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| 1 | Numerical study of a dissipative micropolar fluid flow past an inclined porous plate with heat source/sink显示文摘Micropolar theories present an excellent mechanism for exploring new non-Newtonian materials processing provides a stimulating area for process engineering simulation.Motivated by area for process engineering applications,the present article presents the scope offinite element method in solving a mathematical model for magnetohydrodynamic,incom-pressible,dissipative and chemically reacting micropolar fluid flow and heat and mass transferthrough a porous medium from an inclined plate with heat sourcelsink has been investigated.For this purpose,the set of governing equations have been reframed and put into adimensionless form under the assumption of low Reynolds number with appropriatedimensionless quantities that can fit into the finite element fommulation.In addition tohighlighting the operational aspects of weighted residual scheme,a detailed investigation hasbeen camied out on the associated flow stnucture,heat and mass transfer.The evolution ofmany multi-physical parameters in these variables is illustrated graphically.Finite elementcode is benchmarked with the results reported in the literature to check the validity andaccuracy under some limiting cases and excellent agreement is seen with published solutionsand results of skin friction coefficient,couple stress coefficient,Nusselt number and Sherwoodnumber for invoked parameter are tabulated which shows that increasing heat sourcelsinkparameter elevates temperature.Chemical reaction parameter reduces velocity and concentra-tion gradients.Sherwood number enhances as chemical reaction parameter increases but reverse phenomena is observed in case of inclination of angle.Furthermore,a gridindependency test has been caried out for different grid sizes which has proven this methodis adequate. | Shamshuddin MD Thirupathi Thumma | 2019 | Propulsion and Power Research2019，8，1： | 2 |
| 2 | Mineralogy and factors controlling charge development of three Oxisols developed from different parent materials显示文摘 | Anda M Shamshuddin J Fauziah CI Omar SRS | 2008 | Geoderma2008，143，12： | 1 |
| 3 | Predicting N, P,K and organic depletion in soils using MPSIAC model at the Merek catchment, Iran 显示文摘 | HESHMATI M ARIFIN A SHAMSHUDDIN J | 2012 | Geoderma2012，17，： | 1 |
| 4 | Effects of adding organic materials to an acid sulfate soil on the growth of cocoa seedlings 显示文摘 | SHAMSHUDDIN J MUHRIZAL S FAUZIAH I | 2004 | science of the total environment2004，323，： | 1 |
| 5 | Effects of adding organic materials to an acid sulfate soil on the growth of cocoa seedlings 显示文摘 | SHAMSHUDDIN J MUHRIZAL S FAUZIAH I | 2004 | science of the total environment2004，323，： | 1 |
| 6 | Effects of adding organic materials to an acid sulfate soil on the growth of cocoa seedlings显示文摘 | Shamshuddin J Muhrizal S Fauziah I | 2004 | Science of The total Environment2004，323，： | 1 |
| 7 | Reactions of ground magnesium limestone and gypsum in soil with variable-charge minerals 显示文摘 | Shamshuddin J Ismail H | 1995 | American Journal of Soil Science Society1995，59，： | 1 |
| 8 | Transesterifieation of diethyl malonate with benzyl alco- hol catalyzed by modified zireonia: Kinetic study显示文摘 | Thimmaraju N Mohamod Shamshuddin S Z Pratap S R | 2014 | Jour-hal of Molecular Catalysis A: Chemical2014，391，： | 1 |
| 9 | 生物对流纳米流体流动的von Kármán分解法模拟(英文)显示文摘本研究分析了纳米流体从旋转圆盘中流过时的三维黏性时变旋流生物对流。圆盘的变形沿径向进行,同时考虑Stefan吹气,通过对Buongiorno纳米流体模型的分析,发现布朗运动和热泳动在纳米尺度上起着主导作用。在适当的壁面(圆盘表面)和自由流边界条件下,建立了原始质量守恒方程、径向动量、切向动量和轴向动量、热量、纳米粒子浓度和微生物密度函数。将这个高度非线性、强耦合的非定常偏微分方程系统用经典的von Kármán和其他变换进行归一化,从而将边值问题转化为一个常微分系统。产生的11阶系统包括多种无量纲流动参数,即生物对流Lewis数、不稳定参数、普通Lewis数、Prandtl数、质量对流Biot数、Peclet数、Stefan吹气参数。利用先进的半解析方法得到了系统的解,即Adomian分解法。利用Runge-Kutta拍摄技术计算的早期文献对上述问题进行了验证。 | M D SHAMSHUDDIN S R MISHRA O ANWAR BEG A KADIR | 2019 | Journal of Central South University2019，26，10： | 1 |
| 10 | Transesterification of diethyl malonate with benzyl alcohol catalyzed by modified zirconia: Kinetic study显示文摘 | N Thimmaraju S Z Mohamed Shamshuddin S R Pratap | 2014 | Journal of Molecular Catalysis A: Chemical2014，391，： | 1 |
| 11 | Changes in iron-poor acid sulfate soil upon submergence显示文摘 | Muhrizal S Shamshuddin J Fauziah I Husni MAH | 2006 | Geoderma2006，131，12： | 1 |
| 12 | Synthesis,characterization and catalytic activity studies on cordierite honeycomb coated with ZrO2 based solid super acids显示文摘 | S.Z Mohamed Shamshuddin M.Shyam Sundar N.Thimmaraju Venkatesh G.Vatsalya M.Senthilkumar | | 0，，9： | 1 |
| 13 | Transesterification: sal- ol synthesis over solid acids 显示文摘 | Shamshuddin S Z M Nagaraju N | 2006 | Catalysis Communica- tions2006，7，8： | 1 |
| 14 | Liquid phase transester- ification of methyl salicylate and phenol over solid acids: Kinetic studies 显示文摘 | Shamshuddin S Z M Nagaraju N | 2007 | Journal of Molecular Catalysis A: Chemical2007，273，12： | 1 |
| 15 | Effective acetylation of alcohols,phenols and amines over mesoporous aluminophosphate solid acids under solvent free conditions 显示文摘 | Shyamprasad K Shamshuddin S Z M Vasantha V T | 2014 | Journal of Porous Materials2014，21，6： | 1 |
| 16 | Preservation of organic matter in soils of a climobiosequence in the Main Range of Peninsular Malaysia显示文摘Limited information is available about factors of soil organic carbon(SOC) preservation in soils along a climo-biosequence. The objective of this study was to evaluate the role of soil texture and mineralogy on preservation of SOC in the topsoil and subsoil along a climo-biosequence in the Main Range of Peninsular Malaysia. Soil samples from the A and B-horizons of four representative soil profiles were subjected to particle-size fractionation and mineralogical analyses including X-ray diffraction and selective dissolution. The proportion of SOC in the 250-2000 μm fraction(SOC associated with coarse sand) decreased while the proportion of SOC in the <53 μm fraction(SOC associated with clay and silt)increased with depth. This reflected the importance of the fine mineral fractions of the soil matrix for SOC storage in the subsoil. Close relationships between the content of SOC in the <53 μm fraction and the content of poorly crystalline Fe oxides [oxalate-extractable Fe(Fe_o) – pyrophosphate-extractable Fe(Fe_p)] and poorly crystalline inorganic forms of Al [oxalateextractable Al(Al_o) – pyrophosphate-extractable Al(Al_p)] in the B-horizon indicated the importance of poorly crystalline Fe oxides and poorly crystalline aluminosilicates for the preservation of SOC in the Bhorizon. The increasing trend of Fe_o-Fe_p and Al_o-Al_p over elevation suggest that the importance of poorly crystalline Fe oxides and poorly crystalline aluminosilicates for the preservation of SOC in the Bhorizon increased with increasing elevation. This study demonstrates that regardless of differences in climate and vegetation along the studied climobiosequence, preservation of SOC in the subsoil depends on clay mineralogy. | Amir Hossein JAFARZADEH-HAGHIGHI Jusop SHAMSHUDDIN Jol HAMDAN Norhazlin ZAINUDDIN | 2017 | Journal of Mountain Science2017，14，9： | 0 |
| 17 | Chemical Weathering of New Pyroclastic Deposits from Mt. Merapi (Java), Indonesia显示文摘The Java Island, Indonesia with abundant amount of pyroclastic deposits is located in the very active and dynamic Pacific Ring of Fires. Studying the geochemical weathering indices of these pyroclastic deposits is important to get a clear picture about weathering profiles on deposits resulting from the eruption of Mt. Merapi. Immediately after the first phase of the eruption (March to June 2006), moist and leached pyroclastic deposits were collected. These pyroclastic deposits were found to be composed of volcanic glass, plagioclase feldspar in various proportions, orthopyroxene, clinopyroxene, olivine, amphibole and titanomagnetite. The total elemental composition of the bulk samples (including trace elements and heavy metals) was determined by wet chemical methods and X-ray fluorescence (XRF) analyses. Weathering of the pyroclastic deposits was studied using various weathering indices. The Ruxton ratio, weathering index of Parker, Vought resudual index and chemical index of weathering of moist pyroclastic deposits were lower than those of the leached samples, but the alteration indices (chemical and plagioclase) were slightly higher in the moist compared to the leached pyroclastic deposits. | Dian Fiantis Malik Nelson Eric Van Ranst Jusop Shamshuddin Nikolla P. Qafoku | 2009 | Journal of Mountain Science2009，6，3： | 0 |
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