Assessment of sedimentation processes determined from side-scan sonar surveys in the Buffalo River, New York, USA

An assessment of sedimentation processes was made using side-scan sonar records collected over a 15-year period in the Buffalo River, New York, USA. Spatial and temporal changes in natural and man-made bedforms documented sediment erosion, slumping, and sediment depositional sites. Bedforms and sediment texture were used to divide the mapped portion of the river (9 km) into four sedimentary environments, with Section 1 at the upper end and Section 4 near the mouth where the river discharges into the east end of Lake Erie. Based on annual changes in side-scan sonar records, depositional rates decrease in the downriver direction. Section 2, located 5 km from the river’s mouth, contains sedimentary furrows. The persistence of furrows in this portion of the river requires both sediment erosion and deposition under a bidirectional flow regime. Results from this study confirmed that side-scan sonar is a valuable tool in understanding sediment dynamics and can be useful in river restoration decision making.     

On the edge: changing geographies of the global city precariat in London and Hong Kong

Global cities are marked by precarity, yet little attention has been paid to the spatial overlap between work precarity among migrants and third sector organizations that sustain them. In this paper, we estimate the location of precarious work migrants in two global cities, London and Hong Kong, for both the 2001 and 2011 censuses, using a variety of spatial demographic and quantitative techniques, and then analyze the spatial overlap between this population and immigrant-serving third sector organizations. The results suggest both similarity, in particular between accommodation and work precarity, and difference, with an increasingly tenuous overlap in London by 2011.     

Are Australia’s suburbs swamped by Asians and Muslims? Countering political claims with data

Recent decades have seen substantial growth across many developed-world countries of right-wing populist political parties whose policies oppose immigration and multiculturalism as threats to the majority way of life there. These are exemplified in Australia by Pauline Hanson’s One Nation Party, which was successful at elections there at the turn of the twenty-first century and again in 2016. Part of this party’s rhetoric focuses on the geography of immigrant groups in Australia’s cities, with claims that their members live in ghettos. Is that factually correct? Using data from the 2011 Australian census this paper analyses the distribution of Asians and Muslims (the two groups picked out by One Nation and its leader) at four spatial scales within the country’s 11 largest urban areas. It finds no evidence at all of intensive residential segregation of Muslims, and although there are concentrations of Asians—notably in Sydney and Melbourne—most residents claiming Asian ancestry live in neighbourhoods and suburbs where they form a minority (in many cases a small minority) only of the local population.     

The scale of segregation: ancestral groups in Sydney, 2011

Most studies of urban residential segregation analyse it at a single-scale only, usually the smallest for which relevant census data are available. Following a recent argument that such segregation is multiscalar, this paper reports on multilevel modelling of the segregation of 42 ancestral groups in Sydney, Australia, looking at its intensity at four separate scales in which segregation at each scale is presented nett of its intensity at all higher-level scales. Most groups are more segregated at the macro- and micro-scales than at two intermediate meso-scales, with variations across them reflecting their size, recency of arrival in Australia and cultural differences from the host society. The findings are used as the basis for developing a multiscale appreciation of residential patterning.     

Marine evidence for the last glacial advance across eastern Hudson Strait,eastern Canadian Arctic

Data from accelerator mass spectrometer radiocarbon dated sediment cores and Huntec high-resolution seismic profiles were used to investigate the age and origin of the sediments in the Eastern Basin of Hudson Strait. The data indicate that the ice-contact and glacial-marine sediments on the basin flanks and much of the upper sequence in the deep floor of the basin were produced during the Noble Inlet advance (8.9 to 8.4 ka), the last northward expansion of the Labrador Dome on to southeastern Baffin Island. On the northern flank of Eastern Basin one sequence of ice-contact sediments and glacial-marine deposits overlies bedrock; the glacial-marine sediments are transitional upslope to ice-contact sediments, and form at least two successive ice-sheet grounding zones. The earliest abundance peaks of benthic Foramininfera in glacial-marine sediments date ca. 8.6 and 8.4 ka, and correlate to sediments near the base of the 58-m-thick glacial-marine section in the deepest part of Eastern Basin. This correlation suggests that Noble Inlet ice was grounded throughout Eastern Basin during the early part of its advance. In later stages the thinning ice produced grounding zones on the basin flanks while glacial-marine sediments were deposited in the deep basin. © 1998 John Wiley & Sons, Ltd.     

An estimate of the time taken for a dyke to cool through its curie point

Summary A brief argument is put forward to support the suggestion that dykes such as the members of the Pilandsberg and Tholeiite systems acquire their remanent magnetism in a period of the order of 1 to 10 years. This means that such dykes will cool from, say 550°C to 450°C in that time period.     

Holocene climate and glacial history of the northeastern Antarctic Peninsula: the marine sedimentary record from a long SHALDRIL core

A high-resolution record of Holocene deglacial and climate history was obtained from a 77 m sediment core from the Firth of Tay, Antarctic Peninsula, as part of the SHALDRIL initiative. This study provides a detailed sedimentological record of Holocene paleoclimate and glacial advance and retreat from the eastern side of the peninsula. A robust chronostratigraphy was derived from thirty-three radiocarbon dates on carbonate material. This chronostratigraphic framework was used to establish the timing of glacial and climate events derived from multiple proxies including: magnetic susceptibility, electric resistivity, porosity, ice-rafted debris content, organic carbon content, nitrogen content, biogenic silica content, and diatom and foraminiferal assemblages. The core bottomed-out in a stiff diamicton interpreted as till. Gravelly and sandy mud above the till is interpreted as proximal glaciomarine sediment that represents decoupling of the glacier from the seafloor circa 9400 cal. yr BP and its subsequent landward retreat. This was approximately 5000 yr later than in the Bransfield Basin and South Shetland Islands, on the western side of the peninsula. The Firth of Tay core site remained in a proximal glaciomarine setting until 8300 cal. yr BP, at which time significant glacial retreat took place. Deposition of diatomaceous glaciomarine sediments after 8300 cal. yr BP indicates that an ice shelf has not existed in the area since this time.The onset of seasonally open marine conditions between 7800 and 6000 cal. yr BP followed the deglacial period and is interpreted as the mid-Holocene Climatic Optimum. Open marine conditions lasted until present, with a minor cooling having occurred between 6000 and 4500 cal. yr BP and a period of minor glacial retreat and/or decreased sea ice coverage between 4500 and 3500 cal. yr BP. Finally, climatic cooling and variable sea ice cover occurred from 3500 cal. yr BP to near present and it is interpreted as being part of the Neoglacial. The onset of the Neoglacial appears to have occurred earlier in the Firth of Tay than on the western side of the Antarctic Peninsula. The Medieval Warm Period and Little Ice Age were not pronounced in the Firth of Tay. The breadth and synchroneity of the rapid regional warming and glacial retreat observed in the Antarctic Peninsula during the last century appear to be unprecedented during the Holocene epoch.     

Efficient drilling in horizontal directional drilling by implementing the concept of specific energy

The oil and gas industry has successfully used the concept of specific energy (SE) to maximise drill rate and identify inefficient conditions in drilling operations. This paper proposes the idea of implementing the concept of SE in horizontal directional drilling (HDD), a pipeline installation technique which was adopted from horizontal oil well drilling technology. The similarity of the HDD technique with oil well drilling makes SE surveillance a very useful tool in HDD operations. SE monitoring during the drilling stage of HDD can address drilling dysfunctions and maximise the rate of penetration. SE can be calculated in real-time and displayed to the rig personnel during the operation. This paper discusses the concept of SE and how it can be used in HDD projects, and it also illustrates an example application of SE in a case study.     

Creating Carbon Offsets in Agriculture through No-Till Cultivation: A Meta-Analysis of Costs and Carbon Benefits

Carbon terrestrial sinks are often seen as a low-cost alternative to fuel switching and reduced fossil fuel use for lowering atmospheric CO₂. To determine whether this is true for agriculture, one meta-regression analysis (52 studies, 536 observations) examines the costs of switching from conventional tillage to no-till, while another (51 studies, 374 observations) compares carbon accumulation under the two practices. Costs per ton of carbon uptake are determined by combining the two results. The viability of agricultural carbon sinks is found to vary by region and crop, with no-till representing a low-cost option in some regions (costs of less than $10 per tC), but a high-cost option in others (costs of 100–$400 per tC). A particularly important finding is that no-till cultivation may store no carbon at all if measurements are taken at sufficient depth. In some circumstances no-till cultivation may yield a triple dividend of carbon storage, increased returns and reduced soil erosion, but in many others creating carbon offset credits in agricultural soils is not cost effective because reduced tillage practices store little or no carbon.