City-Suburb Differences in African American Male Labor Market Achievement

This research tests the spatial mismatch hypothesis by comparing the employment probabilities of central city versus suburban African American males in nine metropolitan areas. Treatment effects models are used to control for the effects of both individual characteristics and residential self-selection on the probability of employment. A positive effect of suburban residential location on employment is found for the residents of Dallas, Los Angeles, New York, and Washington, while no effect is found for the residents of Cleveland, Houston. Jackson, Memphis, and Newark. The general conclusion to be drawn is that the spatial mismatch effect is contingent on the particular characteristics of each metropolitan area. Preliminary analysis shows that metropolitan areas with a spatial mismatch effect are large in terms of total population and total land area, and have less efficient transportation systems.     

Discarded containers on a kent beach

Winter beach surveys of discarded containers at Sandwich Bay showed a wide range of fabrication materials and contents. These were manufactured world-wide and probably distributed by seaborne disposal from local shipping. Although blow moulded polyethylene bottles containing toilet cleansers were commonly observed, there was no evidence to indicate an accumulation of these items in the marine environment.     

Proximity to Job Opportunities and African American Male Unemployment: A Test of the Spatial Mismatch Hypothesis in Indianapolis

Despite the lack of substantive research, the spatial mismatch hypothesis remains a pervasive explanation for the high rate of African American male unemployment. This research tests the hypothesis that census tract African American male unemployment rates are negatively related to the number of local job opportunities. This hypothesis is tested for Marion County, Indiana, the central county of the Indianapolis MSA. Weighted partial correlation coefficients of the logit of African American male census tract unemployment rates and indices of the availability of local job opportunities in manufacturing, services, and retail trade are statistically insignificant. The findings reject the spatial mismatch hypothesis in the specific context of Indianapolis in 1990.     

Geological and structural controls on gold mineralization in the Tanami District, Northern Territory

Gold mineralization in the Tanami district is hosted within moderately northwest dipping turbiditic sedimentary and basaltic volcanic rocks of the Paleoproterozoic Mt. Charles Formation. The gold occurs within a complex sinistral wrench-fault array and associated veins and alteration haloes. The main mineralized faults have a northerly trend and dip steeply east. Subsidiary structures trend at 030° and 070° and dip towards the southeast. Paleostress calculations based on fault striation populations and geometry (strike and dip) of faults indicate that at the time of the mineralizing event, σ ₁ was sub-horizontal and SE–NW directed with σ ₂ subvertical. Structural studies indicate that the mineralization occurred after the regional folding event and synchronous with the emplacement of felsic dykes into the mine sequence. Gold veins in the Tanami district are interpreted to be part of an outer thermal aureole gold system that formed during the emplacement of granitoids in the nearby ∼1,815 to ∼1,799 Ma Frankenia and/or Coomarie domes. Economic gold mineralization occurred late in the paragenetic history of the district. Gold is hosted by quartz-carbonate veins within shear zones, and also in the surrounding sericite- quartz- pyrite ± carbonate-altered wallrocks. Gold-mineralized veins precipitated at depths of 3 to 6 km from high temperature (∼300°C), low salinity (∼5 wt% NaCl equivalent) fluids with low CO₂ contents. Barren quartz, dolomite and calcite veins that occur in pre- and post-mineralization thrust faults formed from high salinity (∼20 wt% NaCl equivalent), low temperature (∼120–150°C) basinal brines. Pyrite in the gold mineralized veins and alteration halos has lower δ ³⁴S values (6.8 to 12.5‰) than local diagenetic pyrite (17.8 to 19.2‰) or pyrite in pre-mineralization thrust faults (31.7 to 37.1‰). The mineralizing fluids are inferred to have contained a well-homogenized mixture of magmatic and sedimentary-derived sulfur. Editorial handling: D. Huston     

Meteor shower detection with density‐based clustering

We present a new method to detect meteor showers using the density‐based spatial clustering of applications with noise algorithm (DBSCAN; Ester et al. 1996 ). The DBSCAN algorithm is a modern cluster detection algorithm that is well suited to the problem of extracting meteor showers from all‐sky camera data because of its ability to efficiently extract clusters of different shapes and sizes from large data sets. We apply this shower detection algorithm on a data set that contains 25,885 meteor trajectories and orbits obtained from the NASA All‐Sky Fireball Network and the Southern Ontario Meteor Network (SOMN). Using a distance metric based on solar longitude, geocentric velocity, and Sun‐centered ecliptic radiant, we find 25 strong cluster detections and six weak detections in the data, all of which are good matches to known showers. We include measurement errors in our analysis to quantify the reliability of cluster occurrence and the probability that each meteor belongs to a given cluster. We validate our method through false‐positive/negative analysis and with a comparison to an established shower detection algorithm.     

西藏恰功铁矿成矿斑岩出溶流体特征及成矿潜力

1 成矿地质背景恰功铁矿位于西藏日喀则地区谢通门县春哲乡境内,大地构造位置处于印度-亚洲陆陆碰撞带雅江缝合带北部拉萨地体中.矿区内出露地层包括上白垩统的塔克那组、古近纪林子宗火山岩底部层位的典中组.     

安徽庐江—枞阳地区A型花岗岩的LA-ICP-MS定年及其地质意义

本文对安徽庐江-枞阳地区产出的A型花岗岩体(碱性侵入岩体)进行了锆石LA-ICP-MS U-Pb同位素年代学研究.结果表明,城山岩体、花山岩体、黄梅尖岩体和枞阳岩体的形成年龄分别为126.5±2.1Ma、126.2 ±0.8Ma、125.4±1.7Ma和124.8±2.2Ma,均形成于早白垩世126～124Ma之间.这些岩体的硅含量和全碱含量均较高,准铝质;稀土含量中等,强Eu亏损,呈略右倾的海鸥型稀土配分模式,均为A1型花岗岩.结合长江中下游地区高碱钙碱性侵入岩和盆地内火山岩的研究成果,本文认为126～124Ma是长江中下游地区地壳伸展最强烈的阶段,这一研究成果时探讨长江中下游地区早白垩世早期的动力学背景具有重要的意义.     

Urban greening,property and more-than-human commoning

ABSTRACT

Urban greening is about bringing vegetation into cities in ways that produce flourishing urban ecologies whilst also making cities more liveable for human inhabitants. We focus here on greening that is done through the maintenance or establishment of gardens, parks, urban forests and informal spaces. We argue that in contexts with established property law systems, such as Australia, making urban ecologies through greening is shaped heavily by relations of property tied to land. This includes constraining the extent to which urban greening can contribute to socio-ecologically just cities. We suggest that progressing greening that is more attentive to the geographies and temporalities of more-than-human life requires us to trouble the hold of property over greening. To do this we explore the possibilities opened up by the lens of urban commons/commoning. We engage with the emerging concept of more-than-human commoning as a way of attuning urban greening to nonhuman agency and affordances. We also grapple with the risk of obscuring or concealing difference between humans in the way commoning makes room for more-than-humans, especially in the context of settler-colonialism. We conclude by calling for a more overt politics of urban greening that encompasses diverse human and more-than-human experiences of the city.     

Antibiotic resistance in coliform and faecal coliform bacteria from natural waters and effluents

Coliform and faecal coliform bacteria isolated from potable water supplies (springs and wells), streams, seawater, and effluents were examined for the incidence of antibiotic resistance. More than 40% of the coliform and faecal coliform bacteria isolated from drinking water supplies were resistant to one or more antibiotics. In stream and seawater samples, the incidence was increased to more than 60%, and to more than 70% among faecal coliforms isolated from effluents. Approximately 40% of the isolates resistant to streptomycin or tetra‐cycline were able to transfer their resistance determinants to an antibiotic‐sensitive strain of Escherichia coli within 2 h.

Although the widespread use of antibiotics is perhaps the major selective force favouring the increased incidence of antibiotic‐resistant bacteria, antibiotic‐resistant faecal coliforms may also have a selective advantage in natural waters.     

Water quality of the Waiohewa Stream,Rotorua

The chemical quality of the Waiohewa stream, Rotorua, was assessed from the results of 2 longitudinal surveys in summer 1978–79. In particular, changes in nitrogen concentration were examined. The quantity of ammonia increased downstream from unmonitored geothermal inputs, but, after dilution and neutralisation by a larger inflow of freshwater, considerable proportions of ammonia were converted to nitrate. In the first survey ammonia concentrations decreased from 4.48 to 2.47 g m^‐3 and nitrate concentrations increased from 0.59 to 1.13 g ^‐3 in a 3‐km stretch of the stream. Mass flow calculations show that nitrification could account for at least 55% of the ammonia decrease, the rest probably being lost through assimilation or denitrification. Laboratory incubation experiments showed that nitrification occurred in the stream bed. The geothermal waters contained low concentrations of boron (1.1–4.0 g m^‐3), filterable mercury (0.1–0.8 mg m^‐3) and arsenic (10–14 mg m^‐3).