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| 1 | Monetary Policy and Corporate Investment:Evidence from Chinese Micro Data显示文摘This paper investigates how a firm’s characteristics restrict the influence of monetary policy changes on its investment behavior.Focusing on China ’s listed companies for a sample period from the first quarter of 2002 to the first quarter of 2011,we find that quantityoriented and price-based monetary policies have heterogeneous impacts on corporate investment behavior,but the influence of monetary policies is constrained by the liquidity, inventory,size and asset-liability ratio of a firm.Firms with higher liquidity,lower inventory level and lower asset-liability ratios are less sensitive to the impact from two kinds of monetary policies.The larger the size of the firm,the less it is subject to influence from quantity-oriented monetary policy;it responds more to price-based monetary policy.The policy implication is that the monetary authorities should pay attention to the importance of policy-making based on the monetary demand of microeconomic entities. | Ying Sophie Huang Frank M.Song Yizhong Wang | 2012 | China & World Economy2012，20，5： | 12 |
| 2 | Interest Rate Pass-through in a Dual-track System:Evidence from China显示文摘Using the Phillips-Loretan approach,this paper verifies the degree and speed of passthrough and rigidity of different interest rates in China,as well as the response of private loan interest rates to other interest rates during 2002-2012.The results indicate that the long-term pass-through from the interbank offered rates and deposit and loan interest rates to the treasury bond rate is incomplete,but that the long-term pass-through to private loan interest rates is overshooting.The long-term pass-through from the deposit and loan interest rates to the overnight interbank offered rate is incomplete,while that to the interbank offered rates of other maturities is complete.The short-term passthrough and adjustment speed of interest rates exhibit asymmetry.Therefore,before considering a full liberalization of interest rates,it is important to further enhance the competition of the financial system and the function of different interest rate systems,such as the interbank market and bond market. | Xuejun Jin Frank M.Song Yizhong Wang Yi Zhong | 2014 | China & World Economy2014，22，4： | 7 |
| 3 | Rapid and sensitive liquid chromatography-tandem mass spectrometry:assay development validation and application to a human pharmacokinetic study显示文摘 | M.Song L.Wang H.Zhao | | 0，，： | 1 |
| 4 | The determinants of capital structure:Evidence from China显示文摘 | Guihai HUANG Frank M.SONG | | 0，，： | 1 |
| 5 | 查看详情显示文摘 | H. Sim J.n Kim S. Lee M.Song D.Yoon D.Lim S.Hong | | 0，，： | 1 |
| 6 | China’s participation in the international RRT for I_(c) measurement of superconducting cables organized by IEC/TC90显示文摘Currently,IEC/TC90 is working on standardizing the method for measuring critical current(Ic)in superconducting cables.At the end of 2020,an international round robin test(RRT)was organized,in which five Chinese institutions participated,and four accomplished the test.The electric-field versus current(E-I)curves obtained by each institution are highly repeatable.Those obtained by different institutions are nearly identical after appropriate curve averaging,indicating high reproducibility,except the last participant's inner core curves.The discrepancy was later determined to be the result of sample cable damage.After excluding highly deviated data,it is determined that the maximum relative standard uncertainty in I_(c) is 0.7%,and the maximum relative standard uncertainty in n-value is 12.8%.The I_(c)values are comparable to Japan's domestic RRT results,but the n-values are significantly different.The test results support the DC four-terminal method as a recommended test method,with a target relative uncertainty of less than 2%for the Ic value. | J.Li Y.Shi G.M.Zhang L.W.Jing J.X.Zheng C.L.Liu W.Yuan Y.S.Wang M.Song Y.J.Xia X.H.Zong Y.W.Han D.N.Zheng X.J.Zhou T.Matsushita G.Nishijima | 2022 | Superconductivity2022，，1： | 0 |
| 7 | The Holocene environmental changes revealed from the sediments of the Yarkov sub-basin of Lake Chany,south-western Siberia显示文摘Lake Chany is the largest endorheic lake in Siberia whose catchment is entirely on the territory of Russia.Its geographical location on the climate-sensitive boundary of wet and dry landscapes provides an opportunity to gain more knowledge about environmental changes in the West Siberian interior during the Holocene and about the evolution of the lake itself.Sediment cores obtained from the Yarkov subbasin of the lake in 2008 have been comprehensively studied by a number of approaches including sedimentology and AMS dating,pollen,diatom and chironomid analyses(with statistical interpretation of the results),mineralogy of authigenic minerals and geochemistry of plant lipids(biomarker analysis.).Synthesis of new results presented here and published data provides a good justification for our hypothesis that Lake Chany is very young,no older than 3.6 ka BP.Before that,between 9 and 3.6 ka BP,the Chany basin was a swampy landscape with a very low sedimentation rate;it could not be identified as a water body.In the early lake phase,between 3.6 and 1.5 ka BP,the lake was shallow,1.2–3.5 m in depth,and it rose to its modern size,up to 6.5 m in depth,during the last millennium.Our data reveal important changes in the understanding of the history of this large endorheic lake,as before it was envisioned as a large lake with significant changes in water level since ca.14 ka BP.In addition to hydrology,our proxies provide updates and details of the regional vegetation and climate change since ca.4 ka BP in the WestSiberian forest-steppe and steppe.As evolution of the Chany basin is dependent on hydroclimatic changes in a large region of southern West Siberia,we compare lake-level change and climate-change proxies from the other recently and most comprehensively studied lakes of the region. | S.K.Krivonogov A.N.Zhdanova P.A.Solotchin A.Y.Kazansky V.V.Chegis Z.Liu M.Song S.V.Zhilich N.A.Rudaya X.Cao O.V.Palagushkina L.B.Nazarova L.S.Syrykh | 2023 | Geoscience Frontiers2023，14，2： | 0 |
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