Citation: | Yi-wen Ju, Cheng Huang, Yan Sun, Cai-neng Zou, Hong-ping He, Quan Wan, Xue-qiu Wang, Xian-cai Lu, Shuang-fang Lu, Jian-guang Wu, Hong-tai Chao, Hai-ling Liu, Jie-shan Qiu, Fei Huang, Hong-jian Zhu, Jian-chao Cai, Yue Sun, 2018. Nanogeology in China: A review, China Geology, 1, 286-303. doi: 10.31035/cg2018020 |
Nanogeology is a subject that is a combination of geology and nanoscale science, and it has been a frontier field in recent years. It is also a new subject with the features of intersectionality and multidisciplinary. Digging deeper into geological problems and nanoscale phenomena helps better revealing the more essential mechanisms and processes in geological science, which is also an evitable path in the development of geology. In this paper, we elaborate the concept, feature and main subdisciplines, and summarize three stages of nanogeology development from preliminary research in the 1990s to subject formation in China. After summarizing the researchers’ achievements in this field, we illustrate some primary research progresses of nanogeology in China as eight subdisciplines. On the basis of the above content, we propose the development prospect of nanogeology in China. There are many geologic problems with scientific values and economic benefits, such as research of geologic fundamental problems, resource exploration and development, mechanism study and prediction of geological activities (disasters), mechanism research and management of environmental pollution and others. Nanogeology has a great potential in China to solve all of these problems. As a result, the theories and methods of nanogeology will become enriching and advanced. It offers important theoretical basis and technological methods to deal with major issues concerning the national economy and the people's livelihoods, such as the prediction of geological activities, as well as resource distribution and its exploration and utilization.
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TEM images of (a) morphological and microstructure of nano-rod calcite from Quaternary loess; (b) microstructures of authigenic attapulgite from Lingtai red clay sequence (after Xie QQ et al., 2016).
TEM images of BCNTs prepared from coal (after Wang ZY et al., 2006). (a) an image showing abundant BCNTs; (b) two Y-junctions marked as A and B by black arrows, which are circled in square in (a).
(a) Nanometer hexagonal crystals of Cu–Ti alloy in geogas (after Wang WB et al., 2016). (b) TEM photomicrograph of spherical Pb-bearing particles (b) and cudgel Pb-bearing particle (c) (after Cao JJ et al., 2009).
SEM images of nanoparticles developed in ductile shear zones (after Liu HL et al., 2017). (a) the sample was paragneiss taken from Taroko ductile shear zone in Taiwan. The nano particles on paragneiss surface may be the products at granulating stage. (b) the sample was quartz schist taken from Xiaomei ductile shear zone in Hainan Island. Rubbed (wiped) ridge and groove (trench) constituted by nano particles in belt structure, indicating plastic flow (a-axis), where a-axis represents shear sliding direction. The small arrow represents for wiped ridge formed by accumulation of nano particles.
HRTEM images of tectonically deformed coals (after Ju YW et al., 2017). Brittle deformation: (a, b) basic structure units are scattered and isolated with small diameter and no directionality; small brightness of diffraction ring (002). Ductile deformation: (c, d) basic structure units are stripy and variegated with large diameter and strong directionality; dispersed brightness of diffraction ring (002).
Diagram of pore size in several representative unconventional oil and gas tight reservoirs (after Zou CN et al., 2011; Yang Z et al., 2015b).
SEM images of pores in shale and tight sandstone. Longmaxi Formation from Fuling shale gas field in Sichuan Basin (after Yang YF and Bao F, 2017): (a) BSE image, nanopores within bitumen; (b) SE image, pore-filled bitumen with numerous nanopores. Yanchang Formation from Ordos Basin (after Zou XH et al., 2013): (c) pores in the matrix of slate chloride; (d) organic pores.
Pictures of micro-nanometer grains on the slip surface of the Shaba fault gouge under SEM (after Yuan RM et al., 2014). (a) scattered ball-shaped grains; (b) inlaid elongated grains; (c) complexes of micro-nanometer grains with tension fractures and local tilt edge (marked by the white arrows); (d) worm-shaped (H), cake-shaped (E) and massive-shaped (G) complexes with tension fractures and local tilt edge (marked by the white arrows); loose region exited among these complexes (marked by dashed line).