Flow and deposition of pyroclastic granular flows: A type example from the 1975 Ngauruhoe eruption,New Zealand

Small-volume pyroclastic density currents (PDCs) are generated frequently during explosive eruptions with little warning. Assessing their hazard requires a physical understanding of their transport and sedimentation processes which is best achieved by the testing of experimental and numerical models of geophysical mass flows against natural flows and/or deposits. To this end we report on one of the most detailed sedimentological studies ever carried out on a series of pristine small-volume PDC deposits from the 1975 eruption of Ngauruhoe volcano, whose emplacement were also witnessed during eruption. Using high-resolution GPS surveys, a series of lateral excavations across the deposits, and bulk sedimentological analysis we constrained the geomorphology, internal structure and texture of the deposits with respect to laterally varying modes of deposition.     

饱和正冻土水分迁移及冻胀模型研究

正冻土在温度梯度大的情况下,冻结锋面快速移动,孔隙水变成冰,造成原位体积膨胀;而通常在天然条件下,温度梯度都不大,水从未冻区向冻结区迁移,在某一个位置引起冰的累积,形成分凝冰。由于此诱发的冻胀要比原位冻胀大很多,因此,建立一个能够模拟土体水分迁移及分凝冰形成过程的冻胀模型尤其重要。基于第2冻胀理论,建立了饱和土体冻胀模型。在模型中,假设冻结缘中单位时间内水分迁移速度为常数,以计算冻结缘内水压力,再根据克拉方程得到冰压力。根据冰压力的大小作为分凝冰形成判据,研究中假设新的分凝冰形成以后,上一层分凝冰停止生长。模型把水分迁移和冻胀速率当作基本的未知量,模拟了与可天然土体冻胀类似的底部无压补水和顶部加压的冻胀情况。通过数值模拟与试验结果进行对比,初步验证模型的可靠性,其研究结果为实际寒区工程的冻胀预测提供参考。     

混合料贮料仓离析现象试验研究

针对混合料生产过程中贮料仓卸料时可能出现的离析现象,通过室内小型模拟试验,观测集料从仓体流出的过程,分析流出材料颗粒组成均匀性的变化特点。结果表明,混合料贮料仓卸料时的离析现象主要是由于细料向下渗透而产生的,集料下落时,细料在自重力作用下通过空隙结构向下渗透,集料发生离析;集料粒径比、分布宽度、平均粒径等因素的变化使料仓中形成不同的集料的空隙结构,使得细料的渗透作用的发生程度不同,从而引起集料离析程度的差异。     

Neighborhood racial–ethnic change and home value appreciation: evidence from Philadelphia

A limited number of studies have addressed residential self-selection when considering the relationship between the built environment (BE) and physical activity. Ignoring self-selection may bias the estimate of the strength of the relationship and misinform public policy. Using 2011 data from the Twin Cities, this study employs cross-sectional and quasi-longitudinal analyses to disentangle the impacts between self-selection (through residential preferences and travel attitudes) and neighborhood characteristics on active travel (AT). The two approaches produce somewhat different outcomes: attitudinal factors are extensively present in the cross-sectional analysis and the associations between neighborhood characteristics and AT are greatly attenuated after controlling for attitudinal factors. In contrast, neighborhood characteristics play a dominant role in the quasi-longitudinal analysis, while attitudinal and demographic characteristics carry additional impacts on AT. Overall, both preferences and attitudes help explain the difference in AT. I find that while physical activity infrastructure impacts biking, physical activity infrastructure together with transit and accessibility affects walking, even after controlling for demographic and attitudinal characteristics. The results highlight the importance of shaping the BE in order to provide an infrastructure of alternative modes of transport and access to different land uses in policy efforts to increase AT.     

Southern Suburb/Northern City: Black Entrepreneurship in Segregated Arlington County,Virginia

Most scholarship on racial segregation in U.S. cities retraces the Great Migration, from the rural South to the urbanizing, industrializing North. Arlington County, Virginia, adjacent to the large, prosperous black community of Washington, D.C., provides a unique opportunity to study processes that transcended this dichotomy. During segregation blacks were limited to living and doing business in three of the County's 38 census tracts. Using census data, telephone records, and interviews with black residents, this paper explores the black-owned businesses that grew in Arlington during segregation and the fate of those businesses following integration, concluding that the nature of the businesses was largely determined by the County's unique context. The black neighborhoods were dispersed, lacking public transportation, with insufficient residents to support the self-contained business infrastructure found in many segregated cities of similar size. Conversely Arlington's black residents were welcomed in the extensive black-owned business infrastructure of nearby Washington, D.C.     

The ethno-class trajectory of new neighborhoods in Israel

The subject of this article falls within the debate on the development of new neighborhoods beyond the hub of the metropolis and how this relates to planning from below. It regards new neighborhoods as being increasingly shaped through deliberate action in the form of public policy at the state and local levels. However, it emphasizes the central role of the government establishment, national institutions and ideologies in walling out and exclusionary practices. Research into four representative new neighborhoods in Israel, which were planned under the new spatial regime of the 1990s, reveals patterns of discrimination and ethno-class stratification that enable the preservation of nationalism and ethnic logic as the main, yet concealed, axis organizing social and spatial life.     

Middle Miocene to Quaternary primary basalt and high magnesian andesite magmas of North Hokkaido, Japan: Source mantle characteristics and degrees of partial melting

Abstract   Middle Miocene to Quaternary primitive basalts and high magnesian andesite (HMA) in North Hokkaido resulted from three periods of intense volcanism; early-stage (12–10 Ma), middle-stage (9–7 Ma) and late-stage (3–0 Ma). Based on the chemical compositions of olivines and chromian spinels and bulk chemistry of the primitive rocks, we examined depths of segregation of the calculated primary magmas and the degrees of partial melting of the source mantle. In the context of asthenospheric mantle upwelling, petrological data from the present study can be accounted for by the secular change in the depth of magma segregation from the upwelled asthenospheric mantle, which is composed of fertile peridotite. Thus, the early-stage primary magmas were generated by higher degrees of partial melting of the shallower part of hot asthenospheric mantle, whereas the middle- and late-stage primary magmas resulted from lower degrees of partial melting of a deeper part of the asthenospheric mantle. The early-stage HMA magma was generated by partial melting of the remnant subcontinental lithospheric mantle composed of refractory peridotite. This melting might have resulted from an increased geothermal gradient caused by upwelling of hot asthenosphere.     

Mapping the multiple geographies of mixed-ethnicity couples in Australia

Mixed-ethnicity partnerships are becoming increasingly common in Australia and other countries of high immigration. Formal and de facto marriages involving partners from different ethnic backgrounds are key indicators of decreasing social distance between groups. Yet mixed-ethnicity couples have received scant attention from Australian geographers. We use customised data from the 2011 Australian census to analyse the nation-wide distribution of several types of mixed-ethnicity couples. We focus on couples comprised of an Anglo-European (ethnic majority) partner, and a partner from a ‘visible’ ethnic minority group. Our analyses explore the residential geographies of mixed-ethnicity couples vis-à-vis ‘co-ethnic couples’ (where partners share the same ethnicity). We find that mixed-ethnicity couples are more widely dispersed across Australian cities and regions than comparative co-ethnic couples. However, each type of mixed-ethnicity couple has its own unique residential pattern: there are multiple geographies of mixed-ethnicity couples in Australia. These distinctive patterns reflect the migration and settlement histories of the couples’ constituent ethnic groups, but also hold great potential to shift seemingly entrenched ethnic residential geographies in the present and future.     

四川攀西地区几个小型镁铁-超镁铁岩体含矿性的铂族元素示踪

峨眉山大火成岩省内带,四川攀西地区的杨合伍、黄草坪和清水河等镁铁-超镁铁岩体分布在南北向的安宁河断裂和磨盘山-元谋断裂之间。分析表明,这些岩体无矿岩石与金宝山、杨柳坪、力马河等含矿岩体无矿岩石具有相似的铂族元素组成,普遍较高的Cu/Pd比值暗示这些岩体的母岩浆在侵入到目前层位前经历过硫化物熔离作用。定量模拟计算表明,原始岩浆经过大约0.01%的硫化物熔离作用形成了杨合伍岩体母岩浆,经过0.035%硫化物熔离形成了黄草坪和清水河岩体的母岩浆。根据硫化物熔离情况,认为杨合伍等岩体底部可能形成Ni-Cu-(PGE)硫化物矿床,而黄草坪和清水河岩体之下及附近可能存在Ni-Cu硫化物矿化的岩体。