新疆易灾暴雨的风险区划

将降水量作为新疆易灾暴雨的风险区划指标,对新疆106个气象站1961年以来4-9月的暴雨（≥24mm）降水过程进行分析,确定不同时间尺度各级易灾暴雨的临界致灾雨量指标.选用降水强度和频次来表征易灾暴雨的危险性,利用加权综合评价法和GIS中自然断点分级法,将致灾暴雨的危险性指数按高、次高、中等、次低、低危险区5个等级进行...     

新疆和田阿拉玛斯软玉成因

新疆和田阿拉玛斯矿床中的软玉矿体在花岗闪长岩和白云质大理岩中以脉状和透镜状产出。花岗闪长岩和白云质大理岩之间出现水平和垂直方向分布的软玉分带结构,这种分带包括镁铁尖晶石、透辉石、透闪石、青玉、青白玉、白玉和蛇纹石化白云质大理岩等矿物分带。采用电子探针和ICP-MS对这些白玉、青白玉和青玉的分带进行分析。这些软玉中的Cr (Cr=8.95×10^-6～178.7×10^-6) 和Ni (NiO=0.05×10^-6～3.95×10^-6) 的含量远低于与蛇纹石有关的软玉中的相关含量(Cr₂O₃=0.07%～0.43%,NiO=0.08%～0.36%)。软玉化学成分显示从白玉、青白玉到青玉的颜色变化主要与Fe元素的含量升高有关而与Cr、Mn等元素的含量关系不明显。花岗闪长岩和白云质大理岩之间的矿物分带显示了软玉分带的形成温度从高温到低温的变化、矿物从无OH^-到含OH^-的变化和透闪石颗粒从青玉到白玉不断变小。这些地质特征尤其是软玉分带现象表明了阿拉玛斯矿点是一个与白云质大理岩有关的接触交代成因的透闪石质软玉矿床。     

华南铀矿类型、特点及其空间分布

华南是我国重要产铀区,铀矿类型包括花岗岩型、斑岩型、火山岩型、碳硅泥岩型和砂岩型,文章认为,花岗岩型是指与花岗岩体有关的一类热液铀矿床的代称,斑岩型是指与各类斑岩体有关的一类热液铀矿床的代称,碳硅泥岩型是指与碳硅泥岩层有关的层控铀矿床的代称,砂岩型是指与中新界砂岩层有关的层控铀矿床的代称.总体看,从华南西部向东部,铀矿...     

一种求和法及其应用

为了用泛函的方法解决收敛问题,通过应用拓扑向量空间的一些性质,将一个序列到另一个序列的变化看作是变换,得到复距离空间中一些序列收敛性的等价条件.改进和推广了Abel定理,Mertens定理,O.Stolze公式等.     

湖南省雷电灾害易损性分析及区划

为了对各地防雷减灾工作提供比较科学的理论指导,利用2002-2008年湖南省14个市的雷电灾害统计资料,结合湖南省各市的经济发展状况和人口密度特征,引用雷击密度、雷电灾害频度、生命易损模数以及经济易损模数作为各市雷电灾害易损性评估指标,得出各市综合易损性指标,最后形成湖南省雷电灾害易损度区划。结果表明:某一地区雷击灾害的发生以及其造成的损失不仅与该地区所处的地理位置、气候环境有关,也与该地的人口密度、经济发展有关。     

海洋功能区划控制体系研究

合理利用海域、改善海洋环境质量和降低海洋开发利用活动负外部性,都需要通过加强海洋开发利用活动的控制来实现,而海洋功能区划是控制和管理开发利用活动的重要手段和工具。从文本控制、图则控制、指标控制、海域使用全过程控制四个方面构建了海洋功能区划控制体系,其中文本控制由目标、原则和文本条款组成;图则控制由图则边界、用海类型和管理要求组成;指标控制由规模控制、结构控制、利用方式控制、海域使用强度和效率控制、环境控制指标构成;海域使用全过程控制由建设期、运行期和结束后构成。通过构建海洋功能区划控制体系,有助于区划目标     

基于海洋功能区的海域使用结构优化模型初探

探讨了海域使用结构形成机制,海域使用结构是受海洋资源结构约束,受消费结构引导,通过海洋产业落实到海域空间:分析了海域使用结构现状和变化趋势,结果显示渔业用海呈下降趋势,工业用海呈上升趋势;并以各类海洋功能区为基础,构建了海域使用结构优化模型,为海域使用结构调整提供定量化技术依据.     

Amino acid composition and functional properties of giant red sea cucumber (Parastichopus californicus) collagen hydrolysates

Giant red sea cucumber (Parastichopus californicus) is an under-utilized species due to its high tendency to autolysis.The aim of this study was to evaluate the functional properties of collagen hydrolysates from this species.The degree of hydrolysis (DH),amino acid composition,SDS-PAGE,emulsion activity index (EAI),emulsion stability index (ESI),foam expansion (FE),and foam stability (FS) of hydrolysates were investigated.The effects of pH on the EAI,ESI FE and FS of hydrolysates were also inves-tigated.The results indicated that the β and α1 chains of the collagen were effectively hydrolyzed by trypsin at 50℃ with an En-zyme/Substrate (E/S) ration of 1:20 (w:w).The DH of collagen was up to 17.3% after 3 h hydrolysis with trypsin.The hydrolysates had a molecular weight distribution of 1.1 17 kDa,and were abundant in glycine (Gly),proline (Pro),glutamic acid (Glu),alanine (Ala) and hydroxyproline (Hyp) residues.The hydrolysates were fractionated into three fractions (< 3 kDa,3 10 kDa,and > 10 kDa),and the fraction of 3 10 kDa exhibited a higher EAI value than the fraction of > 10 kDa (P<0.05).The fraction of > 10 kDa had higher FE and FS values than other fractions (P<0.05).The pH had an important effect on the EAI,ESI,FE and FS.All the fractions showed undesirable emulsion and forming properties at pH 4.0.Under pH 7.0 and pH 10.0,the 3 10 kDa fraction showed higher EAI value and the fraction of > 10 kDa showed higher FE value,respectively.They are hoped to be utilized as functional ingredients in food and nutraceutical industries.     

Petrography of Yamato 984028 lherzolitic shergottite and its melt vein: Implications for its shock metamorphism and origin of the vein

Yamato 984028 (Y984028) is a newly identified lherzolitic shergottite, recovered from the Yamato Mountains, Antarctica, in 1999. As part of a consortium study, we conducted petrographic observations of Y984028 and its melt vein in order to investigate its shock metamorphism. The rock displays the typical non-poikilitic texture of lherzolitic shergottite, characterized by a framework of olivine, minor pyroxene (pigeonite and augite), and interstitial maskelynite. Shock metamorphic features include irregular fractures in olivine and pyroxene, shock-induced twin-lamellae in pyroxene, and the complete conversion of plagioclase to maskelynite, features consistent with those found in other lherzolitic shergottites. The melt vein is composed of coarse mineral fragments (mainly olivine) entrained in a matrix of fine-grained euhedral olivine (with several modes of compositional zoning) and interstitial glassy material. Some coarse olivine fragments consist of an assemblage of fine-grained euhedral to subhedral olivine crystals, suggesting shock-induced fragmentation, recrystallization, and/or a process of sintering. The implication is that the fine-grained olivine crystals in the matrix of the melt vein represent complicated crystallization environments and histories.     

基于主体功能区的循环经济发展模式研究

推动不同主体功能区的循环经济发展是转变我国地区经济增长方式的重要途径之一.以优化开发区、重点开发区、限制开发区与禁止开发区四大类型主体功能区为基础,根据各地方循环经济的具体实践,归纳不同区域范围内循环经济发展的类型、动力、特点及未来方向,并针对经济水平、资源禀赋等差异进一步细分为8种循环经济模式,有助于循环经济生产方式与国家宏观空间格局的适应与融合.