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| 1 | Mechanism of Cu(Ⅱ) adsorption inhibition on biochar by its aging process显示文摘Biochar exposed in the environment may experience a series of surface changes, which is called biochar aging. In order to study the effects of biochar aging on Cu(II) adsorption, we analyzed the surface properties before and after biochar aging with scanning electron microscopy(SEM) coupled to an energy-dispersive X-ray spectrometer(EDX) and diffuse reflectance infrared Fourier transform spectroscopy(DRIFTS), and then explored the influence of the aging process on Cu(II) adsorption by batch experiments. After the aging process, the oxygen concentration, phenolic hydroxyl groups, aromatic ethers and other oxygen-containing functional groups on the biochar surface increased, while carboxyl groups slightly decreased. Thus, over a range of pH, the cation exchange capacity(CEC) and adsorption capacity of Cu(II) on the aged biochar were smaller than those of new biochar,indicating that when biochar is incubated at constant temperature and water holding capacity in the dark, the aging process may inhibit Cu(II) adsorption. Meanwhile, the dissociation characteristics of oxygen-containing functional groups changed through the aging process, which may be the mechanism by which the biochar aging process inhibits the Cu(II) adsorption. Carboxyl groups became more easily dissociated at low pH(3.3–5.0),and the variation of maximum adsorption capability(qm) of Cu(II) on the old biochar was enlarged. Phenolic hydroxyl groups increased after the aging, making them and carboxyl groups more difficult to dissociate at high pH(5.0–6.8), and the variation of qmof Cu(II) on the aged biochar was reduced. | Yue Guo Wei Tang Jinggui Wu Zhaoqin Huang Jingyu Dai | 2014 | Journal of Environmental Sciences2014，26，10： | 21 |
| 2 | A Study of Sr, Nd and O Isotopes of the K-rich Melanocratic Dykes in the Late Mesozoic Gold Field in the Jiaodong Peninsula显示文摘Geologic, petrographic and petrochemical studies of the lateMesozoic K-rich melanocratic dykes, including lamprophyres, andesite porphyrites and dacite-porphyry in the gold field system in the Jiaodong Peninsula, China, have shown that these dykes are characterized by rich potassium and alkali but poor titanium. They belong to an ultra-high potassic, shoshonitic and high potassic calc-alkaline rock series. The parental magma has relatively high initial strontium ratios ((87Sr/86Sr)i-0.70895-0.71140) and low (143Nd/144Nd)i ratios (varying from 0.51135 to 0.51231); and its δ18OsMow. whole rock values vary from +5.8‰ to +10.6‰ with a mean of +7.1‰. These features suggest that the source region of the magma is an enriched mantle wedge transformed from a continental lithosphere mantle which has experienced me tasomatism by mantle-derived fluids with H2O-dominated fluids that were provided during the underthrusting of an ocean crust. The initial magma was generated by low-degree partial melting of the enriched mantle in its mature stage in the back-arc spreading environment. The evolution of magmas is associated with two trends, i.e., fractional crystallization and mixing with or intensive contamination by palaeo-crust materials or metamorphic rocks. The former process is evident in the gold field system of quartz-vein type, whereas the latter is dominated in the gold field system of the altered-rock type. This conclusion is very important for more detailed study of petrogenesis and mineralization through the crust-mantle interaction (exchange) in the Mesozoic in this region. | SUN Jinggui, HU Shouxi, LIU Jianmin, SHEN Kun and LING Hongfei Earth Science Institute, Jilin University, Changchun 130062 State Key Laboratory of Research on Metallogenesis of Endogenic Ore Deposits,Nanjing University, Nanjing 210093 Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101 Shandong Institute and Laboratory of Geological Sciences, Jinan 250013 | 2001 | Acta Geologica Sinica(English Edition)2001，75，4： | 14 |
| 3 | Geochemical research on C-O and Sr-Nd isotopes of mantle-derived rocks from Shandong Province, China显示文摘This paper presents systematic studies on the C-O and Sr-Nd isotopic compositions for Cretaceous Badou carbonatites, Fangcheng basalts, and Jiaodong lamprophyres and Paleozoic Mengyin kimberlites in Shandong Province, China. Paleozoic kimberlites have normal and uniform C-O isotopic compositions with δ13C and δ18O in the range of -4.8‰--7.6‰ and +9.9‰-+13.2‰, respectively. However, Cretaceous three different types of mantle-derived rocks have quite different C-O isotopic compositions, indicating that the mantle sources are probably partially contaminated with organic carbon-bearing crustal materials. These Cretaceous rocks show uniform and EMII-like Sr-Nd isotopic compositions and also indicate that the mantle sources were affected by recycled crustal materials. Comparative studies of C-O and Sr-Nd isotopes reveal that the lithospheric mantle beneath the eastern North China Craton had different isotope characteristics in the Paleozoic, the early Cretaceous, and the Tertiary time. This demonstrates that the lithospheric mantle beneath the region underwent at least twice reconstructions since the Paleozoic. Available data imply that the first reconstruction mainly happened during the Triassic-Jurassic time with gradual changes and the second in the Cretaceous with abrupt changes. Results also show that the early Cretaceous (especially at 120-130 Ma) was perhaps the key period leading to the dramatic change of the Mesozoic geodynamics on the eastern North China Craton. | LIU Jianming, ZHANG Hongfu, SUN Jinggui & YE Jie1. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China 2. School of Earth Science, Jilin University, Changchun 130061, China Correspondence should be addressed to Liu Jianming (email: jmliu@mail.igcas.ac.cn) | 2004 | Science China Earth Sciences2004，47，2： | 9 |
| 4 | Decomposition characteristics of organic materials and their effects on labile and recalcitrant organic carbon fractions in a semi-arid soil under plastic mulch and drip irrigation显示文摘Labile organic carbon(LC) and recalcitrant organic carbon(RC) are two major fractions of soil organic carbon(SOC) and play a critical role in organic carbon turnover and sequestration. The aims of this study were to evaluate the variations of LC and RC in a semi-arid soil(Inner Mongolia, China) under plastic mulch and drip irrigation after the application of organic materials(OMs), and to explore the effects of OMs from various sources on LC and RC by probing the decomposition characteristics of OMs using in-situ nylon mesh bags burying method. The field experiment included seven treatments, i.e., chicken manure(CM), sheep manure(SM), mushroom residue(MR), maize straw(MS), fodder grass(FG), tree leaves(TL) and no OMs as a control(CK). Soil LC and RC were separated by Huygens D's method(particle size-density), and the average soil mass recovery rate and carbon recovery rate were above 95%, which indicated this method was suitable for carbon pools size analysis. The LC and RC contents significantly(P<0.01) increased after the application of OMs. Moreover, LC and RC contents were 3.2%–8.6% and 5.0%–9.4% higher in 2016 than in 2015. The applications of CM and SM significantly increased(P<0.01) LC content and LC/SOC ratio, whereas they were the lowest after the application of TL. However, SOC and RC contents were significantly higher(P<0.01) after the applications of TL and MS. The correlation analysis indicated the decomposition rate of OMs was positively related with LC content and LC/SOC ratio. In addition, lignin, polyphenol, WOM(total water-soluble organic matter), WHA(water-soluble humic acid), HSL(humic-like substance) and HAL(humic acid-like) contents in initial OMs played important roles in SOC and RC. In-situ nylon mesh bags burying experiment indicated the decomposition rates of CM, SM and MS were significantly higher than those of MR, FG, and TL. Furthermore, MS could result in more lignin derivatives, WHA, and HAL polymers in shorter time during the decomposition process. In conclusion, the application of MS in the semi-arid soil under a long-term plastic mulch and drip irrigation condition could not only improve soil fertility, but also enhance soil carbon sequestration. | hu juan wu jinggui qu xiaojing | 2018 | Journal of Arid Land2018，10，1： | 7 |
| 5 | An Isotopic(Sr,Nd and Pb) Tracer Study on the Xiaoxinancha Gold-rich Copper Deposit in Yanbian,China:Implication for the Geodynamic Model of Diagenesis and Metallogenesis显示文摘同位素的研究全身地在吉林省在花岗石的建筑群, diorite-porphyrite,矿石和 103 妈 Xiaoxinancha 充满黄金的铜沉积物的矿石矿物质上被执行决定成岩作用和 metallogenesis 的 geodynamic 模型。结果证明花岗石的建筑群的同位素的作文在 0.704250.70505 的范围为的起始的 Nd 和 Sr (87Sr/86Sr ) 我, 0.512430.51264 为 INd,并且 1.31 ~ + 2.64 为 Nd (t) ;diorite-porphyrite 的那些在从 0.704380.70448 的范围为(87Sr/86Sr ) 我, 0.512590.51261 为 INd,和 +1.56 ~ + 2.09 为 Nd (t) 。为矿石和硫化物,(87Sr/86Sr ) 我, INd,和 Nd (t) 价值在从 0.704400.70805 的范围, 0.512590.51279 并且 +1.72 到 +5.56 分别地。花岗石的建筑群的 Pb 同位素的比率为 208Pb/204pb 为 207Pb/204Pb 为 206Pb/204Pb 从 18.299218.6636 ,从 15.534315.5660 ,并且从 38.164038.5657 因为分别地, diorite-porphyrite , 206Pb/204Pb 的同位素的比率, 207Pb/204Pb 和 208Pb/204b 是 18.3919 , 15.5794 和 38.3566 而那些为 206Pb/204Pb 从 18.227518.3770 矿石和矿石硫化物变化,从 15.555515.5934 为 207Pb/204Pb 并且从 38.131838.3131 为 208Pb/204Pb 。结果显示矿化作用被相关到花岗石的建筑群和 diorite-porphyrite 的形成和进化。在岩石学的特征,元素的地球化学和年表与报导数据结合,结论能被得出成岩作用的 geodynamic 设置和这的 metallogenesis 扔,这在早白垩纪期间与 Izanagi 海洋的板的 subduction 一致。diorite-porphyrite 被充实的披风的部分融化触发的 adakitic 岩浆的炮兵阵地形成,它从 subducting 由脱水液体从衍生物大陆人 lithospheric 披风 metasomatized 发源海洋的外壳。花岗石的建筑群被在 adakitic 岩浆和 high-K 之间的混合的部分结晶化生产计算碱的酸的岩浆,它被更低的外壳的 remelting 在 adakitic 岩浆的 intraplate upwelling 期间产生。忍受矿石的液体水库集合在混合岩浆房间的进化的一个迟了的阶段。 | MEN Lanjing SUN Jinggui ZHANG Zengjie LI Yixin XING Shuwen CUI Peilong | 2011 | Acta Geologica Sinica(English Edition)2011，85，1： | 7 |
| 6 | Determination on ^(87)Sr/^(86)Sr ratio and stratigraphic dating of single-grain foraminifera显示文摘The Sr isotopic composition of foraminifera has been used in studies of chronstratigraphy and sedi- mentary geochemistry. However, it is difficult to sample foraminifera without overprinting of later diagenesis, which contains enough amount of Sr for isotopic measurement. Analysis of single-grain foraminifera was successively conducted by a combination of low Sr procedural blank and high precision determination of 87Sr/86Sr ratio. This combi- nation of single-grain foraminifera can be significant for the study and application of Sr isotopic composition of fo- raminifera. Measured foraminifera of this study, having a size between 250 μm and 400 μm, were sampled from the carbonate basement of a ferromanganese crust in western Pacific. Mean value of 87Sr/86Sr ratios of the analyzed sin- gle-grain foraminifera is 0.709150 ±0.000013 with internal precision between 4 ppm and 8 ppm for each measurement run. Average value of total procedural blank of Sr is 14 pg. It is significant but difficult to date foraminifera in carbonate basements of ferromanganese crusts. Based on the ob- tained value of 87Sr/86Sr ratio, the analyzed foraminifera can be dated at 0.91 +0.33/?0.39 Ma. | TONG Jinggui LI Shengrong LI Xiannhui LI Qiuli FANG Nianqiao CHU Fengyou CHEN Fukun | 2006 | Chinese Science Bulletin2006，51，17： | 6 |
| 7 | The Lanshantou Kyanite-bearing Eclogite with Coesite Inclusions in the Sulu Ultrahigh-Pressure Metamorphic Belt and Its PTt Path显示文摘Coesite inclusions are found in kyanite from the Lanshantoueclogite in the Sulu ultrahigh-pressure (UHP) metamorphic belt. This discovery extends the stable region of kyanite to over 2.4 GPa. As an important UHP metamorphic belt in China, the Sulu eclogite belt is the product of A-subduction induced by strong compression of the Yellow Sea terrane to the Jiaodong-northereastem Jiangsu terrane during the interaction of the Eurasian plate and Palaeo-Pacific plate in the Indosinian. It stretches about 350 km and contains over 1000 eclogite bodies. Most eclogites in this belt belong to Groups B and C in the classification of Coleman et al., and commonly contain kyanite, while the Lanshantou eclogite belongs to Group A and contains coesite. The MgO, CaO and FeO contents in garnet and pyroxene show regular variation from the core to the rim, which reveals the PTt paths of progressive metamorphism during the Early Mesozoic (240-200 Ma) and retrogressive metamorphism during the Late Mesozoic and Cenozoic exhumation. | HU Shouxi, SUN Jinggui, LING Hongfei, YE Ying, Fang Changquan and ZHAO Yiying Department of Earth Sciences, Nanjing University, Nanjing 210008, Jiangsu Department of Earth Sciences, Zhejiang University, Hangzhou 310027, Zhejiang | 2001 | Acta Geologica Sinica(English Edition)2001，75，4： | 5 |
| 8 | Enzyme activities and gene expression of starch metabolism provide insights into grape berry development显示文摘Grapes are categorized as a non-climacteric type of fruit which its ripening is not associated to important rises in respiration and ethylene synthesis.The starch metabolism shares a certain role in the carbohydrate metabolic pathways during grape berry development,and is regarded as an important transient pool in the pathway of sugar accumulation.However,the comprehensive role of starch and its contribution to the quality and flavor of grape berry have not been explored thoroughly.In this study,the expression levels of genes enzyme activities and carbohydrate concentrations related to starch metabolism,were analyzed to understand the molecular mechanism of starch accumulation during grape berry development.The results indicated that starch granules in grape berry were located at the chloroplast in the sub-epidermal tissues,acting as the temporary reserves of photosynthetic products to meet the needs for berry development,and relatively high starch contents could be detected at véraison stage.Moreover,both ADP-glucose pyrophosphorylase(EC 2.7.7.27)and sucrose phosphate synthase(EC 2.3.1.14)involved in starch synthesis displayed elevated gene expression and enzymes activities in the sub-epidermal tissue,whileα-andβ-amylases involved in its degradation were highly transcribed and active in the central flesh,explaining the absence of starch in this last tissue.Change in the gene expression and activities of ADP-glucose pyrophosphorylase,β-amylase and sucrose phosphate synthase revealed that they were regulated by the circadian rhythms in the fruitlets compared with those in the leaves.Both the morphological,enzymological and transcriptional data in this study provide advanced understandings on the function of starch during berry development and ripening that are so important for berry quality.This study will further facilitate our understanding of the sugar metabolism in grape berry as well as in other plant species. | Xudong Zhu Chaobo Zhang Weimin Wu Xiaopeng Li Chuan Zhang Jinggui Fang | 2017 | Horticulture Research2017，4，1： | 4 |
| 9 | Geological Anomaly of China显示文摘Geological Anomaly of China￥ZhaoPengda(FacultyofEarthResources,ChinaUniversityofGeosciences,Wuhan430074)WangJinggui;RaoMinghu... | Zhao Pengda(Faculty of Earth Resources,China University of Geosciences, Wuhan 430074)Wang Jinggui Rao Minghui Li Haochang(Department of Geology, East China College of Geology, Fuzhou 344000) | 1995 | Journal of Earth Science1995，14，1： | 3 |
| 10 | Origin and evolution of ore-forming fluid for the Gaosongshan gold deposit, Lesser Xing’an Range:Evidence from fluid inclusions,H-O-S-Pb isotopes显示文摘Epithermal gold deposits are typical precious metal deposits related to volcanic and subvolcanic magmatism.Due to the lack of direct geological and petrographic evidences,the origin of the ore-forming fluid is deduced from the spatial diagenesis-mineralization relationship,chronological data,physicochemical characteristics of mineral fluid inclusions,mineral or rock elements and isotopic geochemical characteristics.By objectively examining this scientific problem via a geological field survey and petrographic analysis of the Gaosongshan epithermal gold deposit,we recently discovered and verified the following points:(1) Pyrite-bearing spherical quartz aggregates (PSQA) occur in the rhyolitic porphyry;(2) the mineralization is structurally dominated by WNW- and ENE-trending systems and occurs mostly in hydrothermal breccias and pyrite-quartz veins,and the ore types are mainly hematite-crusted quartz,hydrothermal breccia,massive pyrite-quartz,etc.;(3) the alteration types consist of prevalent silicification,sericitization,propylitization and carbonation,with local adularization and illitization.The ore minerals are mainly pyrite,primary hematite,native gold,and electrum,with lesser amounts of chalcopyrite,magnetite,sphalerite,and galena,indicating a characteristic epithermal low-sulfidation deposit.The ore-forming fluid may have been primarily derived from magmatic fluid exsolved from a crystallizing rhyolitic porphyry magma.Further zircon U-Pb geochronology,fluid inclusion,physicochemical and isotopic geochemical analyses revealed that (1) rhyolitic porphyry magmatism occurred at 104.6 ± 1.0 Ma,whereas the crystallization of the PSQA occurred at 100.8 ± 2.1 Ma;(2) the hydrothermal fluid of the pre-ore stage was an exsolved CO2-bearing H2O-NaCl magmatic fluid that produced inclusions mainly composed of pure vapor (PV),vapor-rich (WV) and liquid-rich (WL) inclusions with a small number of melt-(M) and solid-bearing (S) inclusions;mineralization-stage quartz contains WL and rare PV,WV and pure liquid (PL) inclusions characterized by the H2O-NaCl system with low formation temperatures and low salinities;(3) the characteristics of hydrogen,oxygen,sulfur,and lead isotopes and those of rare earth elements (REEs) provide insight into the affinity between PSQA and orebodies resulting from juvenile crust or enriched mantle.Combined with previous research on the mineralogenetic epoch (99.32 ± 0.01 Ma),we further confirm that the mineralization of the deposit occurred in the late Early Cretaceous,which coincides with the extension of the continental margin induced by subduction of the Pacific Plate beneath the Eurasian Plate.The formation of the ore deposit was proceeded by a series of magmatic and hydrothermal events,including melting of enriched juvenile crust,upwelling,the eruption and emplacement of the rhyolitic magma,the exsolution and accumulation of magmatic hydrothermal fluid,decompression,the cooling and immiscibility/boiling of the fluid,and mixing of the magmatic fluid with meteoric water,in association with water-rock interaction. | Yang Liu Jinggui Sun Jilong Han Liang Ren Alei Gu Keqiang Zhao Changshen Wang | 2019 | Geoscience Frontiers2019，10，5： | 3 |
| 11 | LA-ICP-MS zircon U-Pb age of rhyolitic lithic-crystal tuffs in Erdaohezi lead-zinc deposit,Inner Mongolia显示文摘Erdaohezi lead-zinc deposit belongs to the Derbugan metallogenic belt lying on the northwestern Hailaer-Genhe Mesozoic volcanic basin,located on the western slope of the Da Hinggan Mountains. The deposit is considered as one of the hypabyssal low-temprature hydrothermal lead-zinc deposits associated with volcanism. In order to lay the foundation on studying its diagenesis and mineralization ages,the detailed studies were carried out by dating the host rocks( i. e. rhyolitic lithic-crystal tuffs) using zircon LA-ICP-MS U-Pb method.The dating results show three groups of ages. The first group is the captured zircons( the weighted mean ^(206)Pb /^(238) U age as 175. 6 ± 2. 3 Ma,MSWD = 0. 70,n = 3). The second group can be regarded as the rockforming age( the weighted mean ^(206)Pb /^(238) U age as 165. 3 ± 1. 9 Ma,MSWD = 2. 40,n = 14). The third group should represent the late stage of the magmatic evolution( the weighted mean ^(206)Pb /^(238) U age as 161. 0 ± 3. 1Ma,MSWD = 0. 86,n = 4). According to the ages and the crystal form or CL image characteristics of zircons,it is determined that the diagenesis occurred in the late Middle Jurassic. Based on the regional geology and geochronological research,the acidic pyroclastic rocks are space accompaniment and time connection with the Tamulangou Formation intermediate-mafic volcanic rocks. Both of them constitute the host rocks of the deposit together. The rock combination also provides favorable conditions for large-scale silver,lead and zinc mineralization in this area. | YAN Jia SUN Jinggui ZHAO Shifeng MING Zhu | 2015 | Global Geology2015，18，4： | 2 |
| 12 | Oceanographic ontology-based spatial knowledge query显示文摘The construction of oceanographic ontologies is fundamental to the 'digital ocean'. Therefore, on the basis of introduction of new con-cept of oceanographic ontology, an oceanographic ontology-based spatial knowledge query (OOBSKQ) method was proposed and de-veloped. Because the method uses a natural language to describe query conditions and the query result is highly integrated knowledge,it can provide users with direct answers while hiding the complicated computation and reasoning processes, and achieves intelligent,automatic oceanographic spatial information query on the level of knowledge and semantics. A case study of resource and environmen-tal application in bay has shown the implementation process of the method and its feasibility and usefulness. | WANG Jinggui SU Fenzhen ZHOU Chenghu DU Yunyan YANG Xiaomei | 2005 | Acta Oceanologica Sinica2005，24，4： | 2 |
| 13 | Rural Ecological Landscape Construction from the Perspective of Rural Revitalization Strategy显示文摘Based on the strategies for rural revitalization proposed in the 19 th National Congress report and 2018 No.1 Document of CPC Central Committee, combined with the current situation of rural environmental pollution in China, this paper first elaborated the connotation of rural ecological landscapes, and analyzed the structure, functions, and values of rural landscape ecology. The principle of building rural landscape ecology under the strategy of rural revitalization was studied. Finally, the methods and approaches of rural landscape ecological construction under the strategy of rural revitalization were studied. | YE Feng MA Jinggui | 2018 | Journal of Landscape Research2018，10，4： | 2 |
| 14 | Relationship between CO_2-bearing fluid and gold mineralization in Haigou gold deposit of Jilin显示文摘Haigou gold deposit is a typical orogenic gold deposit. There are a reasonable amount of fluid inclusions in the gold deposit,including three types: CO2-H2O-Na Cl inclusions,pure CO2 inclusions and Na Cl-H2 O inclusions,of which most of them are CO2-bearing inclusions. The fluid salinity is 1. 43%- 9. 08%,mainly concentrated in the range of 4. 69%- 5. 41%,the density of CO2 is 0. 69- 0. 80 g / cm3,indicating that the mineralization fluid is low-medium salinity and low density fluid. A series of studies on gold-bearing quartz vein and fluid inclusions show that there exists a positive correlation between the degree of the gold mi-neralization and the amount of CO2 in the inclusions,which means the more CO2-bearing inclusions there are,the higher the content of gold is. CO2 is mainly derived from mantle fluid,and the ore-forming fluid should be derived from mantle fluid and the crust shallow fluid. The conclusions have important denotative meaning on the metallogenic mechanism of orogenic gold deposit and the deep prospecting on metal deposit. | GAO Song PENG Xiaolei SUN Jinggui FU Lingzhi WANG Jianyu | 2015 | Global Geology2015，18，1： | 2 |
| 15 | Metabolic system identification and optimization in continuous culture显示文摘 | Jinggui Gao Enmin Feng Zhilong Xiu | 2012 | International Journal of Computer Mathematics2012，，10： | 1 |
| 16 | Modeling and identification of microbial batch fermentation using fuzzy expert system显示文摘 | Jinggui Gao Lei Wang Enmin Feng Zhilong Xiu | 2013 | Applied Mathematical Modelling2013，，： | 1 |
| 17 | Anatomical berry characteristics during the development of grape berries with different shapes显示文摘The aim of this study was to characterize the changes in berry anatomy during the development of grape(Vitis vinifera L.,and Vitis vinifera×Vitis labrusca)with different shapes.Paraffin sectioning was used to examine the structural parameters of the cells.The results revealed that,with the development of berries,the transverse and longitudinal diameters of the flesh cells gradually increased,revealing certain regularity.However,the transverse and longitudinal diameters of the epidermal and sub-epidermal cells were different between varieties,reflecting the specificity of the varieties.The growth of the transverse and longitudinal diameters of the berries was found to be completed in the early stage of development.A combination of correlation analysis and size analysis for each cell layer revealed that,due to the small crosssectional area of the epidermal and sub-epidermal cells,the influence of these cells on the transverse and the longitudinal diameters of the berries would be small.In conclusion,the longitudinal and transverse diameters of the grape berries were mainly determined by the longitudinal and transverse diameters of the flesh cells.The different shapes of the grape berries could mainly be attributed to the different growth rates of the flesh cells in the longitudinal and transverse directions.These different rates of growth led to different lengths and widths of the berry. | Chuan Zhang Xiucai Fan Chonghuai Liu Jinggui Fang | 2021 | Horticultural Plant Journal2021，7，4： | 1 |
| 18 | Prognostic Significance of c - erbB - 2 and Vascular Endothelial Growth Factor in Colorectal Liver Metastases显示文摘 | Jinggui Chen Qingguo Li Changjian Wang | 2010 | Ann Surg Oncol2010，17，： | 1 |
| 19 | Optimal control of switched systems and its parallel optimization algorithm 显示文摘 | Zhai Jingang Shen Bangyu Gao Jinggui | 2014 | Journal of Computational and Applied Mathematics2014，261，： | 1 |
| 20 | Identification and characterization of 27 conserved microRNAs in citrus显示文摘 | Changnian Song Jinggui Fang Xiaoying Li Hong Liu C. Thomas Chao | 2009 | Planta2009，，4： | 1 |
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