白云石化作用及白云岩储层研究进展   总被引：1，自引：0，他引：1  

黄擎宇  刘伟  张艳秋  石书缘  王坤 《地球科学进展》2015,30(5):539-551

白云石化作用和白云岩储层一直都是碳酸盐岩研究中的重要领域。近年来,随着实验分析技术的进步以及油气勘探的深入,对白云岩的研究也取得了诸多进展:1数值模拟技术逐步应用到白云岩研究中,实现了白云石化模式研究由定性到定量的转变;2对微生物白云石化的研究不断加强,识别出了微生物相关白云石的特殊显微形貌特征并对其生物矿化机制进行了分析;3对已有白云石化模式的重新审视:包括对混合水白云石化的修正、对回流白云石化的扩展以及对构造—热液白云石化模式的丰富;4在白云石化与孔隙相关关系的研究中,突破了白云石化增孔的传统认识,逐步强调白云石化在孔隙保存方面的作用;5注重研究白云岩结构、成岩环境、原始相带以及白云岩形成之后的溶蚀改造等因素对白云岩储层发育的控制作用。在未来的研究中,应加强3个方面内容,一是对白云岩结构演化规律的定量研究,二是在成岩流体示踪方面要加强对新技术手段(如二元同位素、Mg同位素)的使用,同时注意借鉴成矿流体研究中的成熟技术和方法,三是要加强对深部白云岩储层形成和保存机制的探索。  相似文献   

全球海洋人为碳储量估算及时空分布研究进展     

Huang Peng  Chen Liqi  Cai Minggang 《地球科学进展》2015,30(8):952-959

海洋是全球最大的碳汇,确定海洋中人为碳含量及其时空变化是一件具有挑战性的工作。就当前海洋人为碳含量确定方法、人为碳储量及其随时间变化进行综述总结。研究表明海洋仍然可以吸收并储藏大量的人为碳,但未来对于海洋吸收储藏人为碳的研究仍具有诸多不确定性。已有证据表明稳态海洋的概念不完全正确,需要在非稳态条件下重新定义人为碳并开展研究。同时需要积累更多的观测数据,采用包括观测和模式模拟等手段来研究不同时间尺度的人为碳的吸收和储藏过程。  相似文献   

Assessment of Constraint Factors of Resources and Environment of Sustainable Development in the Beijing-Tianjin-Hebeiregion: Based on the Framework of Landscape Sustainability Science     

Zhang Da  He Chunyang  Wu Jianguo  Huang Qingxu 《地球科学进展》2015,30(10):1151-1161

The Beijing-Tianjin-Hebei (BTH) region is an important engine for China’s socioeconomic development. Timely and effectively assessing constraint factors of resources and environment is of great significance for the sustainability assessment and the sustainable development of this region. However, comprehensive assessment research considering key resource and environmental constraints are still lacking. In this study, therefore, the limiting factors of resources and the environment in the BTH region were assessed based on the framework of landscape sustainability science. First, we chose five limiting factors, including topographic condition, geological environment, water resource, land resource, and atmospheric environment, to assess the constraints of resources and the environment using the single-factor evaluation method and the multi-factor comprehensive evaluation method. Based on the results, we divided the whole region into five subregions, i.e., the ecological conservation subregion, the geological disaster subregion, the water resource scarcity subregion, the atmospheric pollution subregion, and the cropland protection subregion. The results revealed that the northern BTH region was highly constrained by topographic conditions, the central BTH region was strongly constrained by geological environment and water resources, whereas the southern BTH region was constrained mainly by land resources and atmospheric environment. In addition, water resource was the main limiting factor for regional population growth and economic development. In 2010, the water resource scarcity subregion had a total population of 39.59 million, an urban population of 76.90%, and a gross domestic product of 2 455.57 billion yuan. We argue that the sustainable development of the BTH region should explicitly consider the resource and environmental limiting factors, implement land use optimization according to local conditions, maintain multiple land use types and diverse management strategies, based on the perspective of “strong sustainability”, so as to promote the regional sustainable development.  相似文献   

The Paleoceanography during the Time with High δ13C of Phanerozoic marine carbonates     

Huang Sijing  Li Xiaoning  Wu Wenhui  Zhang Meng  Hu Zuowei  Liu Sibing  Huang Keke  Zhong Yijiang 《地球科学进展》2015,30(11):1185-1197

Carbon isotopic composition of marine carbonates is a record for various important geological events in the process of earth development and evolution. The carbonates of Carboniferous, Permian and Triassic, as the transition from Paleozoic to Mesozoic-Cenozoic have very high ¹³C value. Taking this as the main point, and combined with the oxygen, strontium isotopic composition in carbonates, distribution of carbonate basin area through geologic time, the correlation of carbon isotopic composition of marine carbonates to sea level change, organic carbon burial flux, exchange of CO₂ content in atmosphere and ocean, and long cycle evolution of the earth ecosystems were approached. The results are shown as follows: ①The interval of ¹³C >3‰ during Phanerozoic was concentrated in Carboniferous, Permian and the beginning of Triassic, but the beginning of Triassic was characterized by higher frequency and larger fluctuations in ¹³C value during a short time, whereas the Carboniferous-Permian presented a continuously stable high ¹³C value, indicating a larger amount of organic carbon accumulation in this time interval. Relatively high ¹⁸O values during this time was also observed, showing a long time of glaciations and cold climate, which suggest a connection among rapid organic carbon burial, cold climate, as well as pCO₂ and pO₂ states of atmosphere. ②The over consumption of atmosphere CO₂ by green plants during the time with high ¹³C of seawater forced CO₂ being transferred from ocean to atmosphere for the balance, but the decrease in the seawater amount and water column pressure caused by the global cooling could weaken dissolution capacity of CO₂ in seawater and carbon storage of marine carbonates, and also reduce the carbonate sedimentary rate and decrease the carbonate basin area globally from Devonian to Carboniferous and Permian. During the middle-late Permian carbonate was widely replaced by siliceous sediments even though in shallow carbonate platform, which resulted in the decrease of marine invertebrates, suggesting the Permian chert event should be global. ③The Phanerozoic ⁸⁷Sr/⁸⁶Sr trend of seawater showed a sharp fall in Permian and drop to a minimum at the end of the Permian, indicting input of strontium from the submarine hydrothermal systems (mantle flux). Such process should accompany with a supplement of CO₂ from deep earth to atmosphere and ocean system, but the process associated with widespread volcanism and rises of earth’s surface temperature pricked up the mass extinction during the time of end Permian. ④Cold climate and increase of continental icecap volume, the amalgamation of northern Africa and Laurentia continentals were the main reasons responsible for the sea level drop, but the water consumption result from the significantly increased accumulation of organic carbon should also be one of the reasons for the sea level drop on the order of tens of meters. ⑤The mass extinction at the end Permian was an inevitable event in the process of earth system adjustment. It was difficult for marine invertebrates to survive because of the continuously rapid burial of organic carbon, and of the decrease of sea water amount and its dissolution ability to CO₂. At last, at the end of Paleozoic, the supplement of CO₂ to atmosphere and ocean by widely magma activities resulted in a high temperature of earth surface and intensified mass extinction.  相似文献   

Effects of coring directions on the mechanical properties of Chinese shale     

Qiao Lyu  Ranjith PG  Xinping Long  Yong Kang  Man Huang 《Arabian Journal of Geosciences》2015,8(12):10289-10299

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河南省农作物虚拟水含量时空分异特征     

黄会平  曹明明  宋进喜  韩宇平  陈姗姗 《地域研究与开发》2015,(3):167-171,176

在GIS技术的支持下,通过对1978—2013年河南省冬小麦、夏玉米、花生、棉花、油料作物、蔬菜6种主要农作物虚拟水量的计算与分析,探讨了其时空分异规律。河南省6种农作物单位质量虚拟水量在不断下降的趋势下有波动,2003年出现峰值,与当年大旱、所有农作物大面积减产有关;在农作物类型中,棉花单位质量虚拟水含量最高,多年平均值达到8 077.4 m3/t,蔬菜最低,多年平均值仅为159.95 m3/t。6种作物的虚拟水含量在空间分布上有明显差异,按其2013年的产量进行加权分析得到,第一等级区域为三门峡、郑州、信阳,第二等级为平顶山、洛阳、济源、开封,第三等级为南阳、驻马店、新乡、鹤壁、安阳、濮阳,第四等级为漯河,最低为许昌、周口、商丘、焦作。从整体看,西部、南部虚拟水含量高,而北部、东部虚拟水含量低。  相似文献   

罗霄山区旅游扶贫效应的居民感知与态度研究——以湖南汝城国家森林公园九龙江地区为例     

蒋莉  黄静波 《地域研究与开发》2015,(4)

旅游扶贫应立足于贫困人口的获利和发展,其核心是使贫困人口从旅游开发中获得更多的发展机会和净利益。以居民感知理论为基础,对汝城国家森林公园九龙江地区居民进行问卷调查,采用因子分析法和数理统计法,分析当地居民对旅游扶贫效应的感知和态度。研究结果表明:当地居民对旅游扶贫的社会和经济效应感知明显,对环境效应不敏感,参与旅游业的意愿强,但受经济、文化等因素制约,实际参与能力不足。建议当地政府将旅游业培育成特色产业,以居民受益为出发点,对居民进行扶持与引导,鼓励居民参与旅游开发与决策,并注重资源开发与保护相结合,以期实现贫困人口脱贫和旅游发展的双赢。  相似文献   

北半球夏季中高纬度大气阻塞对北极海冰变化的影响          下载免费PDF全文

肖贻青 黄斌刁一娜  罗德海 《极地研究》2015,27(4):364-378

利用NCEP/NCAR再分析逐日500 h Pa高度场资料,对北半球夏季中高纬度大气阻塞特征进行统计分析,发现大气阻塞活动频率高的地区主要集中在白令海峡区域、鄂霍次克海区域、欧亚大陆区域及格陵兰区域。而通过NSIDC提供的卫星观测资料发现近30年夏季海冰容易减少的区域正好对应阻塞活动北部的高纬度地区。分别通过对以上4个区域有阻塞发生相对没有阻塞发生时的500 h Pa位势高度场、地面温度场、850 h Pa经向瞬变热通量输送和平流输送等异常变化场进行对比分析,结果发现夏季中高纬度阻塞频率的增加对海冰的减少有显著影响,主要体现在阻塞的发生发展可通过增加高纬度地面温度、对极地的热量输送和暖平流输送来加快海冰的融化。这种阻塞引起的热力作用在鄂霍次克海和欧亚大陆区域效果更为显著。  相似文献   

Effects of land-use changes on organic carbon in bulk soil and associated physical fractions in China's Horqin Sandy Grassland     

YuQiang Li  YinPing Chen  ShaoKun Wang  WenDa Huang  JianPeng Zhang 《寒旱区科学》2015,7(1):0050-0058

The Horqin Sandy Grassland is one of the most seriously desertified areas in China's agro-pastoral ecotone due to its fragile ecology, combined with improper and unsustainable land management. We inves...  相似文献   

Large deformation failure analysis of the soil slope based on the material point method     

Peng Huang  Shun-li Li  Hu Guo  Zhi-ming Hao 《Computational Geosciences》2015,19(4):951-963

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