2) collective cultivation
整体培养
1.
At a high level, such creation and innovation of higher education forms the basis of the country in this field and therefore, must follow some important principles: individuality cultivation, collective cultivation, dynamic development and practicality.
我国高等教育的创新是高层次的创新 ,是国家创新体系的支柱和基础 ,它的创新可遵循一些基本原则 ,其中最主要的是个性培养原则、整体培养原则、动态化原则、实践性原则
3) the holistic training
整体化培养
4) mixed culture
混合培养
1.
Comparison of composition of cellulase from monoculture of Trichoderma with mixed culture with yeast or Aspergillus;
木霉及其混合培养酵母和曲霉产生的纤维素酶系的比较研究
2.
Study on the conditions and growth relationships of mixed culture of multi-strains;
多菌种微生物混合培养的条件及生长关系研究
3.
It was found that the ability of flocculating kaolin suspension by the culture broth produced by mixed culture of the two strains in the proportion of 1∶1 was higher than that of pure culture of either strain.
将两株絮凝剂产生菌分别纯培养及以体积比1∶1比例混合培养,发现混合培养发酵液对高岭土悬浊液的絮凝效果优于各菌株的纯培养发酵液。
5) coculture
联合培养
1.
The effect of vascular smooth muscle cells on the adhesion,proliferation and morphology of endothelial progenitor cells in a coculture system;
血管平滑肌细胞对联合培养内皮祖细胞黏附、增殖与形态的影响
2.
In coculture group this immunoreactivity became stronger.
结果显示:各组感觉神经元均产生免疫阳性反应,雪旺氏细胞条件培养基和巨噬细胞条件培养组免疫反应强度与对照组相同,联合培养组免疫反应为强阳性,与巨噬细胞条件培养组相比差别高度显著(P<0。
3.
In this study the influence of shear stress and vascular smooth muscle cells (VSMCs) on the differentiation of EPCs, as well as a role of Akt was detected in a coculture model.
应用EPCs与VSMCs联合培养的平行平板流动腔系统,对EPCs施加5 dynes/cm2切应力,观测切应力和VSMCs对EPCs分化的影响。
6) co-culture
联合培养
1.
Effect of fibroblasts in co-culture model on smooth muscle cell proliferation and morphology;
联合培养的成纤维细胞对平滑肌细胞增殖和形态的影响
2.
Effect of endothelial cell in co-culture model on smooth muscle cell proliferation and morphology;
联合培养的内皮细胞对平滑肌细胞增殖和形态的影响
3.
Differentiation of Bone Marrow Mesenchymal Stem Cells Co-cultured with Endothelial Cells under Shear Stress
剪切应力下与内皮细胞联合培养的骨髓间充质干细胞的分化
补充资料:不整合
不整合 unconformity 上下两套不同时代地层之间出现过沉积间断或地层缺失的地层接触关系。地层不连续,古生物演化顺序也是不连续的,由此确定岩层的时代也是不连续的。地层剖面中的岩层是现存的地层部分,而不整合则是缺失的地层部分。不整合一般分为角度不整合和假整合(又称平行不整合)等类型。前者是两套地层呈一定角度接触,中间为一侵蚀面(即不整合面),说明在前一套地层沉积后,有一次大的构造运动和海陆变化,然后地壳再次下沉又沉积了后一套地层。后者是两套地层大体呈平行接触,中间为一侵蚀面(即不整合面),说明在前一套地层沉积过程中有一次较大的地壳上升或海退运动以后地壳再次拗陷,沉积了后一套地层。识别和鉴定不整合的证据:①地层自然记录缺失的间隔证据,包括古生物自然记录的间断和地层自然记录的间断。②侵蚀的证据,包括构造不一致和地形不规则。③古陆表面的证据,包括风化面、古土壤、底砾岩等。不整合研究具有广泛意义,它是造山幕建立或构造旋回划分、岩石地层单位划分的重要依据。 |
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条