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71篇 您的检索式:作者名="Sahay N"
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1肠道微生态失调与高血压的关系显示文摘新出现的证据表明,肠道菌群是维持生理动态平衡的关键,该研究旨在验证微生态失衡的肠道菌群与高血压相关这一假设,因为遗传、环境和膳食因素对肠道菌群和血压有很大影响。方法:从2种高血压模型大鼠和一个小队列患者人群的粪便样本中提取细菌DNA,用于细菌基因组的分析.刘莉 叶鹏 Yang T Santisteban MM Rodriguez V Li E Ahmari N Carvajal JM Zadeh M Gong M Qi Y Zubcevic J Sahay B Pepine CJ Raizada MK Mohamadzadeh M 2015中华高血压杂志2015,23,5:4
2反思金融深化:新兴市场的稳定与发展显示文摘有深度和流动性良好的金融系统,加上有丰富的金融工具可抵御金融冲击,还可以增加一国金融的稳定性。但是金融发展或许存在一个边界,越过此边界进一步发展其收益或将下降。本文通过研究新兴市场发现:一、大部分新兴市场金融进一步发展仍然对经济的增长和稳定有利。二、金融发展对经济增长的促进作用是倒U型的,在越过高点之后金融深化对要素生产率的促进作用将下降。三、如果金融发展过快,快速深化的金融产业可能引发经济和金融动荡。四、提升金融稳定与金融发展之间没有太大冲突,更好的金融监管有助于提升金融稳定,促进金融发展。五、发展金融机构或金融市场不存在通用的顺序,尽管前者对经济的作用在下降而后者在上升。IMF课题组 Ratna Sahay Martin Cihak Papa N’Diaye Adolfo Barajas Ran Bi Diana Ayala Yuan Gao Annette Kyobe Lam Nguyen Christian Saborowski Katsiaryna Svirydzenka Seyed Reza Yousefi 胡妍斌 王辰 2015新金融2015,0,10:2
3A Model of Surface Site Types on Oxide and Silicate Minerals Based on Crystal Chemistry: Implications for Site Types and Densities, Multi- Site Adsorption, Surface Infrared Spectroscopy, and Dissolution Kinetics显示文摘Koretsky C M Sverjensky D A Sahai N 1998Am J Sci1998,298,5:1
4Alkaline lipase from a novel strain Burkholderia multivorans: statistical medium optimization and production in a bioreactor显示文摘Gupta N Sahai V Gupta R 2007Process Biochemistry2007,42,:1
5GEOSURF: A computer program for modeli ngadsoption on mineral surface from aqueous solution 显示文摘Sahai N Sverjensky D A 1998Computers & Geosci ences1998,24,9:1
6Arene ruthenium complexes incorporating immine/azine hybrid-chelating N- N' donor ligands: Synthetic, spectral, structural aspects and DFT studies 显示文摘 Manish C Abhaya N Sahay 2004Journal of Organometallic Chemistry2004,689,:1
7Piriformospora indica, a cultivable plant-growth-promoting root endophyte 显示文摘Varma A Verma S Sahay N 1999Applied and Environmental Microbiology1999,65,:1
8Effect of media components on cell growth and bacterial cellulose production from Acetobacter aceti MTCC 2623显示文摘Dayal M S Goswami N Sahai A 2013Carbohydrate Polymers2013,94,:1
9Theoretical prediction of single sitesurface-protonation equilibrium constants for oxides and silicates in water显示文摘Sverjensky D A Sahai N 1996Geochimica et Cosmochimica Acta1996,60,:1
10Critical temperature-an approach to define proneness of coal towards spontaneous heating 显示文摘Sahay N Varma N K Ahmad I Sinha V K 2007Journal of Mines Metals and Fuels2007,55,10:1
11Antifertility and cannibalistic properties of some mycotoxins in albino rats 显示文摘Choudhary D N Sahay G R Singh J N 1994J Food Sci Technol1994,31,:1
12Painting with A Molecular Brush:Genomics/Proteomic Interfacing to Define the Drug Action Profile of Novel Solid-tumor Selective Anticancer Agents显示文摘Nakeff A Sahay N Pisano M 2002Cytometry2002,47,1:1
13Alkaline lipase from a novel strain Burkholderia multivorans: statistical medium optimization and production in a bioreactor显示文摘GUPA N SAHAI V GUPTA R 2007Process Biochem2007,42,:1
14A comprehensive review of direct borohydride fuel cells显示文摘Ma J Choudhury N A Sahai Y 0,,01:1
15A model of surface site types on oxide and silicate minerals based on crystal chemistry: Implications for site types and densities, multi- site adsorption, surface infrared spectroscopy, and dissolution kinetics 显示文摘Koretsky C M Sverjensky D A Sahai N 1998Am J Sci1998,298,5:1
16Evaluation of internally consistent parameters for the triple-layer model by the systematic analysis of oxide surface titration data显示文摘Sahai N Sverjensky D A 1997Geochim Cosmochim Acta1997,61,14:1
17Theoretical prediction of single-site surface-protonation equilibrium constants for oxides and silicates in water显示文摘Verjensky D A Sahai N 1996Geochimica et cosmochimica Acta1996,60,:1
18Is silica really an anomalous oxide? Surface acidity and aqueous hydrolysis revisited 显示文摘Sahai N 2002Environ Sci Technol2002,36,3:1
19Spectral response of rice cropand its relation to yield and yield attributs显示文摘PATEL N K SINGH T P SAHAI B 1985International Journal ofRemote Sensing1985,6,5:1
20Piriformospora indica,a cultivable plant-growth-promoting root endophyte显示文摘Varma A Verma S Sahay N 0,,06:1
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