个体老龄化生物标志物体外筛选模型的建立

根据蛋白交联理论,以丙酮醛及人血清白蛋白建立体外筛选模型,模拟体内氨基脲敏感的胺氧化酶介导美拉德反应导致蛋白交联的生物学过程.采用串联质谱结合¹⁸O标记的方法,定量分析丙酮醛对人血清白蛋白肽段的修饰程度用于表征衰老的程度,并对该方法的各项实验条件进行优化.建立了个体老龄化生物标志物体外筛选模型,优化了胰蛋白酶酶切及¹⁸O标记的实验条件.通过对优化条件下酶解后标记效率的评估,认为该方法将来可用于蛋白质组学方法,研究老龄化生物标志.     

多反应监测结合重组蛋白和18O同位素标记对脂肪合成代谢通路进行蛋白质相对定量的新方法

建立了多反应监测结合肽段串联体蛋白（concatamers of Q peptides,QconCATs）和¹⁸O同位素标记对脂肪合成代谢通路的蛋白质进行相对定量的新方法.挑选待检测蛋白的特异性肽段构建QconCAT质粒并将其转化导入大肠杆菌体系后进行表达.通过优化对QconCAT蛋白的酶切条件及考察¹⁸O标记效率.建立脂肪合成代谢通路蛋白多反应监测的蛋白质相对新定量方法,并对肥胖大鼠与正常大鼠脂肪代谢通路的蛋白质进行定量分析.结果发现脂肪合成通路的丙二酸单酰辅酶A-ACP转移酶,烯酰-ACP还原酶表达量均有显著上升（P<0.05）.该结论与之前报道肥胖相关的文献结果吻合,证明了本方法在定量生物样品应用中的可靠性.     

糖尿病早期预警肽类生物标志物的初步筛选

基于蛋白质组学策略结合¹⁸O标记技术,分析人血清白蛋白糖基化程度的糖尿病生物标志物筛选模型.基于HPLC-ESI/TOF MS的检测方法,筛选对葡萄糖敏感的人血清白蛋白酶切肽段.建立糖尿病监测及早期预警肽类生物标志物筛选模型,初步筛选出11个潜在的糖尿病早期诊断生物标志物.     

Pu(H2O)53+和Pu(H2O)54+ 团簇的相对论密度泛函研究

用TPSSTPSS密度泛函方法, Pu离子和H₂O分子分别采用相对论有效原子实势(RECP)和6-31g基组, 研究了Pu(H₂O)₅³⁺和Pu(H₂O)₅⁴⁺ 团簇溶剂化和非溶剂化效应中的几何结构及紫外可见吸收光谱. 计算结果表明: 水溶剂环境对Pu(H₂O)₅³⁺及Pu(H₂O)₅⁴⁺ 团簇的几何结构影响都比较明显. NBO电荷分析表明水分子与钚离子之间没有直接的电荷转移. 所研究团簇的未配对电子都占据5f轨道. 在气相及水溶剂环境下, 所研究团簇的紫外可见吸收光谱存在较大差距. 主要的吸收峰大都源于f电子之间的跃迁.     

1株嗜碱放线菌的生理学特性研究及其鉴定

 对从青海茶卡盐湖岸土样中分离到的1株生理较特殊的嗜碱放线菌YIM80305的生长pH范围,不同碱性物质KOH,K₂CO₃,NaOH,Na₂CO₃对其生长的影响,耐NaCl,KCl特性进行了研究.同时从形态,细胞壁类型,16SrDNA等方面进行了鉴定.结果发现YIM80305对Na⁺碱性物质有一定依赖性,对K⁺敏感,YIM80305可能是Streptomyces属的1个新种.     

广西乐业天坑群中苔藓的放射性核素分析

为探究广西喀斯特地貌对放射性核素分布及当地环境放射性的影响,利用高纯锗探测器对广西喀斯特地区的大曹天坑和邓家坨天坑采集来的苔藓样品中⁷Be、⁴⁰K、²³⁸U、²³²Th、²²⁶Ra、²¹⁰Pb和¹³⁷Cs的放射性比活度进行测量与分析。结果表明：在苔藓植物中, ⁷Be的放射性比活度为202.3-698.8 Bq/kg [平均值：(430.7±169.7) Bq/kg,n=7];⁴⁰K为33.7-159.9 Bq/kg [平均值：(91.6±44.1) Bq/kg, n=7];²³⁸U为检测限(3.0 Bq/kg)至54.4 Bq/kg [平均值：(16.9±23.6) Bq/kg,n=7];²³²Th为1.2-42.5 Bq/kg [平均值：(14.7±15.9) Bq/kg, n=7];²²⁶Ra为0.7-48.4 Bq/kg [平均值：(16.9±20.3) Bq/kg,n=7];²¹⁰Pb为284.1-950.5 Bq/kg [平均值：(555.5±231.0) Bq/kg, n=7]; ¹³⁷Cs为检测限(0.1 Bq/kg)至2.3 Bq/kg [平均值：(1.1±0.9) Bq/kg,n=7]。对比后发现所有测得的数据均在正常范围内,表明天坑这一喀斯特地貌对放射性核素的分布并没有显著影响,该地区也不存在其他污染来源,同时为我国南方喀斯特地区大气示踪提供数据支撑。     

基于掺铕钨酸盐荧光强度比的非接触温度传感

为了突破传统测温技术应用的局限性,利用NaY （WO₄）₂：Eu³⁺玻璃陶瓷（glass ceramics,GC）实现了具有非接触、实时响应、自校准等优势的双模荧光强度比（luminescence intensity ratio,LIR）测温。采用高温熔融淬灭法制备出含NaY （WO₄）₂：Eu³⁺纳米晶的透明GC样品,并进行系列光谱测量和热敏性能分析。结果表明,样品中Eu³⁺的激发态能级⁵D₁和⁵D₀和基态能级⁷F₂和⁷F₀为两对独立的热耦合能级,可分别基于这两对热耦合能级实现性能优异的双模LIR温度传感。该双模LIR测温技术数据可靠、测温范围广、灵敏度高,再结合GC材料优势,是可用于光纤温度传感器的核心技术材料。     

NaBH4还原改性TiO2(B)及光催化性能研究

以TiCl₄为原料,在（CH₂OH）₂溶液中通过一步水热法制备单斜相二氧化钛[TiO₂(B)]。使用不同质量含量NaBH₄对TiO₂(B)进行还原改性,调控其内含Ti³⁺的浓度,合成了含Ti³⁺的TiO₂(B)-NaBH₄X样品。采用X射线衍射仪（X-ray diffraction,XRD）、拉曼光谱仪（Raman spectroscopy）、紫外-可见漫反射光谱仪（UV-visible diffuse reflectance spectroscopy,UV-DRS）、X射线光电子能谱仪(X-ray photoelectron spectroscopy,XPS）对材料进行表征。改性后TiO₂(B)-NaBH₄X样品保持其原有晶体结构,并未发生相变,仅有结晶度的改变。原始TiO₂(B)禁带宽度为3.15 eV,通过改性,Ti³⁺的存在改变了禁带宽度,成功地将禁带宽度降低到2.82 eV,将吸光区域扩展到可见光区域。通过可见光光催化分解水制氢与可见光降解甲基橙试验,确立了TiO₂(B)-NaBH₄3样品有最好的可见光光催化活性,产氢速率达到0.58 μmol·h^-1·g^-1,6 h降解率达到40%。     

水泥基复合固化剂对镉和锌混合污染土的固化试验研究

为了研究水泥基复合固化剂对重金属混合污染土的固化稳定效果及其与单一重金属污染土的固化效果差别,探究锌和镉离子之间是否有协同或拮抗作用,采用水泥、石灰、粉煤灰和蒙脱石等作为复合固化剂,通过开展无侧限抗压强度试验、毒性浸出试验、X射线衍射分析（XRD）以及电镜扫描分析（SEM）,研究锌镉混合污染土在不同固化剂掺量下的强度特性与浸出毒性、pH值与浸出毒性间的关系、重金属混合污染土与单一重金属污染土的固化效果差异,并通过XRD和SEM分别对固化产物的成分和形貌进行微观分析,进而分析固化机理。试验结果表明：用生石灰、粉煤灰、海泡石、蒙脱土替代等量水泥可使固化产物的强度提高;Zn²⁺与Cd²⁺之间不存在拮抗作用,Cd²⁺的存在还会有助于Zn²⁺的固定;重金属离子的浸出浓度随浸出液pH值的增大而明显降低;固化效果好的样品相较于固化效果差的样品有更多的针状、网状等较为致密的结构。     

线性交换子的加权估计

 多线性交换子T_b(f)(x)=∫_Rⁿ∏_i=1^m(b_i(x)-b_i(y))k(x,y)f(y)dy在L^p(Rⁿ)(1K是一个标准的Calderón-Zygmund核.主要研究交换子Mf(x)=sup_x∈Q∫_Q|f(y)|dy,其中f∈L_loc(Rⁿ),x∈Rⁿ,Q是任何包含x的方体,并用Sharp极大估计得到了该多线性交换子在Herz空间的一个加权有界性.     

Oxygen and hydrogen isotopic compositions of coexistent minerals of the Tasigake alkali granite pluton, northern Xinjiang: constraints upon the cause of18OD depletion and the18O/16O exchange kinetics

Oxygen and hydrogen isotopic compositions have been determined of three coexistent mineral triplets of alkali feldspar, quartz, arfvedsonite of 11 samples collected from the Tasigake alkali granite pluton, Ulungur River region, northern Xinjiang. Isotopic exchange with meteoric water during subsolidus cooling caused strong¹⁸O-D depletion and the remarkable nonequilibrium¹⁸O/¹⁶O relation between coexistent minerals.¹⁸O/¹⁶O exchange kinetic effects of the three minerals are simultaneously and consistently modelled. Exsolution and microtextural reorganization of alkali feldspar, and infiltration of water have been mutually facilitated by each other. Shallow intrusion, and circulation of meteoric water throughout the pluton cool it effectively. As a result, the “heat engine” is rapidly extinguished, and the nonequilibrium¹⁸O/¹⁶O relation is frosen.     

Oxygen isotope variation in the water cycle of the Yamzho lake Basin in southern Tibetan Plateau

Given the potential use of stable isotope in the paleoclimate reconstruction from lacustrine records as well as in the local hydrology cycle, it is crucial to understand the processes of stable isotope evolution in catchment in the Tibetan Plateau region. Here we present a detailed study on the water oxygen isotope based on 2 years observation including precipitation, river water and lake water in the Yamzho Lake, south of the Tibetan Plateau. Temporal variation of local precipitation 5180 shows an apparent ＂monsoon cycle＂. In monsoon season, 5180 in waters is lower. In non-monsoon season, δ^18O in precipitation and lake water is higher and higher river δ^18O exists in spring, probably reflecting the effect of land surface evaporation, together with the higher δ^18O values in spring precipitation. It is also found that the surface lake water δ^18O varies seasonally and annually. The lower lake water δ^18O in the late summer is apparently related to the summer monsoon precipitation. The mean δ^18O value of lake water in 2007 is 1.2‰ higher than that in 2004, probably due to the less monsoon precipitation in summer of 2007, as can be confirmed from the precipitation data at the Langkazi meteorological data. It is also found that an obvious shift of vertical lake water δ^18O reflects the fast mixture of lake water. δ^18O values of lake water are over 10‰ higher than those of precipitation and river water in this region due to the evaporation fractionation. The modeled results show that the evaporation process of the lake water is sensitive to relative humidity, and the present lake water δ^18O reflects a relative humidity of 51% in the Yamzho Lake. It shows that the lake will take 30.5 years to reach present lake water δ^18O given a large shift in the input water δ^18O. The modeled results also reveal that surface lake water temperature and inflow δ^18O have slight effect on the isotopic balance process of lake water in the Yamzho Lake.     

Characteristics of δ 18O in precipitation over Eastern Monsoon China and the water vapor sources

Monsoon circulation is an important carrier of water vapor transport, and it impacts the precipitation of the monsoonal regions through the constraints and controls of large-scale water vapor transport and distributions as well as the water vapor balance. An overall research on stable Hydrogen and Oxygen isotopes in precipitation over Eastern Monsoon China could benefit a compre-hensive understanding of the monsoonal precipitation mechanism. Seventeen field stations of the Chinese Network of Isotopes in Precipitation (CHNIP) have been selected to collect monthly composite precipitation samples during the years 2005―2006. Components of δD and δ¹⁸O have been analyzed to achieve the spatiotemporal distributions. The established Local Meteoric Water Line δD=7.46 δ¹⁸O+0.90 based on the 274 obtained monthly samples could be treated as isotope input functions across the region, due to basically reflecting the specific regional meteorological conditions over Eastern Monsoon China. The δ-value de-pleted from coastal to inner area. In Southern China and Northeastern China there were typical periodic patterns of δ¹⁸8O. Differ-ent dominant affecting metrological factors have been raised with different regions. From south to north, the temperature effect of δ¹⁸18O enhanced, while the amount effect changed from existing at an all-year-scale in Southern China to being only remarkable during the main rainy seasons in North China and Northeastern China. Main geographical controls varied from altitude in South-ern China and North China to latitude in Northeastern China. Furthermore, δ¹⁸O had an implication of advance and retreat of the monsoon as well as rainfall belt transfer δ¹⁸O was also a tracer for the movement path of typhoon and tropical storms.     

The seasonal variations of δ~(18)O , Cl~- , Na~+ , NO_3~- and Ca~(2+) in the snow and firn recovered from Princess Elizabeth Land, Antarctica

Snow and firn samples recovered from two snow pits (2.5 and 4.5m deep) and one 50-m firn core along the route of the 1996/1997 Chinese First Antarctic Inland Traverse Expedition in Princess Elizabeth Land, East Antarctica, have been measured for chemical composition and oxygen isotope ratio. In the two snow pits, the variations of NO3- are partly in phase with that of δ18O, while the variations of Cl~ and Na+ are in inverse phase with that of δ18O. The variations of CI- , Na+ , NO3- and δ18O show obvious seasonal variations and annual stratag-raphy. However, with the depth increasing, the seasonal variations of δ18O are gradually smoothed below 3 m (corresponding to about 10-year mass accumulation) in depth while the seasonal variations of Cl- , Na+ and NO3- are kept fairly well in the whole profile of the 50-m firn core (corresponding to about 250-year mass accumulation). The results provide a useful tool for dating the snow stratum in this region. On the contrary, no obvious seasonal variations of Ca2 + are found in the profiles.     

Indian monsoon influences altitude effect of δ~(18)O in precipitation/river water on the Tibetan Plateau

The δ^18O variation in precipitation acquired from 28 stations within the network of Tibetan Observation and Research Platform （TORP） is studied, with the focus on the altitude effect of δ^18O in river water during monsoon precipitation in an effort to understand the monsoon influence on isotopic composition in annual river water. It is found that δ^18O in precipitation on the Plateau is influenced by different moisture sources, with significant Indian monsoon influence on δ^18O composition in plateau precipitation and river water. The δ^18O of water bodies in the monsoon domain is generally more depleted than that in the westerly domain, suggesting gradual rainout of southwesterly borne marine moisture in the course of long-distance transportation and lifting over the Himalayas. The lapse rate of δ^18O in river water with altitude is the largest during monsoon precipitation, due to the increased temperature vertical gradient over the southern Plateau region controlled by monsoon circulation. The combination of δ^18O in river water in monsoon （wet） and non-monsoon （dry） seasons shows a larger lapse rate than that in non-monsoon （dry） season alone. As the altitude effect of δ^18O in precipitation and river water on the Tibetan Plateau results from the combined effect of monsoon moisture supply and westerly moisture supply, the δ^18O composition and its altitude effect on the Plateau during monsoon seasons should be considered in the reconstruction of paleoelevation of the Tibetan Plateau.     

同位素标记结合中性丢失扫描鉴定白蛋白早期糖基化修饰肽段

采用 [13C6] 同位素标记的葡萄糖作为标签,在体外建立非酶糖基化反应模型,并采用MALDI-TOF对模型中的糖基化人血清白蛋白(HSA)进行验证. 以高分辨率的液质联用四级杆飞行时间质谱(HPLC/Q-TOF MS)为分析平台,经过一级质谱(LC/MS)筛选糖基化肽段. 采用target MS/MS模式对筛选出的34条肽段进行分析. 运用蛋白质组学数据分析工具pFind软件对肽段的中性丢失扫描及二级质谱(LC/MS/MS)数据进行分析,最终获得16条早期糖基化修饰肽段的序列及修饰位点信息.      

Climatic significance of δ18O records from precipitation on the western Tibetan Plateau

Analysis of daily precipitation samples for stable oxygen isotopes （δ^18O） collected at the Shiquanhe and Gerze （Gaize, Gertse） stations in the Ngari （Ali） region on the western Tibetan Plateau indicates that air temperature affects the δ^18O variations in precipitation at these stations. In summer, Shiquanhe and Gerze show strongly similar trends in precipitation δ^18O, especially in simultaneous precipitation events. Moreover, both stations experienced low δ^18O values in precipitation during the active monsoon period, resulting from the southwest monsoon （the summer phase of the Indian monsoon）. However, during the break monsoon period （during the summer rainy season, when the monsoon circulation is disrupted）, δ^18O values in summer precipitation remain relatively high and local moisture recycling generally controls the moisture sources. Air temperature correlations with δ^18O strengthen during the non-monsoon period （January--June, and October--December） due to continental air masses and the westerlies. In addition, evaporation also influences the δ^18O variations in precipitation. The observed temporal and spatial variations of δ^18O in precipitation on the western Tibetan Plateau and adjacent regions show that the late May and early June-the late August and early September time frame provides an important period for the transportation of moisture from various sources on the Tibetan Plateau, and that the region of the West Kunlun-Tanggula Ranges acts as a significant climatic divide on the Plateau, perhaps for all of western China.     

Isotopic composition of atmospheric water vapor before and after the monsoon’s end in the Nagqu River Basin

Atmospheric water vapor samples were collected in the Nagqu River Basin in the middle of Tibetan Plateau between August and October in 2004. Results show that there exist some fluctuations of the δ^18O of atmospheric water vapor, especially before and after the monsoon＇s end.Moreover, the variety trend of the δ^18O of atmospheric water vapor inverse correlates with that of dew point. Precipitation events make an important effect upon the variation of δ^18O of atmospheric water vapor. During the whole sampling period, the δ^18O values of atmospheric water vapor are low while precipitation events occurred. The moisture origins w also contribute to the variation of δ^18O of atmospheric water vapor. The oceanic moisture transported by the southwest monsoon results in lower δ^18O of atmospheric water vapor in the Nagqu River Basin. Compared with the influence of the oceanic moisture, the δ^18O values, however, appear high resuiting from the effect of the continental air mass in this region.     

Study of altitudinal lapse rates of δ18O in precipitation/river water with seasons on the southeast Tibetan Plateau

Seasonal δ^18O variation in water on the southeast Tibetan Plateau has been studied, showing the consistent variation pattern of δ^18O with altitude indicative of relevant atmospheric circulation processes. Study shows a similar variation pattern of fixed-site river water δ^18O with that of the precipitation δ^18O in southeast Tibet. δ^18O in regional rivers in southeast Tibet demonstrates a gradual depletion with increasing altitude, though the rates vary seasonally. The most depleted river ^18O occurs during the monsoon period, with the lowest δ^18O/altitude lapse rate. The river ^18O during the westerly period is also depleted, together with low δ^18O/altitude lapse rate. The pre-monsoon rivers witness the most enriched ^18O with least significant correlation coefficient with the linear regression, whilst the postmonsoon rivers witness the largest δ^18O/altitude lapse rate. Different coherence of seasonal δ^18O variation with the altitude effect is attributed to different moisture supplies. Though sampling numbers vary with seasons, the δ^18O-H linear correlation coefficients all reach the 0.05 confidence level, thus witnessing the variation features of δ^18O in seasonal river water due to the influence of atmospheric general circulation and land surface processes revealed from the altitudinal lapse rates.     

The high-resolution climate recorded in the δ18O ofPorites lutea from the Nansha Islands of China

A Porites lutea core from Yongshu Reef of Nansha Islands covering 50 years growth history was analyzed for oxygen isotopic composition with monthly and seasonally resolution. The calibration of the δ ¹⁸O with the instrumental temperature indicated that the coral δ ¹⁸O is a good indicator for sea surface temperature (SST) and air temperature ( t ). It can be used to reconstruct the SST and air temperature of the Yongshu Reef sea area. In addition, the coral δ ¹⁸O provides signatures for the intensity of the East Asia monsoon and it is a record for the activities of El Niño events. With the calibrated SST and air temperature formulas, the most recent fifty years SST and air temperature were reconstructed based on the coral δ ¹⁸O, thus back up the understanding of the climate of Nansha Islands to 1950, far beyond the limit of the instrumental recording since September 1988. It was found that, in general, increasing 1℃ air temperature results in 0.24‰ decrease in skeletal δ ¹⁸O.