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敦煌辐射校正场方向反射特性测量与评价   总被引:1,自引:0,他引:1  
何积泰  陆亦怀 《遥感学报》1997,1(4):246-251
和为中国遥感卫星辐射校正场项目的前期准备工作,于1994年6月和1996年9月,利用自知研制的智能型野外双向反射特征性面测量系统--VF921对敦煌辐射校正场地面方向反射特性(BROF)进行了测量。通过对这两次测量数据的处理和分析,对场地地BROF特性进行了分析和评价。同时,对于整个测量系统和数据获取与处理中还存在的问题进行了讨论。  相似文献   
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Zhang  Yihuai  Lebedev  Maxim  Smith  Gregory  Jing  Yu  Busch  Andreas  Iglauer  Stefan 《Natural Resources Research》2020,29(3):1787-1800

Characterization of coal micro-structure and the associated rock mechanical properties are of key importance for coal seam exploration, coal bed methane development, enhanced coal bed methane production and CO2 storage in deep coal seams. Considerable knowledge exists about coal chemical properties, but less is known about the nanoscale to the micro-scale structure of coals and how they change with coal strength across coal ranks. Thus, in this study, 3D X-ray micro-computed tomography (with a voxel size of 3.43 µm) and nano-indentation tests were conducted on coal samples of different ranks from peat to anthracite. The micro-structure of peats showed a well-developed pore system with meso- and micro-pores. The meso-pores essentially disappear with increasing rank, whereas the micro-pores persist and then increase past the bituminous rank. The micro-fracture system develops past the peat stage and by sub-bituminous ranks and changes into larger and mature fracture systems at higher ranks. The nano-indentation modulus showed the increasing trend from low- to high-rank coal with a perfect linear relationship with vitrinite reflectance and is highly correlated with carbon content as expected.

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