水资源约束下西北干旱区城市经济发展与城市化阈值

城市化水平阈值是指在水资源硬约束下,在确保经济发展达到一定速度与规模、生态环境建设得到基本保障、并具备足以支撑城市接纳一定数量农民进城转为非农人口的经济能力时,能达到的“农转非”人口占总人口的最大比例。以干旱区河西走廊为例,分析了在水资源约束下城市经济发展总量及其对应的城市化阈值。采用阈值模型计算表明,未来30a在不跨区调水的前提下,河西走廊总需水量的上限阈值为7.81×109m3,其中生态需水、生产需水和生活需水比例调整为13.2:83.5:3.3,总需水量对应的国内生产总值为1.81×1011元,历年平均增长速度最快可达到6.91%,第一、二、三产业结构调整为18.99:47.20:33.81。在总需水量阈值、经济总量、需水结构与产业结构调整优化和经济增长速度不低于7%、农业需水按0.61%的速度退水9.12×108m3、生态需水比例不低于13%等多重条件约束下,求得河西走廊未来30a能够达到的总人口为5.82×106人,城镇非农业人口可达到2.05×106人,城市化水平可达到35.14%,这一水平仅相当于中国2001年的平均城市化水平。在跨区调水1.31×109m3的条件下,城市化水平可望达到47.17%。进而采用总人口人均拥有的GDP、非农业人口人均拥有的第二、三产业增加值、农业人口人均拥有的第一产业增加值3项经济指标对水资源约束下经济发展总量对城市化水平的保障程度进行了验证分析。由于各城市的缺水状况、取水条件、发展性质、发展阶段与经济发展实力与前景等各不相同,致使不同城市之间对应的总需水量、经济总量、经济增长速度和城市化水平等均表现出较大的差异性。     

超抗原SEA增强小鼠对HBV DNA 疫苗的免疫反应

观察超抗原SEA(D227A)的真核表达载体(pmSEA),对HBVDNA疫苗诱导Balbc小鼠(H2d)免疫应答的调节作用。肌内注射空载体pcDNA3、HBVDNA疫苗加pmSEA佐剂(pHBVS2S+pmSEA)或不加佐剂(pHBVS2S);ELISA法测定血清抗HBs;ELISPOT检测分泌IFNγ的脾淋巴细胞;4h51Cr释放法检测小鼠脾细胞CTL活性。HBVDNA佐剂组免疫小鼠抗HBsAg抗体滴度明显高于不加佐剂组,其IgG1IgG2a的比例不同于多肽免疫组,二者分别为0.282与10。HBVDNA佐剂组均能增强IgG1和IgG2a的产生,是不加佐剂组的1.36、1.73倍。佐剂组小鼠脾淋巴细胞IFNγ的分泌量是不加佐剂组2～3倍。CTL细胞杀伤活性(E:T=100)佐剂组与不加佐剂组分别为:69.77%±7.5%、42.81%±7.7%,差异显著(P<0.05)。HBVDNA疫苗具有较强的免疫原性,能够诱导机体产生特异性的抗体及CTL反应;pmSEA佐剂能够提高小鼠对DNA疫苗的免疫应答,有望成为DNA疫苗的免疫佐剂。     

城市景观功能的区域协调规划——以深圳市为例

城市景观功能的完善是城市可持续发展的重要保障之一,其与区域景观功能的相互协调是城市规划的重要组成部分,有利于城市和区域的整体持续发展。在分析城市景观基本特征的基础上,探讨了城市景观功能区域协调规划的基本思路,以城市景观为规划对象,以人类社会的功能需求为立足点,依据景观生态学理论,将城市景观的功能划分为生物生产功能、环境服务功能、文化支持功能和信息输运功能,对体现这些基本功能的景观类型进行区域协调规划。以深圳市为例,实证分析了其景观功能在珠江三角洲地区的协调规划。     

一种新的乙型肝炎病毒表面抗原结合蛋白的筛选、表达及其生物学活性的初步研究

为了研究乙肝病毒侵染肝细胞过程中的功能蛋白 ,通过印迹免疫分析技术从人肝cDNA噬菌体表达库中筛选出一株编码乙肝表面抗原结合蛋白 (hepatitisBsurfaceantigenbindingprotein ,HBsAg BP)的cDNA克隆 .基因测序结果表明 ,该cDNA具有独立的开放阅读框架 ,编码 1个由 344个氨基酸残基构成的可溶性蛋白分子 ,属于免疫球蛋白超家族成员 .将该基因克隆到原核表达载体pTriplEx后 ,在E .coliXL1 Blue菌株中获得 4 4kD的重组蛋白 .重组蛋白经Western印迹和ELISA实验证明具有与乙肝表面抗原特异性结合的能力 .进一步经流式细胞仪实验显示 ,在纯化的重组蛋白存在的情况下 ,天然的HBsAg与肝细胞株HepG2的亲和力显著增高 .结果显示 ,该乙肝表面抗原结合蛋白可能是介导乙肝病毒对肝细胞亲和侵染的可溶性辅助受体 .     

蛋白质组学研究中的一种新方法——配体垂钓

基于表面等离子共振技术的配体垂钓技术能在蛋白质组水平上研究蛋白质的相互作用与功能,提供控制细胞功能的新靶标．其通过将受体固定在芯片表面,当被检测样品流过芯片表面时,配体与受体相结合, 实现俘获未知的相互作用的伙伴蛋白或复合体,并结合质谱技术鉴定出未知蛋白及其序列．     

Functional studies with membrane-bound and detergent-solubilized α2-adrenergic receptors expressed in Sf9 cells

A chip-based biosensor technology using surface plasmon resonance (SPR) was developed for studying the interaction of ligands and G protein-coupled receptors (GPCRs). GPCRs, the fourth largest superfamily in the human genome, are the largest class of targets for drug discovery.We have expressed the three subtypes of α₂-adrenergic receptor (α₂-AR), a prototypical GPCR as functional fusion proteins in baculovirus-infected insect cells. The localization of the expressed receptor was observed in intracellular organelles, as detected by eGFP fluorescence. In addition, the deletion mutants of α_2B-AR, with a deletion in the 3rd intracellular loop, exhibited unaltered K_d values and enhanced stability, thus making them more promising candidates for crystallization. SPR demonstrated that small molecule ligands can bind the detergent-solubilized receptor, thus proving that α₂-AR is active even in a lipid-free environment. The K_d values obtained from the biosensor analysis and traditional ligand binding studies correlate well with each other. This is the first demonstration of the binding of a small molecule to the detergent-solubilized state of α₂-ARs and interaction of low-molecular mass-ligands in real time in a label-free environment. This technology will also allow the development of high throughput platform for screening a large number of compounds for generation of leads.     

Premicellar complexes of sphingomyelinase mediate enzyme exchange for the stationary phase turnover

During the steady state reaction progress in the scooting mode with highly processive turnover, Bacillus cereus sphingomyelinase (SMase) remains tightly bound to sphingomyelin (SM) vesicles (Yu et al., Biochim. Biophys. Acta 1583, 121-131, 2002). In this paper, we analyze the kinetics of SMase-catalyzed hydrolysis of SM dispersed in diheptanoylphosphatidyl-choline (DC₇PC) micelles. Results show that the resulting decrease in the turnover processivity induces the stationary phase in the reaction progress. The exchange of the bound enzyme (E*) between the vesicle during such reaction progress is mediated via the premicellar complexes (E_i^#) of SMase with DC₇PC. Biophysical studies indicate that in E_i^# monodisperse DC₇PC is bound to the interface binding surface (i-face) of SMase that is also involved in its binding to micelles or vesicles. In the presence of magnesium, required for the catalytic turnover, three different complexes of SMase with monodisperse DC₇PC (E_i^# with i = 1, 2, 3) are sequentially formed with Hill coefficients of 3, 4 and 8, respectively. As a result, during the stationary phase reaction progress, the initial rate is linear for an extended period and all the substrate in the reaction mixture is hydrolyzed at the end of the reaction progress. At low mole fraction (X) of total added SM, exchange is rapid and the processive turnover is limited by the steps of the interfacial turnover cycle without becoming microscopically limited by local substrate depletion or enzyme exchange. At high X, less DC₇PC will be monodisperse, E_i^# does not form and the turnover becomes limited by slow enzyme exchange. Transferred NOESY enhancement results show that monomeric DC₇PC in solution is in a rapid exchange with that bound to E_i^# at a rate comparable to that in micelles. Significance of the exchange and equilibrium properties of the E_i^# complexes for the interpretation of the stationary phase reaction progress is discussed.     

Evaluating the efficacy of planktonic foraminifer calcite δO data for sea surface temperature reconstruction for the Late Miocene

This study examines the efficacy of published δ¹⁸O data from the calcite of Late Miocene surface dwelling planktonic foraminifer shells, for sea surface temperature estimates for the pre-Quaternary. The data are from 33 Late Miocene (Messinian) marine sites from a modern latitudinal gradient of 64°N to 48°S. They give estimates of SSTs in the tropics/subtropics (to 30°N and S) that are mostly cooler than present. Possible causes of this temperature discrepancy are ecological factors (e.g. calcification of shells at levels below the ocean mixed layer), taphonomic effects (e.g. diagenesis or dissolution), inaccurate estimation of Late Miocene seawater oxygen isotope composition, or a real Late Miocene cool climate. The scale of apparent cooling in the tropics suggests that the SST signal of the foraminifer calcite has been reset, at least in part, by early diagenetic calcite with higher δ¹⁸O, formed in the foraminifer shells in cool sea bottom pore waters, probably coupled with the effects of calcite formed below the mixed layer during the life of the foraminifera. This hypothesis is supported by the markedly cooler SST estimates from low latitudes—in some cases more than 9 °C cooler than present—where the gradients of temperature and the δ¹⁸O composition of seawater between sea surface and sea bottom are most marked, and where ocean surface stratification is high. At higher latitudes, particularly N and S of 30°, the temperature signal is still cooler, though maximum temperature estimates overlap with modern SSTs N and S of 40°. Comparison of SST estimates for the Late Miocene from alkenone unsaturation analysis from the eastern tropical Atlantic at Ocean Drilling Program (ODP) Site 958—which suggest a warmer sea surface by 2-4 °C, with estimates from oxygen isotopes at Deep Sea Drilling Project (DSDP) Site 366 and ODP Site 959, indicating cooler than present SSTs, also suggest a significant impact on the δ¹⁸O signal. Nevertheless, much of the original SST variation is clearly preserved in the primary calcite formed in the mixed layer, and records secular and temporal oceanographic changes at the sea surface, such as movement of the Antarctic Polar Front in the Southern Ocean. Cooler SSTs in the tropics and sub-tropics are also consistent with the Late Miocene latitude reduction in the coral reef belt and with interrupted reef growth on the Queensland Plateau of eastern Australia, though it is not possible to quantify absolute SSTs with the existing oxygen isotope data. Reconstruction of an accurate global SST dataset for Neogene time-slices from the existing published DSDP/ODP isotope data, for use in general circulation models, may require a detailed re-assessment of taphonomy at many sites.     

城市胁迫生境下二球悬铃木叶片的发育稳定度及其环境指示功能

对采自上海市区14个样点的二球悬铃木叶片发育稳定度、叶片气孔密度和气孔长径进行研究。结果表明,在3个采样时期,根据叶片宽度确定的非稳态不对称指数(FA1)和根据叶片侧脉长度确定的偏向性不对称指数(RDA1)在不同环境胁迫程度(UESL)下均表现出显著的差异,但进一步分析表明,各样点FA1与环境胁迫程度UESL之间呈显著的非线性回归关系,而RDA1与环境胁迫程度之间却未显示类似关系。此外,FA1与叶片气孔密度和气孔长径之间的显著相关关系表明,它们可共同作为指示小尺度上环境胁迫的有效指标,而RDA1是叶片的一种正常发育状态参数,并不适于反映环境胁迫状态。     

城市生态系统景观格局特征及形成机制

以城市生态系统的格局一过程一功能等相关概念的辨析为基础,重点分析了城市景观格局的基本特征,以及城市格局对生态系统过程和功能的影响。结果表明,高度人工化、高度的时空异质特性、破碎性、不稳定性是城市景观格局最为显著的特征。城市所在区域的自然环境条件,历史文化传统,城市格局的基本骨架——交通系统和城市职能是影响城市格局形成和演变的重要驱动因素。城市景观结构决定了其生态过程。综合研究城市景观格局-过程-功能的关系,认识城市的发展演变过程,可为城市规划、建设和管理提供重要的科学基础。