基于宜出行大数据的多中心空间结构分析——以重庆主城区为例

多中心已成为中国大多数城市的空间发展战略,多中心结构的有效识别对于规划效果评价、规划策略制定具有重要意义。相比于百度热力与手机信令数据,腾讯宜出行数据具有时空分辨率高、获取成本低的优点,可精细比较城市主副中心的人口集聚能力,为多中心结构的动态识别提供新的手段。论文以重庆主城区为例,基于连续一周的宜出行热力数据,利用核密度分析等方法,识别其多中心城市结构、影响范围与组团发育情况。结果表明：作为山地城市,重庆在自然限制、经济驱动与规划引导下主动选择了“多中心、组团式”结构。重庆内环以内的各个城市中心人口高度集聚、用地规模相近、发育相对成熟,并强于内环以外的副中心。研究指出,西永、茶园副中心及外围组团的发展与人口集聚能力有待提高。     

SiCp/Mg复合材料的制备及其阻尼特性研究

采用搅拌铸造法在真空度为200 Pa的条件下制备得到含有微量氧化物的SiCp/Mg复合材料,通过显微组织观察和动态热机械分析等对其阻尼特性进行了研究。结果表明,所制备的SiCp/Mg复合材料基体晶界处分布着附着有氧化物的网状结构,且随着SiCp含量的增加,网状结构增多,且分布更加分散。此结构增大了位错密度和晶粒界面滑移,位错脱钉和界面滑移在振动过程中耗能量增大,因此所制备的SiCp/Mg复合材料具有理想的阻尼性能。     

Self-thinning Rules at Chinese Fir (Cunninghamia lanceolata) Plantations—Based on a Permanent Density Trial in Southern China

Data selection and methods for fitting coefficients were considered to test the self-thinning law. The Chinese fir (Cunninghamia lanceolata) in even-aged pure stands with 26 years of observation data were applied to fit Reineke’s (1933) empirically derived stand density rule (N $propto$ d¯ ^-1.605, N = numbers of stems, d¯ = mean diameter), Yoda’s (1963) self-thinning law based on Euclidian geometry (v¯ $propto$ N ^-3/2, v¯ = tree volume), and West, Brown and Enquist’s (1997, 1999) (WBE) fractal geometry (w¯ $propto$ d¯ ^-8/3). OLS, RMA and SFF algorithms provided observed self-thinning exponents with the seven mortality rate intervals (2%-80%, 5%-80%, 10%-80%, 15%-80%, 20%-80%, 25%-80% and 30%-80%), which were tested against the exponents, and expected by the rules considered. Hope for a consistent allometry law that ignores species-specific morphologic allometric and scale differences faded. Exponents α of N $propto$ d¯^α, were significantly different from -1.605 and -2, not expected by Euclidian fractal geometry; exponents β of w¯ $propto$ N^β varied around Yoda’s self-thinning slope -3/2, but was significantly different from -4/3; exponent γ of w¯ $propto$ d¯^γ tended to neither 8/3 nor 3.     

基于长期密度试验的杉木人工林自然稀疏线研究（英文）

采用杉木人工同龄纯林26年连续观测数据,拟合Reineke(1933)经典的林分密度效应法则、Yoda(1963)基于欧几里德几何的自疏法则以及West, Brown和Enquist的分形几何(1997, 1999)。通过OLS、RMA和SFF算法得到7种枯损率区间(2%-80%, 5%-80%, 10%-80%, 15%-80%, 20%-80%, 25%-80%and 30%-80%)的自稀疏指数,对这些指数与考虑的几种法则相应指数进行验证。发现Reineke密度效应法则的指数显著区别于-1.605和-2,而不是预想的欧几里德分形几何结果。Yoda自疏法则指数在-3/2左右变动,但显著区别于-4/3。West、Brown和Enquist的分形几何式中指数参数既不趋向于8/3,亦不趋向于3。     

海带CRY-DASH基因的克隆与转录表达分析

利用cDNA末端快速克隆(RACE)技术,获得海带(Saccharina japonica) CRY-DASH基因(SjCRYDASH)全长序列,结构分析发现,其ORF区长1779 bp,编码592个氨基酸。进行氨基酸同源序列比对,其与其他藻类和高等植物间存在两个重要辅基MTHF和FAD结合的保守域。通过不同光质照射诱导海带幼孢子体,发现蓝光、白光诱导1h后,均能使SjCRY-DASH转录水平上升,且SjCRY-DASH对蓝光的响应更强烈。本研究结果为研究大型褐藻-海带CRY-DASH受光诱导调控功能打下基础。     

多目标优选水下采油设施下放方法评价指标体系

水下采油设施下放是海上油气工程开发中的重要环节。经过长期发展,人们已研究出多种下放方法,但如何优选恰当的下放方法是尚待解决的问题。考虑海洋环境中可供数据源的复杂性、不确定性与不完整性,多目标、主客观要素并重是优选方法设计的重要准则。针对水下下放方法优选特点,建立对应评价指标体系。考虑评价指标体系多目标优选决策的特点,提出多目标非均一化灰色关联度模型;为更好地体现主客观要素并重并辩证表达决策者的主客观偏好,在非均一化处理中,运用回归原理与靶向偏差评价思想,提出变系数主客观权值修正模型。最后结合具体案例验证模型的可行性与有效性。结果表明,模型能够满足优选对象要求,对类似多目标主客观评价优选模型的建立具有一定借鉴意义。     

初始几何缺陷对UOE焊管屈曲压溃影响研究

UOE焊管经过一系列成型工艺可以得到高质量的成型结果,但管道截面仍存在一定初始几何缺陷,这将对管道性能产生明显影响。通过试验测定X65钢在循环载荷下的力学性能,并利用有限元分析软件对UOE焊管成型全过程进行模拟,分析主要成型参数对管道屈曲压溃压力的影响。分别采用有限元模拟和试验测量方法确定管道截面初始几何缺陷分布情况,并采用余弦函数形式拟合几何缺陷。结果表明,扩径阶段芯轴数目将对缺陷形式产生影响,且实际厚壁UOE管道几何缺陷形式更接近梨形而非椭圆形。评估厚壁UOE管道性能时,近似认为截面形式为椭圆形可能发生过于保守的问题。     

近千年来台湾以东黑潮主流区沉积物来源及其对气候波动的响应

基于AMS¹⁴C定年结果,对近千年来台湾以东黑潮主流区沉积物的粒度、黏土矿物组成及结晶学特征等进行研究,分析该区沉积特征、物质来源及近千年来环境演化的沉积记录。结果表明,台湾以东黑潮主流区沉积物主要为细粒的粉砂和黏土,沉积速率平均为34.44 cm/ka,低于东海陆架和冲绳海槽南部,高于开阔大洋,具有从陆架向大洋过渡的沉积特征。黏土矿物组成的分析结果表明,台湾以东黑潮主流区沉积物黏土矿物组成以伊利石(平均57%)和蒙脱石(平均25%)为主,含有少量绿泥石(平均16%),几乎不含高岭石(平均2%),其中蒙脱石主要来源于吕宋岛弧物质输送和附近海域原位的基性火山物质蚀变,伊利石和绿泥石主要来源于亚洲大陆风尘输送和台湾东部河流输入,高岭石主要来源于台湾东部河流和吕宋岛弧物质输入。黏土矿物的物源定量识别研究表明,研究站位的黏土矿物有26%～72%来源于亚洲大陆风尘输送,11%～55%来源于台湾东部河流输入,11%～26%来源于吕宋岛弧物质输送。近千年来沉积物物源的变化特征较好地反映了中世纪暖期、小冰期和现代暖期这3个百年尺度的全球性气候变化阶段。亚洲大陆风尘输送和台湾东部河流输入对研究区沉积物的相对贡献量变化反映了中世纪暖期较强的东亚冬季风特征和台湾地区较为干旱的气候环境,同时也反映了小冰期逐渐减弱的东亚冬季风强度和台湾地区较为湿润的气候环境。现代暖期和中世纪暖期在东亚热力差异和降水异常上的差别反映了人类活动对沉积物的扰动。而研究区小规模的沉积特征突变事件主要与暴雨、台风和地震活动相关。     

巴伦支海海冰多年变化及其影响因子研究

本文采用1900—2010年ECMWF海冰密集度、海面温度、风场和NCAR北极涛动等长序列资料,运用EOF分解、线性回归和相关分析等统计方法,分析了巴伦支海海冰年际变化特征及其与影响因子之间的关系。结果表明:巴伦支海海冰面积4月最大,9月最小,每年减少约1653km^2;面积距平正负位相交替出现,1969年后以负距平为主,冰情先重后轻;密集度逐月不同,明显降低的区域呈现“中部偏东—中部—东北部—西北部—中部偏东”转移特点,部分区域每年减少0.006以上;密集度变化的空间特征可由密集度EOF第一主模态表示,与温度的相关系数高于风场;海冰面积与AO呈负相关。我国以往单独针对巴伦支海海冰变化的研究较少,本文丰富了这方面的资料,对浮式平台开发冰区油气资源提供初步参考。     

Structural analysis and anti-complement activity of polysaccharides extracted from Grateloupia livida (Harv.) Yamada

Polysaccharides were extracted from Grateloupia livida(Harv.) Yamada using hot water(extracted product denoted WGW) and then degraded in dilute sulfuric acid(degraded product denoted WGWD). The degraded mixture was then separated into four fractions through anion exchange chromatography on 2-diethylaminoethanol(DEAE)-Bio-Gel Agarose FF gel. Electrospray ionization collision-induced dissociation tandem mass spectrometry(ESI-CID-MS/MS) was performed to elucidate the structural features of all fractions. In combination with nuclear magnetic resonance spectroscopy(NMR)and infrared spectroscopy(IR) data, the major polysaccharide structures were concluded to be μ-carrageenan and κ-carrageenan. μ-Carrageenan usually has a backbone of alternating 1,3-linked β-D-galactopyranose residues sulfated at C-4 and 1,4-linked a-D-galactopyranose residues sulfated at C-6, while κ-carrageenan consists of alternating 1,3-linked β-D-galactopyranose residues sulfated at C-4 and 1,4-linked a-D-3,6-anhydrogalactopyranose residues. Trace v-carrageenan, composed of 1,3-linked β-D-galactopyranose residues sulfated at C-4 and 1,4-linked a-D-galactopyranose residues sulfated at C-2 and C-6, was also detected. Furthermore, the polysaccharide had a backbone comprising 1,3-linked β-D-galactopyranose and1,4-linked α-L-galactopyranose sulfated at C-6, which is the agarose precursor. The hydroxy groups in the galactopyranose were partially substituted by methyl and pyruvic acid acetal(PA) groups. The anticomplementary activities of WGW and its derivatives against classical pathways were measured. The native polysaccharides in WGW had higher activities, while the derivatives had much weaker activities. This indicated that the molecular weight and sulfate content were important factors affecting the anti-complement activity.