bluuebunny/crossref_metadata_2025_split huggingface dataset:
‘I was treated like dirt’: evaluating links between betrayal and mental contamination in clinical samples
Authors: Pagdin Rowena , Salkovskis Paul M. , Nathwani Falguni , Wilkinson-Tough Megan , Warnock-Parkes Emma 
Published: August 2020

AbstractBackground:Little is known about the impact of interpersonal betrayal experiences on mental health. Research suggests a link between betrayal and mental contamination (MC) within some forms of obsessive compulsive disorder (OCD). This study represents an initial exploration of that link in clinical samples.Aims:A measure for assessing perceptions of betrayal was developed and evaluated (Study 1) in order to assess the extent of specificity of any association between the impact of betrayal and MC, and to estimate the extent of the impact of betrayal across common psychological disorders (Study 2).Method:In Study 1, the Perception of Betrayal Scale (POBS) was completed by 217 community participants; an exploratory principal components analysis identified the dimensional structure of the POBS. Study 2 was based on a cross-sectional, between-groups design, with three clinical groups [OCD (n = 23), other anxiety disorders (n = 21) and depression (n = 18)] and a non-clinical control group (n = 21). Three clinical groups (OCD, other anxiety disorders, and depression) and a community group completed a selection of measures via questionnaire.Results:In Study 1, the POBS was found to have an internal consistency of α = .95, and four factors were identified: preoccupation with betrayal events, belief that betrayal had caused major life change, lack of trust due to betrayal and betrayal leading to traumatic responses. In Study 2, the OCD group scored more highly in terms of maladaptive perceptions of betrayal than the other groups. Regression analysis showed betrayal scores to be a moderate predictor of the experience of MC; the POBS subscales lack of trust due to betrayal and betrayal leading to traumatic responses were found to be significantly associated with MC. Although there was some overlap with bitterness, betrayal better predicted MC.Conclusion:Findings support the hypothesis of a specific relationship between the construct of betrayal and MC.
The Evolution of the Dispute Settlement Mechanism in Preferential Trade Agreements [PTAs]: The Case of Indonesia
Authors: WIDIATEDJA I Gusti Ngurah Parikesit 
Published: August 2020

AbstractThe dispute settlement mechanism [DSM] under preferential trade agreements [PTAs] is crucial to ensure adequate implementation and enforcement of commitments among contracting parties. The DSM has evolved from political/diplomatic styles with a low level of legalism to judicial styles with a high level of legalism. Indonesia has also experienced this evolution process in its PTAs. This paper aims to show the evolution of the DSM in Indonesian PTAs, analyzing several related factors behind this trend. The paper argues that the evolution of the DSM from the GATT to WTO, Indonesia's participation in regional trade agreement, that is, ASEAN, the influence of trade partners, the existence of domestic factors, and the ongoing WTO dispute encourage the evolution of the DSM in Indonesian PTAs from political styles to more judicial styles with a high level of legalism.
China's State-Centric Approach to Corporate Social Responsibility Overseas: A Case Study in Africa
Authors: Liu Bingyu 
Published: August 2020

AbstractCorporate social responsibility (CSR) is conventionally understood as voluntary and market- based corporate behaviour without direct government involvement. The development of CSR in China challenges this understanding in the light of the growing role of government in promoting it. Over the past decade China has demonstrated a state-centric approach towards promoting CSR. Existing studies focus only on Chinese domestic CSR practices. However, with the rise of Chinese companies in Africa under China's ‘Belt and Road Initiative’, it is important to examine how the state-centric approach applies to the overseas CSR practice of Chinese companies. This article aims to fill the literature gap through in-depth interviews and analysis of the Standard Gauge Railway project in Kenya. It shows that close institutional, relational, and bureaucratic ties between the state and the business community give the Chinese government the power to influence the behaviour of Chinese state-owned enterprises overseas. The Chinese government can influence the CSR practices of Chinese companies overseas through mandating, facilitating, endorsing and partnering in order to minimize the negative externalities of companies’ overseas activities. However, the state-centric CSR approach limits the space for civil society engagement and the effectiveness of the approach abroad is constrained by a variety of institutional contexts and corporate ownership models.
Mineral Nutrients Sourced in Deep Regolith Sustain Long‐Term Nutrition of Mountainous Temperate Forest Ecosystems
Authors: Uhlig D. , Amelung W. , von Blanckenburg F. 
Published: August 2020

AbstractPrimary productivity of forest ecosystems depends on the availability of plant‐essential mineral nutrients. Because nutrient demand of trees often exceeds nutrient supply from rock, tree nutrition is sustained by efficient reutilization of organic‐bound nutrients. These nutrients are continuously returned from trees to the forest floor in litterfall. However, over millennia nutrient limitation may develop in landscapes from which nutrients are permanently lost by drainage and erosion. Such a deficit is prevented if advection of unweathered bedrock toward the surface as driven by erosion continuously supplies fresh nutrients. Yet the mechanisms and the depth range over which this deep nutrient resource is accessed are poorly known. We show that in two montane temperate forest ecosystems in the Black Forest and Bavarian Forest the geogenic source of nutrients was found within a depth zone of several meters. This deep zone contains a large pool of biologically available nutrients. We applied isotope ratios as proxies for nutrient uptake depth, and we tracked the regolith depth at which the isotope ratios of 87Sr/86Sr and 10Be(meteoric)/9Be match the respective values in plant tissue. We mapped the depth distribution of the biologically available calcium‐bound form of the most plant‐essential mineral nutrient phosphorus and found that the depth of phosphorus availability is as deep or even deeper as the range defined by the isotope ratios. We conclude that nutrient supply from a regolith depth of several meters is critical for forest ecosystem function in landscapes of moderate hillslopes and rainfall that are affected by permanent nutrient loss.
Resolving the Kinematics and Moment Release of Early Afterslip Within the First Hours Following the 2016 Mw 7.1 Kumamoto Earthquake: Implications for the Shallow Slip Deficit and Frictional Behavior of Aseismic Creep
Authors: Milliner C. , Bürgmann R. , Inbal A. , Wang T. , Liang C. 
Published: August 2020

AbstractAs stresses following rupture are dissipated continuous measurements of postseismic surface deformation provide insight into variations of the frictional strength of faults and the rheology of the lower crust and upper mantle. Due to the difficulty of capturing the earliest phase of afterslip, most analyses have focused on understanding postseismic processes over timescales of weeks to years. Here we investigate the kinematics, moment release, and frictional properties of the earliest phase of afterslip within the first hours following the 2016 Mw 7.1 Kumamoto earthquake using a network of 5‐minute sampled continuous Global Positioning System (GPS) stations. Using independent component analysis to filter the GPS data, we find that (1) early afterslip contributes only ~1% of total moment release within the first hour and 8% after 24 hr. This suggests that the lack of a coseismic slip deficit, which we estimate using standard geodetic data sets (e.g., InSAR, GPS, and pixel offsets) and which span the first 4 days of the postseismic period, is largely reflective of the dynamic rupture process and we can rule out contamination of moment release by early afterslip. (2) Early afterslip shows no evidence of a delayed nucleation or acceleration phase, where instead fault patches transition to immediate deceleration following rupture that is consistent with frictional relaxation under steady state conditions with dependence only on the sliding velocity. (3) There is a close correlation between the near‐field aftershocks and afterslip within the first hours following rupture, suggesting afterslip may still be an important possible triggering mechanism during the earliest postseismic period.
Black Carbon Absorption Efficiency Under Preindustrial and Present‐Day Conditions Simulated by a Size‐ and Mixing‐State‐Resolved Global Aerosol Model
Authors: Matsui Hitoshi 
Published: August 2020

AbstractThe positive radiative forcing of black carbon (BC) aerosol depends not only on the spatial and temporal distribution of BC but also its absorption efficiency. The mass absorption cross section (MAC) of BC is enhanced by atmospheric aging processes that increase particle size and non‐BC coating amounts (mixing state) of BC‐containing particles. However, the representation of MAC (or absorption enhancement) in current global aerosol models has a large uncertainty. This study used a global aerosol model that resolves particle size and mixing state to show that the MAC of anthropogenic BC has increased by 50% from preindustrial to present‐day conditions (from 5.6 to 8.6 m2 g−1) because faster present‐day aging processes increase the fraction of thickly coated BC particles, which have high absorption efficiency. This effect is apparent only when the model considers BC mixing state with sufficient resolution. The impact of this MAC enhancement on BC direct radiative forcing is estimated to be 0.051–0.086 W m−2 globally (22–37% of anthropogenic BC direct radiative forcing, 0.23 W m−2) and exceeds 0.5 W m−2 near‐source regions in East Asia. Sensitivity simulations show that BC direct radiative forcing and MAC are highly sensitive to non‐BC emissions, secondary aerosol formation, and aerosol size distribution and mixing state in emissions. We must therefore improve our understanding of these factors by further observations and reduce their discrepancies between models to achieve better estimates of BC absorption efficiency and radiative forcing.
Iron Mobility During Diagenesis at Vera Rubin Ridge, Gale Crater, Mars
Authors: L'Haridon J. , Mangold N. , Fraeman A. A. , Johnson J. R. , Cousin A. , Rapin W. , David G. , Dehouck E. , Sun V. , Frydenvang J. , Gasnault O. , Gasda P. , Lanza N. , Forni O. , Meslin P.‐Y. , Schwenzer S. P. , Bridges J. , Horgan B. , House C. H. , Salvatore M. , Maurice S. , Wiens R. C. 
Published: August 2020

AbstractTheCuriosityrover investigated a topographic structure known as Vera Rubin ridge, associated with a hematite signature in orbital spectra. There,Curiosityencountered mudstones interpreted as lacustrine deposits, conformably overlying the 300 m‐thick underlying sedimentary rocks of the Murray formation at the base of Mount Sharp. While the presence of hematite (α‐Fe2O3) was confirmed in situ by both Mastcam and ChemCam spectral observations and by the CheMin instrument, neither ChemCam nor APXS observed any significant increase in FeOT(total iron oxide) abundances compared to the rest of the Murray formation. Instead,Curiositydiscovered dark‐toned diagenetic features displaying anomalously high FeOTabundances, commonly observed in association with light‐toned Ca‐sulfate veins but also as crystal pseudomorphs in the host rock. These iron‐rich diagenetic features are predominantly observed in “gray” outcrops on the upper part of the ridge, which lack the telltale ferric signature of other Vera Rubin ridge outcrops. Their composition is consistent with anhydrous Fe‐oxide, as the enrichment in iron is not associated with enrichment in any other elements, nor with detections of volatiles. The lack of ferric absorption features in the ChemCam reflectance spectra and the hexagonal crystalline structure associated with dark‐toned crystals points toward coarse “gray” hematite. In addition, the host rock adjacent to these features appears bleached and shows low‐FeOTcontent as well as depletion in Mn, indicating mobilization of these redox‐sensitive elements during diagenesis. Thus, groundwater fluid circulations could account for the remobilization of iron and recrystallization as crystalline hematite during diagenesis on Vera Rubin ridge.
Experiments on the Morphodynamics of Open Channel Confluences: Implications for the Accumulation of Contaminated Sediments
Authors: Yu Qingcheng , Yuan Saiyu , Rennie Colin D. 
Published: August 2020

AbstractContaminated sediments are common in river networks. The flow convergence and particular flow structures in confluences, such as the flow separation zone, may result in greater accumulation of contaminated sediments than in other river locations, but this issue is rarely studied. In addition, the contaminated sediment transport is driven by the particular morphodynamics occurring at confluences. This article describes a novel confluence flume experiment on both morphodynamics and deposition patterns of contaminated sediments as a function of geometric and flow conditions. The initial equilibrium bed geometry was developed from a mobile bed and then fixed, allowing for subsequent flow velocimetry and sediment feeding. Colored sediments of fine gradation, which mimic contaminated sediments, were then fed to the tributary channel. The results suggest that the junction angle primarily determines the confluence bed morphology and sediment transport pattern while the discharge ratio is a secondary factor. It was also observed that most introduced sediments tended to deposit immediately after the cessation of feeding at the stoss of the bar in the flow separation zone. The time history of the transport of the contaminated sediments was also investigated. Sediment that initially deposited at the stoss of the bar eventually moved to the lee of the bar and deposited around the bar downstream of the confluence, demonstrating that the sedimentation pattern evolved to a state similar to the equilibrium bed morphology.
Denuding a Craton: Thermochronology Record of Phanerozoic Unroofing From the Pilbara Craton, Australia
Authors: Morón Sara , Kohn Barry P. , Beucher Romain , Mackintosh Vhairi , Cawood Peter A. , Moresi Louis , Gallagher Stephen J. 
Published: August 2020

AbstractCratons are ancient regions of relatively stable continental fragments considered to have attained long‐term tectonic and geomorphic stability. Low‐temperature thermochronology data, however, suggest that some cratons have experienced discrete Phanerozoic heating and cooling episodes. We report apatite fission track, and apatite and zircon (U‐Th)/He low‐temperature thermochronology data from the Archean Pilbara craton and adjacent Paleoproterozoic basement, NW Australia. Inverse thermal history simulations of this spatially extensive data set reveal that the region has experienced ~50–70°C cooling, which is interpreted as a response to the unroofing of erodible strata overlying basement. The timing of cooling onset is variable, mainly ~420–350 Ma in the southern and central Pilbara‐eastern Hamersley Basin and ~350–300 Ma in the northern Pilbara, while the westernmost Pilbara‐central Hamersley Basin does not record a significant Paleozoic cooling event. These differences are attributed to variations in sedimentary thickness and proximity to adjacent rift basins, which lack Archean age zircons in their Paleozoic strata. The onset of Paleozoic cooling coincides with the timing of the episodic intraplate late Ordovician‐Carboniferous Alice Springs Orogeny. This orogeny is thought to have resulted from far‐field plate margin stresses, which in turn caused the opening of the adjacent Canning Basin, to the north and east of the craton. We propose that basin development triggered a change of base level, resulting in denudation and the crustal cooling event reported here. Our results provide further evidence for the transmission of far‐field forces to cratons over hundreds of kilometers and support the view that cratons have experienced geomorphic changes during the Phanerozoic.
Small‐Scale Capillary Heterogeneity Linked to Rapid Plume Migration During CO2 Storage
Authors: Jackson Samuel J. , Krevor Samuel 
Published: August 2020

AbstractUnpredicted, rapid plume elongation has been observed at subsurface CO2 storage projects worldwide, exemplified by the Sleipner project. We show that conventionally ignored centimeter‐meter scale heterogeneity in capillary pressure characteristics can manifest as rapid field‐scale, decameter‐kilometer, plume migration. We analyze the effect in the Goldeneye field, UK, a proposed storage site with a unique combination of sample/data accessibility and generality as an archetype sandstone reservoir. We overcome previous barriers by characterizing in greater detail over larger scales—the 65 m reservoir height at cm‐m resolution—and through use of an upscaling scheme which resolves small‐scale heterogeneity impacts in field‐scale simulations. These models reveal that significant early time retardation of buoyantly rising CO2 plumes is followed by rapid migration under the caprock in the presence of anisotropic, layered heterogeneities. Lateral migration speeds can be enhanced by 200%, placing first‐order controls on fluid flow and providing a mechanistic explanation for field observations.
Anomalous Behavior of the Equatorial Ionization Anomaly During the 2 July 2019 Solar Eclipse
Authors: Jonah O. F. , Goncharenko L. , Erickson P. J. , Zhang S. , Coster A. , Chau J. L. , de Paula E. R. , Rideout W. 
Published: August 2020

AbstractA solar eclipse is a spectacular phenomenon resulting from a Sun‐Moon alignment as viewed from the Earth. Eclipses have a great influence on the state of the ionosphere and trigger significant variations during this extraordinary event, as daytime sunlight turns to darkness and back again. Therefore, understanding how this dramatic solar‐lunar event affects the Earth's atmosphere is of enormous importance. In this study, we took advantage of the proximity of a 2 July 2019 solar eclipse to the equatorial ionization anomaly (EIA) in order to investigate EIA dynamics during the eclipse total obscuration as it made its first landfall over the South American continent. We found the following eclipse dynamic features (1) analogous to prior results at the EIA, a 57% enhancement of the total electron content (TEC) in the EIA crest during total obscuration in areas a few degrees to the north from totality; (2) a 35% TEC suppression along the path of totality to the south of the EIA (sub‐EIA) crest; (3) temporal and spatial extension of the southern EIA crest; (4) enhancement of the fountain effect and associated with it vertical plasma drift in the magnetic equatorial region; and (5) unusual observation of TEC bite‐out near the EIA crest prior to local eclipse onset.
Lithosphere Mantle Density of the North China Craton
Authors: Xia Bing , Thybo Hans , Artemieva Irina M. 
Published: August 2020

AbstractWe constrain the lithospheric mantle density of the North China Craton (NCC) at both in situ and standard temperature‐pressure (STP) conditions from gravity data. The lithosphere‐asthenosphere boundary (LAB) depth is constrained by our new thermal model, which is based on a new regional heat flow data set and a recent regional crustal model NCcrust. The new thermal model shows that the thermal lithosphere thickness is <120 km in most of the NCC, except for the northern and southern parts with the maximum depth of 170 km. The gravity calculations reveal a highly heterogeneous density structure of the lithospheric mantle with in situ and STP values of 3.22–3.29 and 3.32–3.40 g/cm3, respectively. Thick and reduced‐density cratonic‐type lithosphere is preserved mostly in the southern NCC. Most of the Eastern Block has a thin (90–140 km) and high‐density lithospheric mantle. Most of the Western Block has a high‐density lithospheric mantle and a thin (80–110 km) lithosphere typical of Phanerozoic regions, which suggests that the Archean lithosphere is no longer present there. We conclude that in almost the entire NCC the lithosphere has lost its cratonic characteristics by geodynamic processes that include, but are not limited to, the Paleozoic closure of the Paleo‐Asian Ocean in the north, the Mesozoic Yangtze Craton flat subduction in the south, the Mesozoic Pacific subduction in the east, the Cenozoic remote response to the Indian‐Eurasian collision in the west, and the Cenozoic extensional tectonics (possibly associated with the slab roll‐back) in the center.
High‐Frequency Submesoscale Motions Enhance the Upward Vertical Heat Transport in the Global Ocean
Authors: Su Zhan , Torres Hector , Klein Patrice , Thompson Andrew F. , Siegelman Lia , Wang Jinbo , Menemenlis Dimitris , Hill Christopher 
Published: August 2020

AbstractThe rate of ocean heat uptake depends on the mechanisms that transport heat between the surface and the ocean interior. A recent study found that the vertical heat transport driven by motions with scales smaller than 0.5° (submesoscales) and frequencies smaller than 1 day−1 is upward. This transport competes with the other major components of the global heat transport, namely, the downward heat transport explained by the large‐scale wind‐driven vertical circulation and vertical diffusion at small scales and the upward heat transport associated with mesoscale eddies (50‐ to 300‐km size). The contribution from motions with small spatial scales (<0.5°) and frequencies larger than 1 day−1, including internal gravity waves, has never been explicitly estimated. This study investigates this high‐frequency (subdaily) submesoscale contribution to the global heat transport. The major result of this study, based on the analysis of a high‐resolution ocean model, is that including this high‐frequency contribution surprisingly doubles the upward heat transport due to submesoscales in winter in the global ocean. This contribution typically concerns depths down to 200–500 m and can have a magnitude of up to 500 W m−2 in terms of wintertime heat fluxes at 40‐m depth, which causes a significant upward heat transport of ~7 PW when integrated over the global ocean. Thus, such submesoscale heat transport, which is not resolved by climate models, impacts the heat uptake in the global ocean. The mechanisms involved in these results still need to be understood, which should be the scope of future work.