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A recent review identified three key principles for good practice in urban humanitarian response; taking these on board may help all actors to avoid wasting effort and missing opportunities.

Previous studies have observed mineral specific variations in the ratios of IRSL signals stimulated at the different discrete wavelengths of lines corresponding to Xe lamp emission lines, which fall within the broad excitation spectrum of IRSL. Meanwhile recent accounts of IRSL have referred to single trapping systems within the excitation band, and modelled excitation spectra as continuous gaussian distributions. A simple single trap model should not result in variations in the ratio of IRSL intensities produced at different wavelengths. In the study reported here 22 different feldspar samples, which have all been characterised by SEM and x-ray analysis, were measured using a portable OSL instrument equipped with 890 nm and 940 nm diode arrays to confirm and extend the previous observations of variations in IRSL intensity ratios. Of the samples investigated the sensitivity varied over 3–4 orders of magnitude. Albite samples in this selection showed consistently high responses. The plagioclase samples show significant variations, and the microcline and K-feldspar samples produced a large range of responses. Excitation ratios of 940 nm–890 nm show mineralogically linked variations which together with the earlier Xe lamp data point to distributions of trapping systems within the variable environments of these minerals. These results do not readily fit simple single trap models for luminescence from feldspars; instead, they suggest multiple traps or a series of similar traps which are significantly perturbed by their local lattice structural environments. Post Stimulation Phosphorescence (PSP) was observed for all samples, and phototransferred thermoluminescence (PTTL) has also been confirmed following IR stimulation suggesting that recombination mechanisms involve charge mobility and interactions with shallow traps in band-tail states rather than primarily being associated with direct quantum tunnelling recombination. The relative proportions of PSP to prior IRSL also varied between the two stimulation wavelengths which further emphasises the physical differentiation between processes influencing different subpopulations of the trapping states associated with IRSL and their local lattice environments.

This paper presents the findings of a review of academic literature concerning the degree to which corruption worsens naturally-triggered disasters in the built environment. The research employed a 'systematic literature review' methodology to analyse leading academic databases, resulting in a detailed analysis of 59 peer-reviewed, published papers. It was found that while much of the literature focuses on earthquakes (relating to building and infrastructure collapse), the quality of governance and the drivers of corruption, there is presently limited scholarship concerning the general scope, reach and scale of how disasters are worsened by corruption. This article is protected by copyright. All rights reserved.

This paper presents a review of international peer-reviewed academic research into the question of how corruption in the construction industry can exacerbate the human impact of naturally-triggered disasters. A systematic review of peer-reviewed academic papers from the fields of corruption, construction and disaster management over the past thirty years reveals a dearth of empirical research in this area. Results indicate that existing research tends to focus on the quality of governance and the drivers of corruption and is fragmented, limited and narrow in scope. Despite these limitations, evidence is found to support the proposition that corruption in the construction industry can significantly worsen the economic, social and environmental impacts of naturally-triggered disasters. This appears to be especially the case where corruption, disaster, and poverty intersect. Acknowledging the methodological challenges of undertaking research in this area, it is concluded that more research is needed to test this proposition which intersects the related fields of corruption, natural disasters and the construction industry.

River confluences can be meta-stable and contain valuable geological records of catchment response to decadal-millennial scale environmental change. However, in alluvial reaches flood stratigraphies are particularly hard to date \ud using 14C. In this paper we use a novel combination of optically stimulated luminescence (OSL) and multi proxy sedimentological analyses to provide a flood record for the Severn-Teme confluence over the last two millennia which we compare with independent European climate records. The results show that by c.2000 BP the Severn-Teme confluence had stabilized and overbank alluviation had commenced. Initially this occurred from moderately high flood magnitudes between c.2000-1800 BP (50 BCE-CE 150), but was followed from 1800-1600 BP (CE 150-350) by fine alluvial deposition and decreased flood intensity. From 1600-1400 BP (CE 350-550) the accumulation rate increased with evidence of large flood events associated with the climatic deterioration of the Dark Age Cold Period. \ud Following a period of reduced flood activity after c.1400 BP (c. CE 550) larger flood events and increase in accumulation rate once again became more prevalent from c.850 BP (c. CE 1100) coincident with the start of the Medieval Climate Anomaly, a period associated with warmer, wetter conditions and increased land-use intensity. This state persisted until c.450 BP (c. CE 1500) after which increased flood magnitudes can be associated with climatic variations during the Little Ice Age. We demonstrate that from the combination of high-resolution dating techniques and multiple analytical parameters, distinctive phases of relative flood magnitude vs flood duration can be determined to a \ud detailed chronological precision beyond that possible from 14C dating. This permits the identification of the regional factors behind floodplain sedimentation, which we correlate with the intensification of land-use and climatic drivers over the last two millennia.

Purpose\ud \ud The purpose of this paper is to investigate the relationship between occupiers’ satisfaction with the property management service they receive and the financial performance of commercial real estate.\ud \ud Design/methodology/approach\ud \ud The study uses occupier satisfaction data for 240 UK commercial properties collected over a 12-year period and the annual total returns achieved by those properties. Various statistical techniques are employed to assess whether increasing occupier satisfaction leads to greater returns for investors. These include comparing excess returns and risk-adjusted returns with occupier satisfaction at each property to assess whether superior property management generates outperformance (“positive alpha”). The study also investigates whether the relationship between occupier satisfaction and returns is the same across all sectors and whether it is affected by market conditions.\ud \ud Findings\ud \ud A positive correspondence is found between benchmark outperformance and occupier satisfaction. The relationship is similar for all sectors of commercial property and is particularly strong during the Global Financial Crisis, indicating that paying attention to satisfying the needs of occupiers has particular benefits during periods when the supply of commercial real estate exceeds demand.\ud \ud Research limitations/implications\ud \ud The sample of properties was restricted to those for which occupier satisfaction data had been collected by RealService Ltd and whose owners permitted access to the financial performance results. This meant that the properties belong to only three landlords, all UK REITs that care sufficiently about occupier satisfaction to commission studies. Thus the findings might not apply to all commercial properties. The mechanism by which the positive relationship between satisfaction and financial performance occurs is not tested, but the conventional mechanisms of reputation and customer loyalty (the “service-profit chain”) are discussed.\ud \ud Practical implications\ud \ud The findings suggest that it is worthwhile for landlords, or property managers acting on their behalf, to understand the needs of their occupiers in order to deliver the level of service that those occupiers desire. Leases in the UK are generally “triple net” and the total returns used for this analysis are net of property management costs, so the positive relationship between satisfaction and performance is not the result of economising on service delivery. A further implication is that valuers should take more account of occupier satisfaction when assessing the capital value of a property, from which total returns are assessed.\ud \ud Originality/value\ud \ud Demonstrating the links between customer service, customer satisfaction and business profitability is rarely attempted because of the many confounding factors that affect profitability. UK listed real estate companies are typically reluctant to reveal the financial performance of individual properties, and information about occupiers’ satisfaction is not generally available. The authors were fortunate to be granted access to a time series of such data, and to be able to demonstrate that attention to delivering a property management service that satisfies occupiers is likely to bring financial rewards to the owners of the property.

On March 11 2011 the north-eastern region of Japan was hit by a magnitude 9 earthquake, which occurred underneath the sea-bed 70 km east of the Oshika peninsula in Tohoku. The north-eastern shore of Honshu was hit by a tsunami resulting from this earthquake. As a consequence, reactors 1-4 at the nuclear power station Fukushima-Daiichi suffered a completed loss of power and cooling causing a partial core meltdown in units 1, 2 and 3 followed by a series of explosions and the release of large quantities of radioactivity into the environment. The accident was rated level 7 (the highest level) on the International Nuclear Event Scale. While most of the emissions were driven towards the Pacific Ocean, a significant amount of radioactive material was deposited onto the Japanese land-mass, resulting in enhanced localised radiation exposure.\ud \ud \ud This report covers measurements and detailed radiation maps conducted by a UK University team working with Japanese colleagues during a series of visits in 2012. They have been presented and shared locally in Japan at time of acquisition. Since then the data have been cross-validated relative to soil samples from a reference site established at the University of Fukushima, and analysed independently in the UK and in Japan. This report provides detailed descriptions of the data sets, validated radiometric maps for 134Cs, 137Cs and the overall gamma dose rates, together with a full account of the establishment of the calibration site. The work reported here demonstrates the utility of detailed radiometric maps in helping to understand the distribution of radionuclides in complex environmental systems. This information is potentially of use to help avoid unnecessary external radiation exposure in the outdoor environment, to help to visualise and target areas for remediation, to evaluate the effectiveness of clean-up and soil removal activities, to examine uptake of radioactivity from the environment through agricultural systems, and to monitor redistribution over time of the activity in the environment. The report includes full copies of digital data sets for the demonstration surveys.\ud \ud \ud Radiometric methods provide means of measuring radioactivity with recognised roles in nuclear emergency response, and environmental applications. In the aftermath of nuclear accidents they are crucial to evaluate the environmental impact of the accident and guide remediation measures. The Scottish Universities Environmental Research Centre (SUERC) is a research centre attached to the University of Glasgow with extensive experience of radiometric mapping using airborne and ground based systems, conducting most of the UK post-Chernobyl radiation mapping using airborne systems and coordinating European projects to harmonise and cross-calibrate systems for nuclear emergency response purposes. In the early stages of major accidents the most pressing needs are for rapid, large scale, information. Airborne surveys of the affected area were conducted initially by a joint US/Japanese team and later on by The Ministry of Education Science and Technology (MEXT) and the Japanese Atomic Energy Agency (JAEA), eventually providing national scale radiation maps with a spatial resolution of several hundred meters. In later stages of accident recovery there are increasing needs for more detailed spatial information and increasing requirements for objective, traceable and cross validated analysis. Systems for this work need to be mobile, preferably portable, efficient, robust and well calibrated, providing detailed real time information directly on location. The SUERC Portable Gamma Spectrometry system fulfils these criteria. It provides a spatial resolution of better than 10 m for mapped data and allows a real time identification of spatial features down to 10-20 cm.\ud \ud \ud In the work reported here, calibration sites have been established in Fukushima at the campus of Fukushima University and the Fukushima Prefecture Fruit Tree Research Institute to provide objective and internationally traceable validation of ground based instruments. High resolution HPGe spectrometry of soil samples conducted at laboratories at Fukushima University and SUERC was used for validation of the field instrument. Values of 137Cs activity concentration measured by the two laboratories were in full agreement to high precision. Agreement for the 134Cs activity concentration values was within 5-10%. The soil samples used in this process were analysed as a function of depth, revealing that while the majority of activity was retained in near surface layers, a small component of approximately 1% of the total activity appears to have migrated more rapidly to greater depths. This suggests complex transport behaviour in the soil columns which should be investigated further. The calibration sites are open for future use. These data establish a traceable record between local facilities and internationally acknowledged standards for future use. \ud \ud \ud Deployment of the SUERC system in vehicles has demonstrated the ability of relatively small detectors to measure regional scale deposition patterns over a wide range of radioactivity levels, varying from 10,000 Bq per square meter up to more than 10 million Bq per square meter. These activity levels are broadly consistent with the national scale airborne maps for the study areas, but the ground based maps provide very high level of local detail, which allow small scale changes to be readily observed and related to the local soils, land cover and built environment. Areas covered in two surveys in March and July 2012, respectively, cover parts of the Fukushima Prefecture including parts of the evacuation and exclusion zones as well as areas directly affected by the 2011 tsunami. Short backpack surveys in urban areas associated with the car trips were also conducted e.g. in Fukushima City (in the heart of the prefecture), Ōkuma (within 3 km of the Fukushima Daichi reactors), Minami-Daira and Kawauchi-mura (within the initial evacuation zones), demonstrate the versatility of a system which can be rapidly moved from a vehicle to backpack where further detailed information is needed.\ud \ud \ud With a fully spectrometric system as used in this study, it is possible to identify specific radioactive isotopes and to quantify the activity concentrations of natural and artificial sources spanning many orders of magnitude, from less than 10 kBq m-2 to above 10 MBq m-2 for radiocaesium. This information has been used to estimate the contribution to the dose rate from different sources, so that a comparison between the contributions from naturally occurring radioactive materials (not affected by the accident) and the different radiocaesium isotopes present following the accident can be readily made. These data provide vital information to the local population and emergency services in guiding remediation efforts, and also over the course of time, in observing the extent to which weathering and radioactivity decay processed are gradually reducing the relative contributions from the accident. In the long term it is hoped that this type of representation will help put the accident contributions into perspective, and to register improvements with time which may help to establish increased confidence in affected areas. \ud \ud \ud In urbanised areas backpack systems provide the means of producing detailed surveys in locations where people spend their time. Surveys conducted of Fukushima University and Fukushima Iizaka have demonstrated the ability of detailed radiometric mapping to identify locations with highly varying levels of contamination, from more highly contaminated areas around drain pipes to the relatively low levels of contamination on roads and other hard surfaces where rain and snow melt have removed deposited activity. The effectiveness of the remediation work conducted on the University campus was evident, showing the ability of radiometric surveys to demonstrate the effectiveness of remediation and to identify where remaining activity is located. The remediation methods employed resulted in a three- to fourfold reduction in dose rate compared to untreated areas.\ud \ud \ud Remediation efforts in orchards or woodland are particularly challenging. Given the economic importance of agriculture in the Fukushima area and the possible pathways from contaminated produce into the human body, a precise evaluation of the local radiation risk is of prime importance. The SUERC system has been demonstrated in orchards at the Fukushima Prefecture Fruit Tree Research Institute, and at other orchards in the Prefecture. Work has also been undertaken with agricultural research institutions at Tsukuba, Ibaraki Prefecture. The comparison of measurements taken at these same sites over the time of a year show a decrease in activity following the half-life of the radioisotopes deposited, superimposed by environmental factors like precipitation, illustrating self-remediation. Ongoing work on these sites will allow an assessment of transfer of activity from to the fruit, and the impact of measures to remediate the orchards or reduce uptake of activity in the fruit, and the evaluation of external doses to workers in the orchards.\ud \ud \ud The data collected during this work contain the specific activity per isotope at a given surveyed location and at a given moment in time. The data accompanying this report are transparent, open and independently validated. They are made available for reference purposes and further utilisation.\ud \ud \ud The work presented here highlights many of the difficult challenges ahead in the monitoring and remediation effort in the area affected by the accident in the Fukushima Dai-ichi nuclear power plant. It demonstrates the capabilities and methods at the disposal of the international community in aiding the Japanese efforts, demonstrating the value of international collaboration in helping to address some of the difficult problems associated with recovery from a serious nuclear accident. It is hoped that these data, and the methods which they demonstrate, will contribute, together with future work, to increased understanding of the environmental impacts of the accident, and that future cooperative work involving Japanese and international teams will contribute to recovery and restoration of confidence in affected areas and communities.

This chapter reports a pilot study by two luminescence laboratories on samples from the 2004 excavations of Karabai I. The Scottish Universities Environmental Research Centre (SUERC) examined the optical stimulated luminescent (OSL) properties of the sediments using a method called luminescence profiling (Burbidge et al. 2007); the Max-Planck-Institute for Evolutionary Anthropology, Leipzig attempted to analyse the thermoluminescence (TL) age of a small collection of heated stones. Luminescence profiling is a rapid survey method for assessing the suitability of sediments for full dating based on the presence of particular minerals, grain-sizes and luminescence signals. At Karabai I the study revealed many factors that would complicate a subsequent full dating study, however a tentative age range of 60-115 ka was obtained using the ‘IRSL’ and ‘post IR & OSL TL’ signal from the polymineral coarse fraction. Luminescence signals based on quartz were found to be saturating and so could provide only minimum ages. Only one heated rock of sufficient mass, recovered in square 4H archaeological layer 2, exhibited acceptable properties for successful dating. The resulting TL age, 142 ± 23 ka (EVA-LUM-06/01), places Karabai I within MIS 6. This contrasts with the luminescence profile study that suggested sedimentary deposition within MIS 4-5. In both studies it is important to recognise the tentative nature of these conclusions.