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| 1 | Projection of the Zhujiang(Pearl) River Delta's potential submerged area due to sea level rise during the 21st century based on CMIP5 simulations显示文摘Projections of potential submerged area due to sea level rise are helpful for improving understanding of the influence of ongoing global warming on coastal areas. The Ensemble Empirical Mode Decomposition method is used to adaptively decompose the sea level time series in order to extract the secular trend component. Then the linear relationship between the global mean sea level(GMSL) change and the Zhujiang(Pearl) River Delta(PRD)sea level change is calculated: an increase of 1.0 m in the GMSL corresponds to a 1.3 m(uncertainty interval from1.25 to 1.46 m) increase in the PRD. Based on this relationship and the GMSL rise projected by the Coupled Model Intercomparison Project Phase 5 under three greenhouse gas emission scenarios(representative concentration pathways, or RCPs, from low to high emission scenarios RCP2.6, RCP4.5, and RCP8.5), the PRD sea level is calculated and projected for the period 2006–2100. By around the year 2050, the PRD sea level will rise 0.29(0.21 to 0.40) m under RCP2.6, 0.31(0.22 to 0.42) m under RCP4.5, and 0.34(0.25 to 0.46) m under RCP8.5, respectively.By 2100, it will rise 0.59(0.36 to 0.88) m, 0.71(0.47 to 1.02) m, and 1.0(0.68 to 1.41) m, respectively. In addition,considering the extreme value of relative sea level due to land subsidence(i.e., 0.20 m) and that obtained from intermonthly variability(i.e., 0.33 m), the PRD sea level will rise 1.94 m by the year 2100 under the RCP8.5scenario with the upper uncertainty level(i.e., 1.41 m). Accordingly, the potential submerged area is 8.57×103 km2 for the PRD, about 1.3 times its present area. | XIA Jiangjiang YAN Zhongwei ZHOU Wen FONG Soi Kun LEONG Ka Cheng TANG Iu Man CHANG S W LEONG W K JIN Shaofei | 2015 | Acta Oceanologica Sinica2015，34，9： | 3 |
| 2 | Seasonal variation analysis of atmospheric CH_4,N_2O and CO_2 in Tianjin offshore area显示文摘The concentrations of CH4, N2O and CO2 at the sea level were observed from November 2007 to August 2008 in order to study the greenhouse gases in the Tianjin offshore area of Bohai Sea. CH4 concentrations varied from 1.87 to 2.61 ppm with the highest value appearing in summer and the lowest in winter. The concentration range of N2O was 319.3 to 347.7 ppb, with the maximal value appearing in winter. CO2 was higher in the heating season than in non-heating season in this area. Concentrations of the three greenhouse gases in the study area exceeded the 2005 global background values. Backward trajectory model was used to analyze the sources. All three gases were influenced evidently by continental sources in the inshore area during the sampling periods. Every gas was compared with each other by correlation analysis, showing that the correlation of CO2 and N2O was more significant than to CH4 and their relationship with meteorological factors was consistent. It can be concluded these three greenhouse gases may be influenced by some similar sources, especially for CO2 and N2O. | KONG ShaoFei, LU Bing, HAN Bin, BAI ZhiPeng, XU Zhun, YOU Yan, JIN LiangMao, GUO XiaoYang & WANG Rui State Environmental Protection Key Laboratory of Urban Ambient Air Particulate Matter Pollution Prevention and Control, College of Environmental Science and Engineering, Nankai University, Tianjin 300071, China | 2010 | Science China Earth Sciences2010，53，8： | 2 |
| 3 | New β-delayed Proton Precursor ^(135)Gd显示文摘Newβ-delayedProtonPrecursor^(135)Gd￥XuShuwei;XieYuanxiang;LiZhankui;MaRuichang;GeYuanxiu;WangChunfang;GuoBing;XingJianping;Hu?.. | Xu Shuwei Xie Yuanxiang Li Zhankui Ma Ruichang Ge Yuanxiu Wang Chunfang Guo Bing Xing Jianping Huang Wenxue Zhang Tianmei Liu Zhong Zhu Shaofei Jin Genming and Luo Yixiao | 1996 | IMP & HIRFL Annual Report1996，，1： | 2 |
| 4 | Hierarchical responses of soil organic and inorganic carbon dynamics to soil acidification in a dryland agroecosystem,China显示文摘Soil acidification is a major global issue of sustainable development for ecosystems. The increasing soil acidity induced by excessive nitrogen(N) fertilization in farmlands has profoundly impacted the soil carbon dynamics. However, the way in which changes in soil p H regulating the soil carbon dynamics in a deep soil profile is still not well elucidated. In this study, through a 12-year field N fertilization experiment with three N fertilizer treatments(0, 120, and 240 kg N/(hm^2·a)) in a dryland agroecosystem of China, we explored the soil p H changes over a soil profile up to a depth of 200 cm and determined the responses of soil organic carbon(SOC) and soil inorganic carbon(SIC) to the changed soil p H. Using a generalized additive model, we identified the soil depth intervals with the most powerful statistical relationships between changes in soil p H and soil carbon dynamics. Hierarchical responses of SOC and SIC dynamics to soil acidification were found. The results indicate that the changes in soil p H explained the SOC dynamics well by using a non-linear relationship at the soil depth of 0–80 cm(P=0.006), whereas the changes in soil p H were significantly linearly correlated with SIC dynamics at the 100–180 cm soil depth(P=0.015). After a long-term N fertilization in the experimental field, the soil p H value decreased in all three N fertilizer treatments. Furthermore, the declines in soil p H in the deep soil layer(100–200 cm) were significantly greater(P=0.035) than those in the upper soil layer(0–80 cm). These results indicate that soil acidification in the upper soil layer can transfer excess protons to the deep soil layer, and subsequently, the structural heterogeneous responses of SOC and SIC to soil acidification were identified because of different buffer capacities for the SOC and SIC. To better estimate the effects of soil acidification on soil carbon dynamics, we suggest that future investigations for soil acidification should be extended to a deeper soil depth, e.g., 200 cm. | JIN Shaofei TIAN Xiaohong WANG Hesong | 2018 | Journal of Arid Land2018，10，5： | 1 |
| 5 | Global brown carbon emissions from combustion sources显示文摘Light-absorbing organic carbon(OC),sometimes known as Brown Carbon(BrC),has been recognized as an important fraction of carbonaceous aerosols substantially affecting radiative forcing.This study firstly developed a bottom-up estimate of global primary BrC,and discussed its spatiotemporal distribution and source contributions from 1960 to 2010.The global total primary BrC emission from both natural and anthropogenic sources in 2010 was 7.26(5.98-8.93 as an interquartile range)Tg,with 43.5%from anthropogenic sources.High primary BrC emissions were in regions such as Africa,South America,South and East Asia with natural sources(wild fires and deforestation)contributing over 70%in the former two regions,while in East Asia,anthropogenic sources,especially residential solid fuel combustion,accounted for over 80%of the regional total BrC emissions.Globally,the historical trend was mainly driven by anthropogenic sources,which increased from 1960 to 1990 and then started to decline.Residential emissions significantly impacted on emissions and temporal trends that varied by region.In South and Southeast Asia,the emissions increased obviously due to population growth and a slow transition from solid fuels to clean modern energies in the residential sector.It is estimated that in primary OC,the global average was about 20%BrC,but this ratio varied from 13%to 47%,depending on sector and region.In areas with high residential solid fuel combustion emissions,the ratio was generally twice the value in other areas.Uncertainties in the work are associated with the concept of BrC and measurement technologies,pointing to the need for more studies on BrC analysis and quantification in both emissions and the air. | Rui Xiong Jin Li Yuanzheng Zhang Lu Zhang Ke Jiang Huang Zheng Shaofei Kong Huizhong Shen Hefa Cheng Guofeng Shen Shu Tao | 2022 | Environmental Science and Ecotechnology2022，，4： | 0 |
| 6 | Study on the Water Surge Height Line of Landslide Surge of Linear River course Reservoir Based on FLOW-3D显示文摘 | Wen Chen Peng Hui Jin Ke Wu Fan Yin Shaofei | 2016 | Journal of Environmental Science and Engineering(B)2016，5，6： | 0 |
| 7 | Spin-canting and weak ferromagnetism in two novel 1D alternating chains with single cis-end-to-end azido bridges显示文摘By combining trans-4-styrylprydine (tsp) with azide system, we obtained two rare 1D cis-EE-azido-bridged compounds of [M2(N3)4(tsp)4(H2O)2] [M = Mn (1), Co (2)]. The magnetic study reveals that metal ions are anti-ferromagnetically coupled by cis-EE-azido-bridges and they show weak ferromagnetism below 4.0 K (1) and 4.2 K (2) due to the spin-canting caused by asymmetric magnetic interaction. | SUN HaoLing XIONG Jin JI ShaoFei ZHEN Xue JIA Li LIU Tao | 2012 | 中国科学:化学2012，42，6： | 0 |
| 8 | Spin-canting and weak ferromagnetism in two novel 1D alternating chains with single cis-end-to-end azido bridges显示文摘By combining trans-4-styrylprydine (tsp) with azide system, we obtained two rare 1D cis-EE-azido-bridged compounds of [M2(N3)4(tsp)4(H2O)2] [M = Mn (1), Co (2)]. The magnetic study reveals that metal ions are anti-ferromagnetically coupled by cis-EE-azido-bridges and they show weak ferromagnetism below 4.0 K (1) and 4.2 K (2) due to the spin-canting caused by asymmetric magnetic interaction. | SUN HaoLing XIONG Jin JI ShaoFei ZHEN Xue HA Li LIU Tao | 2012 | Science China Chemistry2012，55，6： | 0 |
| 9 | Band Structure in Doubly Odd ~17Ta Nucleus显示文摘BandStructureinDoublyOdd~170TaNucleus￥ZhangYuhu;ZhaoQingzhong;ZhouXiaohong;XuHushan;GuoYinxiang;LeiXiangguo;LuJun;ZhuShaofei;?.. | Zhang Yuhu Zhao Qingzhong Zhou Xiaohong Xu Hushan Guo Yinxiang Lei Xiangguo Lu Jun Zhu Shaofei Huang Wenxue Liu Zhong Gou Quanbu Jin Hanjuan Hu Bitao Luo Yixiao Sun Xiangfu Zhu Yongtai Wen Shukian and Wu Shaoguang (The China Institute of Ato | 1996 | IMP & HIRFL Annual Report1996，，1： | 0 |
| 10 | The Deformation and Stress Analysis of Na Ba Reservoir Concrete Face Rock-Fill Dam显示文摘 | Yin Shaofei Peng Hui Wu Fan Wen Chen Jin Ke Han Kai | 2016 | Journal of Environmental Science and Engineering(B)2016，5，10： | 0 |
| 11 | First In-beam γ Spectroscopy Experiment at HIRFL 显示文摘FirstIn-beamγSpectroscopyExperimentatHIRFL￥GuoYiugxiang;ZhuShaofei;ZhouXiaohong;LeiXiangguo;LiuZhong;JinHanjuan;ZhangYuhu;Zha... | Guo Yiugxiang Zhu Shaofei Zhou Xiaohong Lei Xiangguo Liu Zhong Jin Hanjuan Zhang Yuhu Zhao Qingzhong Sun Xiangfu and Luo Yixiao | 1996 | IMP & HIRFL Annual Report1996，，1： | 0 |
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