Search

When institutional frictions threaten to disrupt collaborations, an external authority can be brought in to resolve disputes. How effective is such external imposition? What are the institutional circumstances in which it works? Framed by the collaborative governance regime (CGR), which sees established procedures and institutions as a critical collaborative capacity, this research employs a unique concept—collaborative friction—to explore the role of external imposition in collaboration among entities with significant institutional differences. We examined 965 recorded collaborative frictions from four large collaborative infrastructure projects between governments in Hong Kong and mainland China. Our finding suggests a significant, but limited, effect of the central government's imposition on collaborative frictions. We also find a significant role of sociopolitical circumstances in collaboration. Based on the findings, we make several theoretical propositions articulating external imposition's role in collaboration. [ABSTRACT FROM AUTHOR]

Aim: Methane oxidation driven by soil aerobic methanotrophs exhibits the largest methane sink capacity in forest ecosystems and plays important roles in the alleviation of global warming. Many studies have revealed the distribution of methanotrophs in forest ecosystems at field scales; however, the biogeographical patterns of methanotrophic communities and related ecological processes and the drivers shaping methanotrophic communities at a large scale remain poorly understood. Location: China's forests. Time period: 2012–2013. Major taxa studied: Methanotrophic communities. Methods: We evaluated the geographical distributions of soil methanotrophic communities across 26 forests along a 4,000‐km north–south transect in China using a MiSeq high‐throughput sequencing technique. The assembly processes and drivers of the methanotrophic communities were evaluated using the phylogenetic null model approach and structural equation modelling, respectively. Results: The results showed that the upland soil cluster α (USCα) and ammonia‐ oxidizing bacteria‐related (AOB‐rel) methanotrophs were the most abundant taxa in forest soils and exhibited contrasting distributions of relative abundance across different climate zones, suggesting that they occupy different environmental niches. The α‐diversity pattern of the soil methanotrophic community followed a hump‐shaped pattern along a large latitudinal gradient. Statistical analyses suggest that aridity and vegetation productivity [here represented with the normalized difference vegetation index (NDVI)] are major drivers of the α‐diversity of the methanotrophic community, whereas soil pH is the key environmental factor shaping the β‐diversity of the methanotrophic community at a large scale. Additionally, the community assembly of the methanotrophs primarily resulted from deterministic processes, among which heterogeneous selection had a greater contribution in shaping the methanotrophic community than homogeneous selection. Main conclusions: Our study provides new insights into the biogeographical distributions, assembly processes and ecological predictors of the methanotrophic community in forest soil at a large scale. These results can be used to improve simulation models for the better prediction of ecosystem functions under predicted global changes. [ABSTRACT FROM AUTHOR]

Aim: Many studies have found that diazotrophic distribution is mainly determined by soil properties from field to regional scales. However, we lack strong evidence for the relative importance of different drivers controlling broad‐scale biogeography of forest diazotrophs, especially for soil multi‐nutrients. Location: China's forests. Time period: 2012−2013. Major taxa studied: Diazotrophic communities. Methods: We investigated the distribution of soil diazotrophic communities from 146 sites along a 3,900‐km south–north transect by sequencing N‐fixing nifH gene amplicons. The relative contributions of environmental variables were assessed using a combination of stepwise multiple regression, variation partitioning analysis, multiple regression on distance matrices and partial least squares path modelling. Results: Overall, aridity index and temperature were the predominant parameters governing diazotrophic community diversity and structure, mainly through their indirect effects on soil pH, nutrient contents and plant productivity. Although soil multi‐nutrients (Ca, Mg, Fe, Mn, Na, Cu and Zn) were included in the statistical analysis, they still exhibited lower impacts on diazotrophic communities than climate. Intriguingly, the microelement Mo could not explain the diazotrophic community patterns, despite its significance in nitrogenase enzymes. This unexpected phenomenon was attributed to the relatively high Mo supply in our work. Moreover, the distinct responses of diazotroph taxa to climatic factors and large heterogeneity of diazotrophic diversity among forests in different climatic zones further support the dominant role of climatic variation. These results indicate the presence of differentiated climatic niches for diazotrophs, such as warm‐adapted Bradyrhizobium and cool‐adapted Azospirillum. Main conclusions: Our findings suggest for the first time that unlike prior studies, the key roles of soil nutrient limitation (even for Mo) and pH‐dependent mechanisms in small‐scale diazotrophic communities can be surpassed by large‐scale climatic gradients. Future changes in drought severity and temperature might greatly shape diazotrophic distribution and its potential function in forest N2 fixation. [ABSTRACT FROM AUTHOR]

Pro‐environmental leadership behaviours have been examined as the result of institutional forces, though anecdotes suggest the significant role of individual leaders. Little is known about this role in environmental policy implementation, and few empirical studies explore pro‐environmental leadership behaviours in the public sector. In this study, we empirically test a typology of pro‐environmental leadership behaviours and examine administrative leaders' motives for engaging in pro‐environmental behaviours. We then establish the relevance of our findings in environmental policy implementation. We empirically confirm the construct validity of pro‐environmental leadership behaviours that require leaders should articulate a policy vision, change followers' perception, and take symbolic actions. Our findings show that leaders' environmental efforts are largely prompted by legal compliance and motivated by instrumental self‐interest (e.g. increased economic opportunities), and normative values of engaging with broad sustainability issues may also have limited but potentially long‐lasting effects. Moreover, the evidence also suggests the importance of a workplace environment conducive to pro‐environmental leadership behaviours. These findings can be used to develop local strategies that stress policy implementation capacity building to induce pro‐environmental leadership behaviours in China. [ABSTRACT FROM AUTHOR]

Background: This study's initial results revealed significant decreases in treatment‐related esophagitis and pneumonitis cases in patients with thoracic esophageal squamous cell carcinoma (ESCC) treated with involved‐field irradiation (IFI), compared to elective nodal irradiation (ENI). This report outlines the long‐term trial results, specifically; overall survival (OS), progression‐free survival (PFS), metastasis‐free survival (MFS), and locoregional progression‐free survival (LRFS). Materials and Methods: Stage II–III thoracic ESCC patients were assigned randomly, in a 1:1 ratio, into either the ENI or IFI arm. Radiation therapy was delivered once a day in 1.8‐2.0 Gy fractions to a total dose of 60.0‐66.0 Gy to the gross tumor volume and 50.0‐54.0 Gy to the clinical target volume. The primary endpoints were acute treatment‐related esophagitis and pneumonitis. The results for the primary endpoints were previously published in 2018. In this article, we analyzed the secondary endpoints including PFS, LRFS, MFS, and OS. Results: Between April 2012 and October 2016, 228 patients from nine participating centers in China were enrolled into this study and randomly assigned to two treatment groups. For ENI and IFI groups, respectively, the results showed similarity and were as follows: median PFS (20.3 months vs 21.4 months), OS (32.5 months vs 34.9 months), MFS (28.2 months vs 26.0 months), and LRFS (25.0 months vs 26.6 months). In particular, respective OS rates in the ENI and IFI groups were 84.6% and 82.5% after 1 year, 45.1% and 48.7% after 3 years, and 29.8% and 30.7% at 5 years. PFS rates after 1, 3, and 5 years were 58.9%, 34.2%, and 26.9%, respectively, in the ENI arm compared to 64.4%, 30.8%, and 27.7%, respectively, in the IFI arm. Multivariate analysis identified clinical stage and tumor responses as independent predictors of OS. Meanwhile, tumor location, cStage, and tumor response were identified as independent factors influencing PFS. Conclusion: IFI was associated with similar survival as ENI in patients with thoracic ESCC, suggesting that IFI is an acceptable treatment method for thoracic ESCC. [ABSTRACT FROM AUTHOR]

Gravity‐drainage‐assisted steam flooding is a new technology to improve the recovery factor after deep penetration in deep super‐heavy oil reservoirs. This study is based on a model of the 60‐H25 test well group in Block 59 in Liaohe Oilfield, China. The numerical model uses the C programming language to analyze the influence of change in the bottom water height on the drainage effect and provides a theoretical basis for physical model experiments and field production. The physical model experiment uses similar principles to describe the production characteristics at different stages in a short cycle. We combine the numerical model and the physical model experiment to analyze the production rule of the Wa59 block over a long time period. The results show that the physical model experiment and the actual production of the block reflect the productivity change law of the well group, the degree of production, and the productivity relationship of the well group over short cycles and long periods, respectively. The comparison showed that the actual production was consistent with the production model of the physical model test, and the drainage effect was verified. The study of gravity‐drainage‐assisted steam flooding provides a reliable basis for the next stage of oilfield production. [ABSTRACT FROM AUTHOR]

Abstract: The Lanping Basin in the Nujiang‐Lancangjiang‐Jinshajiang (the Sanjiang) area of northeastern margin of the Tibetan Plateau is an important part of eastern Tethyan metallogenic domain. This basin hosts a number of large unique sediment‐hosted Pb‐Zn polymetallic deposits or ore districts, such as the Baiyangping ore concentration area which is one of the representative ore district. The Baiyangping ore concentration area can be divided into the east and west ore belts, which were formed in a folded tectogene of the India‐Asia continental collisional setting and was controlled by a large reverse fault. Field observations reveal that the Mesozoic and Cenozoic sedimentary strata were outcropped in the mining area, and that the orebodies are obviously controlled by faults and hosted in sandstone and carbonate rocks. However, the ore‐forming elements in the east ore belt are mainly Pb‐Zn‐Sr‐Ag, while Pb‐Zn‐Ag‐Cu‐Co elements are dominant in the west ore belt. Comparative analysis of the C‐O‐Sr‐S‐Pb isotopic compositions suggest that both ore belts had a homogeneous carbon source, and the carbon in hydrothermal calcite is derived from the dissolution of carbonate rock strata; the ore‐forming fluids were originated from formation water and precipitate water, which belonged to basin brine fluid system; sulfur was from organic thermal chemical sulfate reduction and biological sulfate reduction; the metal mineralization material was from sedimentary strata and basement, but the difference of the material source of the basement and the strata and the superimposed mineralization of the west ore belt resulted in the difference of metallogenic elements between the eastern and western metallogenic belts. The Pb‐Zn mineralization age of both ore belts was contemporary and formed in the same metallogenetic event. Both thrust formed at the same time and occurred at the Early Oligocene, which is consistent with the age constrained by field geological relationship. [ABSTRACT FROM AUTHOR]

The Sepikou region is located in the eastern Bogda Mountains of the east Tianshan. The Bogda belt is mainly composed of Carboniferous strata, including the Lower Carboniferous Qijiaojing Formation (C1q), Upper Carboniferous Liushugou Formation (C2l), and Qijiagou Formation (C2qj). Here, we report the petrology, geochemistry, and geochronology of bimodal volcanic rocks from the Upper Carboniferous Liushugou Formation, which is widely distributed in the Sepikou region. The basalts, basaltic andesite, and keratophyre have similar petrochemical characteristics and exhibit the high‐Na, low‐K characteristics belonging to calc‐alkalic rocks. These are characterized by the high abundance of K, Rb, Th, Ba, the depletion of HFSE (Nb, Ta, Zr, and Hf), and the slight depletion of Ti. Chondrite‐normalized rare‐earth elements (REE) patterns for basalts‐keratophyre show right‐leaning parallel curve clusters, together with a slight enrichment in light rare‐earth elements (LREE) contents and low heavy rare‐earth elements (HREE)/LREE ratios. The keratophyre exhibits slightly negative Eu anomalies. Compared with the basalts, the rhyolites have high alkali contents, slightly high ∑REE contents, low heavy rare‐earth elements/LREE ratios, negative εSr(t) (−9.1 to −12.0), low 87Sr/86Sr initial ratio, highly positive εNd (t) (+5.3 to +6.4), and low Pb isotope ratios. The fractionated REE patterns with prominent negative Eu anomalies suggest they were chiefly derived from the mantle magma underplated basaltic body remelting from the depleted mantle source. The LA‐ICP‐MS analysis on zircons from quartz keratophyre and rhyolite yield similar ages of 314.9 ± 1.2 and 314.0 ± 1.1 Ma, respectively, suggest that the major bimodal volcanism took place in the Late Carboniferous epoch. The quartz keratophyre zircons, with the 176Hf/177Hf ratios of 0.282897–0.283097, have highly positive εHf (10.99–19.97) and depleted mantle model ages between 180 and 628 Ma. The mafic rocks were chiefly derived from the depleted mantle with the partial incorporation of crustal components. The bimodal volcanic rocks were formed under a continental rift setting. The rift experienced extension in the early period of the Early Carboniferous and its final closure arose after a late period of the Late Carboniferous. [ABSTRACT FROM AUTHOR]

What is the impact of performance-based budgeting (PBB) on governmental spending? Do various PBB implementation strategies result in different outcomes? The authors, Jack Yun-jie Lee of National Open University in Taiwan and XiaoHu Wang of the University of Central Florida, gathered data from the United States, Taiwan, and China (Guangdong Province) to explore the possible intermediate- and long-term results of PBB. The data demonstrate how the impacts of PBB vary across countries and regions. [ABSTRACT FROM AUTHOR]