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| 1 | Distribution of Grain Hardness in Chinese Wheats and Genetic Analysis显示文摘A hundred winter wheat and 41 spring wheat cultivars and advanced lines were used to investigate the distribution of grain hardness in Chinese wheats and correlations between grain hardness and other kernel traits. P1, P2, F1, F2 and F3 from three crosses, i. e. , Liken2/Yumai2, 85Zhong33/Wenmai6 and 85Zhong33/95Zhong459 were sown to study the genetics of grain hardness. Significant correlation was observed between hardness measured by Single Kernel Characteristic System 4100 (SKCS 4100) and Near Infrared (NIR) Spectroscopy, r ranging from 0. 85 to 0.94. Chinese wheat is a mixed population in terms of hardness, ranging from very soft to very hard. For autumn-sown wheat, on average, grain hardness decreases from north to south and spring-sown wheat is dominant with hard type. Hardness is negatively associated with flour color, and its associations with flour yield and ash content differ in winter and spring wheats. Grain hardness is controlled by a major gene and several minor genes with additive effect mostly, but dominant effect is also observed, with heritability of 0.78. | ZHOU Yan-hua, HE Zhong-hu, YAN Jun, ZHANG Yan, WANG De-sen and ZHOU Gui-ying(Institute of Crop Breeding and Cultivation, Chinese Academy of Agricultural Sciences / National Wheat Improvement Center,Beijing 100081 ,P. R. China CIMMYT China Office, C/OCAAS, Beijing 100081 ,P. R. China) | 2002 | Agricultural Sciences in China2002，1，11： | 3 |
| 2 | Benthic filterfeeding a natural eutrophication contro1显示文摘 | Officer C Smayda T | 1982 | Mar Eco1 Prog Sot1982，，9： | 1 |
| 3 | The possible importance of sili- con in marine eutrophication显示文摘 | OFFICER C B RYTHER J H | 1980 | Mar Ecol Prog Set1980，3，1： | 1 |
| 4 | Preparation, characterisation and biosensor application of conducting polymers based on ferrocene substituted thiophene and terthiophene 显示文摘 | CHEN J TOO C WALLACE G BURRELL A COLLIS G OFFICER D SWEIGERS G | 2002 | Electrochim Acta2002，47，： | 1 |
| 5 | Theoretical and spectroscopic study of a series of styryl-substituted terthiophenes 显示文摘 | Clarke T M Gordon K C Officer D L | 2003 | The Journal of Physical Chemistry A2003，107，11： | 1 |
| 6 | Directors' and officers' liability insurance and acquisition outcomes 显示文摘 | Lin C Officer M S Zou H | 2011 | Journal of Financial Economics2011，102，3： | 1 |
| 7 | Benthic filter feeding: A natural eutrophication control 显示文摘 | Officer C B Smayda T J Mann R | 1991 | Mar Ecol Prog Ser1991，69，2： | 1 |
| 8 | Benthic filter feeding a natural eutrophica- tion control 显示文摘 | Officer C Smayda T | 1982 | Mar Ecol Prog Sot1982，9，： | 1 |
| 9 | Conjugated polymers:New materials for photovoltaics 显示文摘 | Wallace G G Dastoor P C Officer D L | 2001 | Chem In- nov2001，30，4： | 1 |
| 10 | Termination fees in mergers and acquisitions显示文摘 | Officer M C | 2003 | Journal of Financial Economics2003，69，： | 1 |
| 11 | Benthic fdter feeding:A natural eutrophication conrtol显示文摘 | Officer C B Smayda T J Mann R | 1982 | Mar Ecol Prog Ser1982，9，： | 1 |
| 12 | Late Cretaceous and paroxysmal Cretaceous/Tertiary extinctions显示文摘 | Officer C B Hallam A Drake C L | 1987 | Nature1987，326，6109： | 1 |
| 13 | The possible importance of silicon in marine eutrophication显示文摘 | OFFICER C B RYTHER J H | 1990 | Marine Ecology Progress Series1990，3，： | 1 |
| 14 | Discussion of the turbidity maximum minpartially mixed estuaries显示文摘 | OFFICER C B | 1980 | Estuarine and Coastal Marine Science1980，10，： | 1 |
| 15 | Benthic filter feeding:a natural eutro- phication control 显示文摘 | Officer C B Dollar Z A | 1988 | Marine Ecology Progress Series1988，9，： | 1 |
| 16 | Benthic filter feeding:a natural eutrophication control显示文摘 | Officer C B Smayda T J Mann R | 1991 | Mar Ecol Prog Ser1991，69，： | 1 |
| 17 | Dynamic Deformation of Volcanic Ejecta from the Toba Caldera:Possible Relevance to Cretaceous/Tertiary Boundary Phenomena显示文摘 | Officer C B Chesner C A | 1986 | Geology1986，14，： | 1 |
| 18 | Late Cretaceous and Paroxysmal Cretaceous/Tertiary Extinction显示文摘 | Hallam A Drake C L | 1987 | Nature1987，326，： | 1 |
| 19 | Cloud microphysical and rainfall responses to zonal perturbations of sea surface temperature:A cloud-resolving modeling study显示文摘The cloud microphysical and rainfall responses to zonal perturbations of sea surface temperature (SST) are investigated by analyzing the equilibrium simulation data (from day 31-40) obtained from a series of two-dimensional cloud-resolving simulations with a zonal model domain of 768 km. Four experiments imposed by zonal SST perturbations of wavenumbers 1 (SST29Z1), 2 (SST29Z2), 4 (SST29Z4), and 8 (SST29Z8) are compared to the control experiment imposed by zonally uniform SST (SST29). The model domain mean SST is 29 °C, and the two-dimensional cloud-resolving model with a cyclic lateral boundary is also imposed by zero vertical velocity and constant zonal wind. The time and model domain mean surface rain rates in SST29Z1, SST29Z2, and SST29Z8 are about 10% larger than those in SST29, whereas the mean surface rain rates in SST29Z4 and SST29 are similar. The analysis of mean surface rainfall budgets shows that local water vapor and hydrometeor changes play important roles in determining the differences and similarities in mean surface rain rate between the perturbation experiments and the control experiment. Both convective and stratiform rain rates are larger in SST29Z1 and SST29Z2 than in SST29 due to the smaller advection of rain from convective regions into raining stratiform regions and the larger vapor condensation rates associated with the larger water vapor convergence over raining stratiform regions in SST29Z1 and SST29Z2. The convective rain rates are larger in SST29Z4 and SST29Z8 than in SST29 because of the larger condensation rates associated with the larger water vapor convergence over convective regions in SST29Z4 and SST29Z8. The stratiform rain rates in SST29Z4 and SST29Z8 are smaller than in SST29 due to the smaller vapor condensation rates and smaller collection rates of cloud water by rain over raining stratiform regions in SST29Z4 and SST29Z8. | Xiaopeng Cuia, Xiaofan Lib, Zhiping Zongc a Laboratory of Cloud-Precipitation Physics and Severe Storms (LACS), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China b Joint Center for Satellite Data Assimilation and NOAA/NESDIS/Office of Research and Applications, Camp Springs, MD, USA c National Meteorological Center, China Meteorological Administration, Beijing 100081, China | 2009 | Progress in Natural Science:Materials International2009，19，5： | 1 |
| 20 | Late Cretaceous and paroxysmal Cretaceous / Tertiary extinctions 显示文摘 | Officer C B Hallam A Drake C L | 1987 | Nature1987，326，： | 1 |
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