Classification of five new ordinary chondrites (RC 073, 074, 076–078) from Roosevelt County,New Mexico

Abstract— Five new ordinary chondrites from Roosevelt County, New Mexico, USA, have been assigned to a chemical group, petrologic type and shock stage. All five are moderately to heavily weathered. They are: RC 073, H5(S2); RC 074, L5(S3); RC 076, L4(S3); RC 077 , L4(S2); RC 078, L4(S2).     

Adding Human Health Risk Analysis Tools to Geographic Information Systems

The development of a module for performing human health risk analysis is presented. This risk module differs from other tools in that it is integrated into a geographic information system (GIS) in a plug–in fashion. The main challenge in the development of the risk module was handling the many different spatial data structures in an open GIS environment. Selection of programming language and other development issues are discussed. The application of the risk module to two mining activities in Bolivia is described.     

Critically Understanding Race‐Connected Practices: A Reading of W. E. B. Du Bois and Richard Wright

In this article, I argue that race‐connected practices should be understood in their appropriate historical and geographical context. While race is mediated by language, texts, and interpretation, a reading of W. E. B. Du Bois and Richard Wright suggests that it is in some fundamental sense beyond text, located in space and time.     

Soil erosion in the Falkland Islands: an assessment

Observations and data concerning soil erosion on clay-rich, sand-rich and organic soil materials are reported for the Falkland Islands, South Atlantic, where soil erosion is both widespread and currently active, though rather uneven in its distribution. The most extensively eroded areas are located on coastal sand deposits and where sandy soils occur at inland sites. There is evidence that some erosion is natural and was initiated before the Islands were settled; other erosion is of more recent origin and can be associated with land management practices, principally grazing management, stocking rates, and the frequency and intensity of pasture burning. The impact of soil erosion on the agricultural economy of the Islands appears to be negligible and it is not perceived to be an important environmental issue. This lack of concern probably arises because the on-farm and off-farm costs of erosion have never been determined and there are no data relating to rates of erosion. It is suggested that a research programme be established aimed at monitoring erosion rates, assessing land use practices that initiate erosion, and assessing the costs of erosion. Furthermore, guidelines for soil conservation should be established. If pasture burning is to continue, a recommended code of practice should be drawn up. Given the importance of the sheep industry to the Falkland Islands, it is desirable that the grazing potential be maintained.     

Ambient vibration measurements on a cable-stayed bridge

An extensive programme of full-scale ambient vibration tests has been conducted to measure the dynamic response of a 542 m (centre span of 274 m) cable-stayed bridge—the Quincy Bayview Bridge in Illinois. A microcomputer-based system was used to collect and analyse the ambient vibration data. A total of 25 modal frequencies and associated mode shapes were identified for the deck structure within the frequency range of 0–2 Hz. Also, estimations were made for damping ratios. The experimental data clearly indicated the occurrence of many closely spaced modal frequencies and spatially complicated mode shapes. Most tower modes were found to be associated with the deck modes, implying a considerable interaction between the deck and tower structure. No detectable levels of motion were evident at the foundation support of the pier. The results of the ambient vibration survey were compared to modal frequencies and mode shapes computed using a three-dimensional finite element model of the bridge. For most modes, the analytic and experimental modal frequencies and mode shapes compare quite well, especially for the vertical modes. Based on the findings of this study, a linear elastic finite element model appears to be capable of capturing much of the complex dynamic behaviour of the bridge with very good accuracy, when compared to the low-level dynamic responses induced by ambient wind and traffic excitations.     

Coherent motions in windbreak flow

Experimental data on windbreak flows have been analysed, using several statistical methods. Our analysis demonstrates that coherent structures exist in the mixing region of a porous windbreak (50% porosity) flow, and are largely responsible for the momentum transport that re-accelerates the leeward flow. A comparison between windbreak flow and laboratory turbulent mixing layers suggests that the dominant structures in these two flows are similar. Some previous numerical and experimental results are interpreted in light of the coherent structures and the self-similar property in the mixing region of a windbreak flow.     

Complex unmixed spinels in layered intrusions within an obducted ophiolite in the Natal-Namaqua mobile belt

Spinellids showing unmixed intergrowths of chromite or chromian spinel (sensu stricto) and magnetite or chromian magnetite are not known in mafic or ultramafic igneous rocks. They do occur within metamorphosed rocks that attained temperatures sufficiently high (upper amphibolite facies) for the formation of homogeneous Al-Cr-Fe³⁺-Ti spinel phases with compositions not matched in slowly cooled igneous rocks. In the Tugela Rand intrusion complex intergrowths of chromian spinel, chromian magnetite, ulvöspinel, ilmenite and a transparent aluminous spinel are observed and interpreted in terms of the thermal history of the rocks. Compositional differences between the separate areas of chromian spinel and chromian magnetite in complex intergrowths exhibited by the metamorphosed Tugela Rand and Mambulu Complexes confirm the extension of the magnetite-hercynite solvus (Turnock and Eugster 1962) towards magnesium- and chromium-rich compositions. The Tugela Rand spinellids are compared with those from the Carr Boyd Complex (Purvis et al. 1972) and the ultramafic rocks of the Giant Nickel Mine (Muir and Naldrett 1973) and the Red Lodge district (Loferski and Lipin 1983). Significant differences between the spinels from the Red Lodge district compared to the other three occurrences may reflect the different metamorphic histories of these areas.