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Publications by Si-Ya Xiao

A Climatological Interpretation of Precipitation-Based &Lt;i>&delta;18O Across Siberia and Central Asia

Earth System Dynamics Discussions

2019

English

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&Lt;sup>13C-&Lt;sup>18O Bonds in Precipitated Calcite and Aragonite: An &Lt;i>ab Initio Study

Open Journal of Geology

2014

English

Intel&reg; Math Kernel Library PARDISO* For Intel&reg; Xeon PhiTM Manycore Coprocessor

Applied Mathematics

2015

English

From &Lt;i>E = &Lt;i>mc2 To &Lt;i>E = &Lt;i>mc2/22—a Short Account of the Most Famous Equation in Physics and Its Hidden Quantum Entanglement Origin

Journal of Quantum Information Science

2014

English

Characterization of Six Categories of Systematic 2n－(n－k) Fractional Factorial Designs

Open Journal of Statistics

2014

English

Solutions of the Exponential Equation &Lt;i>yx/Y = &Lt;i>x Or Lnx/&Lt;i>x = Lny/&Lt;i>y And Fine Structure Constant

Journal of Applied Mathematics and Physics

2017

English

Comparison of Textural Characteristics of Ceria Solids Prepared via Triton X Reverse Micelles and &Lt;i>in Situ Synthesized Ce(OiPr)4 And Ce(OiPr) &Lt;sub>3 Precursors

Materials Sciences and Applications

2019

English

How Dry Was the Younger Dryas? Evidence From a Coupled &Lt;i>δ2H–δ18O Biomarker Paleohygrometer Applied to the Gemündener Maar Sediments, Western Eifel, Germany

English

C ∕ N Ratio, Stable Isotope (&Lt;i>δ13C, &Lt;i>δ15N), and &Lt;i>n-Alkane Patterns of Brown Mosses Along Hydrological Gradients of Low-Centred Polygons of the Siberian Arctic

Biogeosciences

Earth-Surface Processes

English

Characterization of NADase-Inactive NAD+ Glycohydrolase in &Lt;i>Streptococcus Pyogenes

Advances in Microbiology

2013

English

Amanote Research

Discover open access scientific publications

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Publications by Si-Ya Xiao

A Climatological Interpretation of Precipitation-Based &Lt;i>&delta;</I><sup>18</Sup>O Across Siberia and Central Asia

Related publications

&Lt;sup>13</Sup>C-&Lt;sup>18</Sup>O Bonds in Precipitated Calcite and Aragonite: An &Lt;i>ab Initio</I> Study

Intel<sup>&reg;</Sup> Math Kernel Library PARDISO<sup>*</sup> For Intel<sup>&reg;</Sup> Xeon Phi<sup>TM</Sup> Manycore Coprocessor

From &Lt;i>E</I> = &Lt;i>mc</I><sup>2</Sup> To &Lt;i>E</I> = &Lt;i>mc</I><sup>2</Sup>/22—a Short Account of the Most Famous Equation in Physics and Its Hidden Quantum Entanglement Origin

Characterization of Six Categories of Systematic 2<sup><i>n</I>－(<i>n</I>－<i>k</I>)</Sup> Fractional Factorial Designs

Solutions of the Exponential Equation &Lt;i>y</I><sup><i>x/Y</I></Sup> = &Lt;i>x</I> Or Ln<i>x</I>/&Lt;i>x</I> = Ln<i>y</I>/&Lt;i>y</I> And Fine Structure Constant

Comparison of Textural Characteristics of Ceria Solids Prepared via Triton X Reverse Micelles and &Lt;i>in Situ</I> Synthesized Ce(O<sup>i</Sup>Pr)<sub>4</Sub> And Ce(O<sup>i</Sup>Pr) &Lt;sub>3</Sub> Precursors

How Dry Was the Younger Dryas? Evidence From a Coupled &Lt;i>δ</I><sup>2</Sup>H–<i>δ</I><sup>18</Sup>O Biomarker Paleohygrometer Applied to the Gemündener Maar Sediments, Western Eifel, Germany

C ∕ N Ratio, Stable Isotope (&Lt;i>δ</I><sup>13</Sup>C, &Lt;i>δ</I><sup>15</Sup>N), and &Lt;i>n</I>-Alkane Patterns of Brown Mosses Along Hydrological Gradients of Low-Centred Polygons of the Siberian Arctic

Characterization of NADase-Inactive NAD<sup>+</sup> Glycohydrolase in &Lt;i>Streptococcus Pyogenes</I>

Amanote Research

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Publications by Si-Ya Xiao

A Climatological Interpretation of Precipitation-Based &Lt;i&gt;&amp;delta;&lt;/I&gt;&lt;sup&gt;18&lt;/Sup&gt;O Across Siberia and Central Asia

Related publications

&Lt;sup&gt;13&lt;/Sup&gt;C-&Lt;sup&gt;18&lt;/Sup&gt;O Bonds in Precipitated Calcite and Aragonite: An &Lt;i&gt;ab Initio&lt;/I&gt; Study

Intel&lt;sup&gt;&amp;reg;&lt;/Sup&gt; Math Kernel Library PARDISO&lt;sup&gt;*&lt;/sup&gt; For Intel&lt;sup&gt;&amp;reg;&lt;/Sup&gt; Xeon Phi&lt;sup&gt;TM&lt;/Sup&gt; Manycore Coprocessor

From &Lt;i&gt;E&lt;/I&gt; = &Lt;i&gt;mc&lt;/I&gt;&lt;sup&gt;2&lt;/Sup&gt; To &Lt;i&gt;E&lt;/I&gt; = &Lt;i&gt;mc&lt;/I&gt;&lt;sup&gt;2&lt;/Sup&gt;/22—a Short Account of the Most Famous Equation in Physics and Its Hidden Quantum Entanglement Origin

Characterization of Six Categories of Systematic 2&lt;sup&gt;&lt;i&gt;n&lt;/I&gt;－(&lt;i&gt;n&lt;/I&gt;－&lt;i&gt;k&lt;/I&gt;)&lt;/Sup&gt; Fractional Factorial Designs

Solutions of the Exponential Equation &Lt;i&gt;y&lt;/I&gt;&lt;sup&gt;&lt;i&gt;x/Y&lt;/I&gt;&lt;/Sup&gt; = &Lt;i&gt;x&lt;/I&gt; Or Ln&lt;i&gt;x&lt;/I&gt;/&Lt;i&gt;x&lt;/I&gt; = Ln&lt;i&gt;y&lt;/I&gt;/&Lt;i&gt;y&lt;/I&gt; And Fine Structure Constant

Comparison of Textural Characteristics of Ceria Solids Prepared via Triton X Reverse Micelles and &Lt;i&gt;in Situ&lt;/I&gt; Synthesized Ce(O&lt;sup&gt;i&lt;/Sup&gt;Pr)&lt;sub&gt;4&lt;/Sub&gt; And Ce(O&lt;sup&gt;i&lt;/Sup&gt;Pr) &Lt;sub&gt;3&lt;/Sub&gt; Precursors

How Dry Was the Younger Dryas? Evidence From a Coupled &Lt;i&gt;δ&lt;/I&gt;&lt;sup&gt;2&lt;/Sup&gt;H–&lt;i&gt;δ&lt;/I&gt;&lt;sup&gt;18&lt;/Sup&gt;O Biomarker Paleohygrometer Applied to the Gemündener Maar Sediments, Western Eifel, Germany

C ∕ N Ratio, Stable Isotope (&Lt;i&gt;δ&lt;/I&gt;&lt;sup&gt;13&lt;/Sup&gt;C, &Lt;i&gt;δ&lt;/I&gt;&lt;sup&gt;15&lt;/Sup&gt;N), and &Lt;i&gt;n&lt;/I&gt;-Alkane Patterns of Brown Mosses Along Hydrological Gradients of Low-Centred Polygons of the Siberian Arctic

Characterization of NADase-Inactive NAD&lt;sup&gt;+&lt;/sup&gt; Glycohydrolase in &Lt;i&gt;Streptococcus Pyogenes&lt;/I&gt;

A Climatological Interpretation of Precipitation-Based &Lt;i>δ</I><sup>18</Sup>O Across Siberia and Central Asia

&Lt;sup>13</Sup>C-&Lt;sup>18</Sup>O Bonds in Precipitated Calcite and Aragonite: An &Lt;i>ab Initio</I> Study

Intel<sup>®</Sup> Math Kernel Library PARDISO<sup>*</sup> For Intel<sup>®</Sup> Xeon Phi<sup>TM</Sup> Manycore Coprocessor

From &Lt;i>E</I> = &Lt;i>mc</I><sup>2</Sup> To &Lt;i>E</I> = &Lt;i>mc</I><sup>2</Sup>/22—a Short Account of the Most Famous Equation in Physics and Its Hidden Quantum Entanglement Origin

Characterization of Six Categories of Systematic 2<sup><i>n</I>－(<i>n</I>－<i>k</I>)</Sup> Fractional Factorial Designs

Solutions of the Exponential Equation &Lt;i>y</I><sup><i>x/Y</I></Sup> = &Lt;i>x</I> Or Ln<i>x</I>/&Lt;i>x</I> = Ln<i>y</I>/&Lt;i>y</I> And Fine Structure Constant

Comparison of Textural Characteristics of Ceria Solids Prepared via Triton X Reverse Micelles and &Lt;i>in Situ</I> Synthesized Ce(O<sup>i</Sup>Pr)<sub>4</Sub> And Ce(O<sup>i</Sup>Pr) &Lt;sub>3</Sub> Precursors

How Dry Was the Younger Dryas? Evidence From a Coupled &Lt;i>δ</I><sup>2</Sup>H–<i>δ</I><sup>18</Sup>O Biomarker Paleohygrometer Applied to the Gemündener Maar Sediments, Western Eifel, Germany

C ∕ N Ratio, Stable Isotope (&Lt;i>δ</I><sup>13</Sup>C, &Lt;i>δ</I><sup>15</Sup>N), and &Lt;i>n</I>-Alkane Patterns of Brown Mosses Along Hydrological Gradients of Low-Centred Polygons of the Siberian Arctic

Characterization of NADase-Inactive NAD<sup>+</sup> Glycohydrolase in &Lt;i>Streptococcus Pyogenes</I>