头的超压孔隙发育区为主。 展开更多
关键词 四川盆地 筇竹寺组 页岩展布 主控因素 富集模式 前景展望
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四川盆地南部地区五峰组—龙马溪组深层页岩气富集控制因素新认识 被引量:5
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作者 陈更生 石学文 +7 位作者 刘勇 吴伟 杨雨然 朱逸青 陈丽清 徐亮 钟可塑 殷樱子 《天然气工业》 EI CAS CSCD 北大核心 2024年第1期58-71,共14页
近年来,随着四川盆地五峰组—龙马溪组页岩气勘探开发迈向深层(埋深介于3500~4500 m),在四川盆地南部(下文简称川南)地区的泸州、长宁和渝西等区块深层页岩气不断取得了重要突破,展现了深层页岩气良好的开发前景。为了准确认识川南地区... 近年来,随着四川盆地五峰组—龙马溪组页岩气勘探开发迈向深层(埋深介于3500~4500 m),在四川盆地南部(下文简称川南)地区的泸州、长宁和渝西等区块深层页岩气不断取得了重要突破,展现了深层页岩气良好的开发前景。为了准确认识川南地区深层页岩在局部地区出现的低电阻率、高含水饱和度、测试微气现象,分别从页岩有机质成熟演化、页岩气源内运移特征和区域多期断裂活动影响等3个方面系统地分析了页岩气富集控制因素。研究结果表明:①高—过成熟度有机质石墨化造成了页岩电阻率和含气量明显降低,在有机质成熟度(Ro)大于3.6%以后,有机质生气能力衰竭,颗粒孔隙度明显降低,含水饱和度明显升高;②页岩气存在“源内侧向运移”特征,含气性与现今构造区带构造位置相对高低相关,表现为相对海拔高部位含气饱和度高,相对海拔低部位含气饱和度低;③Ⅰ级断裂对天然气的散失有显著的控制作用,建议距离Ⅰ级断裂1.5 km范围内勿部署实施井位,Ⅱ级断裂对含气性影响范围有限,距离Ⅱ级断层700 m以外时对页岩气体积压裂的影响较小。结论认为,充分考虑页岩有机质热演化程度、构造位置相对高低关系以及断裂发育特征等因素对深层页岩气富集的影响,有利于完善深层页岩气评价标准,对认识深层页岩气资源潜力以及优选有利区,具有重要现实意义,并可为推动实现深层页岩气规模增储和效益开发提供理论支撑。 展开更多
关键词 川南地区 五峰组—龙马溪组 深层页岩气 保存条件 富集规律 控制因素
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陆相拗陷湖盆细粒沉积有机质富集机制研究:以松辽盆地长岭凹陷青山口组为例 被引量:2
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作者 孟庆涛 张训 +9 位作者 杨亮 高家俊 刘招君 胡菲 邢济麟 张成铭 康嘉楠 崔博 董秦玮 张恩威 《古地理学报》 CAS CSCD 北大核心 2024年第2期401-415,共15页
松辽盆地作为白垩纪形成的大型陆相拗陷含油气盆地,沉积了巨厚的湖相细粒沉积,近年来在非常规油气方面展现了巨大的勘探潜力,其中青山口组是松辽盆地页岩油的重点攻关层系,细粒沉积有机质富集机制对于非常规油气勘探至关重要。在松辽盆... 松辽盆地作为白垩纪形成的大型陆相拗陷含油气盆地,沉积了巨厚的湖相细粒沉积,近年来在非常规油气方面展现了巨大的勘探潜力,其中青山口组是松辽盆地页岩油的重点攻关层系,细粒沉积有机质富集机制对于非常规油气勘探至关重要。在松辽盆地南部长岭凹陷分别选取位于不同沉积区的3口井,针对其青一段水进体系域的细粒沉积岩,借助岩心观察、有机地球化学和生物标志化合物等技术手段,讨论在不同沉积环境和水进过程中,有机质来源和有机质保存条件的变化,分析有机质富集的关键控制因素,并建立相关的有机质富集模式。结果表明:研究区青一段细粒沉积岩有机质丰度较高,有机质类型以Ⅱ型干酪根为主,整体呈现有机质丰度南低北高、下低上高的特征;饱和烃中正构烷烃主要表现为单峰、前峰型,具有微弱奇数碳优势;萜类化合物中以三环萜烷和五环三萜烷为主;甾类化合物中C_(27-29)规则甾烷以C_(27)规则甾烷丰度最高;芳香烃中三芴系列化合物以二苯并噻吩为主。研究区青一段细粒沉积岩有机质来源以湖泊内源菌藻类为主,含有一定的陆源高等植物输入,古水体整体为弱还原的半咸水环境。其中,有机质来源和古盐度是控制有机质富集的关键因素。在平面上,半深湖—深湖沉积区相较三角洲外前缘沉积区,受河流影响较弱,陆源输入较弱,水体盐度较高,有机质类型较好,有机质更加富集。在垂向上,随着水体加深,河流影响减弱,水体盐度呈升高的趋势,有机质类型变好,有机质富集。 展开更多
关键词 拗陷湖盆 细粒沉积 有机质富集 控制因素 青山口组一段 白垩系 长岭凹陷 松辽盆地
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高含水油井关停后剩余油再富集速度研究
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作者 孔维军 李立峰 +4 位作者 张建宁 苏书震 师国记 黄耀 张美丹 《断块油气田》 CAS CSCD 北大核心 2024年第3期503-511,共9页
高含水断块油藏开发末期构造高部位油井在关井一段时间后,会产生剩余油再富集现象。目前关于剩余油再富集速度的研究中,对剩余油运移过程的影响因素考虑不够全面,影响计算精度。针对该问题,在对运移中剩余油再富集受力分析的基础上建立... 高含水断块油藏开发末期构造高部位油井在关井一段时间后,会产生剩余油再富集现象。目前关于剩余油再富集速度的研究中,对剩余油运移过程的影响因素考虑不够全面,影响计算精度。针对该问题,在对运移中剩余油再富集受力分析的基础上建立小油滴状和柱状剩余油再富集速度模型,通过正交试验确立2种剩余油再富集速度的主要敏感因素,并建立了2种剩余油再富集速度及再富集时间图版。研究结果表明:存在驱替压差时,储层渗透率为影响2种剩余油再富集速度的主控因素;当储层渗透率一定,驱替压差的增大和原油黏度的减小有利于2种剩余油再富集速度的增大;同一注采井距位置处的小油滴距离孔隙中滞留柱状剩余油越近,聚集过程中剩余油再富集时间越长,但数值上增加不多。该研究对高含水油藏剩余油再富集潜力区评价具有借鉴意义。 展开更多
关键词 高含水油井 剩余油 再富集速度 敏感因素 储层渗透率
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氦气富集理论及富氦资源勘探思路
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作者 秦胜飞 窦立荣 +6 位作者 陶刚 李济远 齐雯 李晓斌 郭彬程 赵姿卓 王佳美 《石油勘探与开发》 EI CAS CSCD 北大核心 2024年第5期1160-1174,共15页
基于国内外重要含油气盆地天然气样品和岩石样品,进行氦气含量、组分、同位素及岩石样品中U、Th含量分析,对氦气富集机理、富集模式、分布规律和勘探思路等进行研究。研究认为,能否形成富氦气藏取决于气藏中氦气的供给量和天然气对氦气... 基于国内外重要含油气盆地天然气样品和岩石样品,进行氦气含量、组分、同位素及岩石样品中U、Th含量分析,对氦气富集机理、富集模式、分布规律和勘探思路等进行研究。研究认为,能否形成富氦气藏取决于气藏中氦气的供给量和天然气对氦气的稀释程度,其富集成藏特征可以概括为“多源供氦、主源富氦;氦氮伴生、同溶共聚”。氦气主要来自岩石中U和Th的放射性衰变,所有岩石都含有微量的U和Th,都可为气藏提供一定的氦源,但以花岗岩或变质岩为主的大型古老基底往往是富氦气藏的主力氦源。古老基底中的U和Th经历漫长地质历史时期的衰变生成的氦气连同基底岩石中无机含氮化合物裂解生成的氮气溶解在水中,随构造抬升,地层水沿断裂往上运移至气藏并释放出氦和氮气,使气藏同时富集氦和氮气,氦氮的伴生关系十分明显。在东部拉张型盆地,构造活动强烈,天然气中混有一定比例的幔源氦气。富氦气藏大多发育于有断裂沟通的古老基底之上、后期经历大幅度构造抬升、盖层封盖能力适中、天然气充注强度中等、地下水比较活跃的常压或低压区。氦气勘探须放弃以寻找天然气甜点和高产大气田的传统“兼探”思路,根据氦气富集特点,寻找有断裂并与古老基底沟通、晚期构造抬升幅度较大、盖层封盖能力相对较弱、天然气充注强度不高、古老地层水较丰富的气藏。 展开更多
关键词 氦气 富氦气藏 富集理论 分布规律 主控因素 勘探思路
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喀斯特地区尾矿库周边植物重金属富集特征及空间分布
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作者 韦岩松 农韦杰 +1 位作者 郑华明 李秀玲 《有色金属(矿山部分)》 2024年第4期133-141,共9页
目的:了解典型喀斯特地区尾矿库周边植物的重金属富集特性和空间分布特征,筛选优势植物品种。方法:计算富集系数来判断不同植物对不同重金属的富集能力;采用地理信息分析软件(GIS)通过普通克里金插值和半变异函数分析,建立植物重金属空... 目的:了解典型喀斯特地区尾矿库周边植物的重金属富集特性和空间分布特征,筛选优势植物品种。方法:计算富集系数来判断不同植物对不同重金属的富集能力;采用地理信息分析软件(GIS)通过普通克里金插值和半变异函数分析,建立植物重金属空间分布模型;计算皮尔逊相关系数,以分析植物体内各重金属之间及与土壤pH值的相关性。结果:该尾矿库周边28种植物中,茄科植物红丝线、菊科的野茼蒿和荨麻科的八角麻对Cd有较强富集能力,植物中Cd污染严重;乌毛蕨科的苏铁蕨、海金沙科的小叶海金沙和大戟科的禾串树对Pb有较强富集能力;各植物对Cu和Zn均无富集作用。重金属空间分布模型显示,Cd主要分布在尾矿库南面、西南面、东南面和西北面;Pb主要分布在东南部、坝下小溪及正南面;Cu主要分布在正南、西南和坝下小溪方向;Zn主要分布在西面、西南、西北和正北面。在半变异函数模型参数中,Cd和Zn以随机性因素误差为主,各点的空间相关性弱,Pb、Cu以结构性因素误差为主,空间相关性较强;植物体内重金属含量空间变异性和空间相关性排序为Zn<Cd<Cu<Pb。Cd与Cu存在中等程度正相关关系,Cd与Pb、Zn呈正弱相关关系;植物体内各重金属含量与土壤pH值相关性不强。结论:筛选出的部分优势植物可作为矿区土壤重金属富集转移和生物修复的备选品种,初步了解了该区域重金属在土壤和植物之间的迁移规律,为开展矿区重金属污染治理提供了依据。 展开更多
关键词 喀斯特地区 铅锌尾矿库 植物重金属富集 空间分布特征 富集系数
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