|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | 小麦谷蛋白亚基的组成及含量与谷蛋白聚合体大分子的关系及其对面包烘焙品质的影响显示文摘含有高分子量谷蛋白亚基 (HMW -GS) 5 + 10的生物型小麦与 2 + 12的生物型小麦相比 ,前者谷蛋白具有更大的分子量分布。高低分子量谷蛋白亚基的比例对于谷蛋白聚合体分子量的大小起着重要的作用 ,谷蛋白聚合体的体积越大 ,含有的高低分子量谷蛋白亚基的比例越高。SDS非可溶性谷蛋白含有较高比例的高低分子量谷蛋白亚基 ,并且其分子量要比可溶性谷蛋白聚合体的大。谷蛋白聚合体分子量分布的差异是不同小麦品种面包烘焙品质存在差异的重要因素。 | 王凤成 朱金宝 K.Khan L.O’Brien 陈万义 | 2004 | 中国粮油学报2004，19，3： | 12 |
| 2 | 'Rewriting'Cultural Safety within the Postcolonial and Postnational Feminist Project:Toward New Epistemologies of Healing显示文摘 | Anderson J.P J.Perry C.Blue A.Henderson and K.Khan | | 0，，03： | 1 |
| 3 | Upper mantle anisotropy inferred from shear wave splitting beneath the Eastern Indian Shield region显示文摘We estimate the shear wave splitting parameters vis-a-vis the thicknesses of the continental lithosphere beneath the two permanent seismic broadband stations located at Dhanbad(DHN) and Bokaro(BOKR) in the Eastern Indian Shield region. Broadband seismic data of 146 and 131 teleseismic earthquake events recorded at DHN and BOKR stations during 2007-2014 were analyzed for the present measurements.The study is carried out using rotation-correlation and transverse component minimization methods. We retain our 'Good', 'Fair' and 'Null' measurements, and estimate the splitting parameters using 13 'Good' results for DHN and 10 'Good' results for BOKR stations. The average splitting parameters(φ,δt)for DHN and BOKR stations are found to be 50.76°±5.46° and 0.82±0.2 s and 56.30°±5.07° and0.95 ± 0.17 s, and the estimated average thicknesses of the anisotropic layers beneath these two stations are ~94 and ~109 km,respectively. The measured deviation of azimuth of the fast axis direction(0)from the absolute motion of the Indian plate ranges from ~8° to 14°. The measured deviation of azimuth of the fast axis direction(0) from the absolute motion of the Indian plate ranges from ~8° to 14°. The eastward deviation of the fast axis azimuths from absolute plate motion direction is interpreted to be caused by induced outflow from the asthenosphere. Further, the delay time found in the present analysis is close to the global average for continental shield areas, and also coherent with other studies for Indian shield regions. The five 'Null' results and the lower delay time of ~0.5-0.6 s might be indicating multilayer anisotropy existing in the mantle lithosphere beneath the study area. | Kuntal Bhukta Prosanta K.Khan Prantik Mandal | 2018 | Geoscience Frontiers2018，9，6： | 1 |
| 4 | Testing the intraplate origin of mega-earthquakes at subduction margins显示文摘灾难性的 Mw 9.3 (地震时刻 1. | Prosanta K.Khan Partha Pratim Chakraborty G.Tarafder S.Mohanty | 2012 | Geoscience Frontiers2012，3，4： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员