Island Biocultural Assemblages — The Case of Kinmen Island

ABSTRACT A growing mass of research contributes to our understanding of how biological and cultural diversity are related in complex and important ways. This paper presents an assembling process of biodiversity and cultural diversity on an island, Kin‐men (Quemoy), based on 1600 years of its environmental history. The study shows that the island's biocultural assemblages are a result both of external relations with the island's surrounding environment and internal relations within the island's changing human ecology. Distant political powers and economic forces are the two major external influences that have affected the flow of natural and cultural elements to and from the island, while ‘screening effects’ and ‘isolation effects’ are two factors that explain internal interactions. The island's biocultural assembling processes reveal that the openness of the island facilitates increase in the diversity of biocultural elements, while its less disturbed isolated condition fosters natural succession and co‐evolution. The study suggests that biocultural assemblages and the associated processes of co‐evolution and nature–society interactions are accomplished through the intermittent opportunities purposively provided by or inadvertently found in the openings and closures of boundaries, setting the scene for both boundary crossings and bounded shelter, by intent or chance.     

Experimental investigation of carbon dioxide trapping due to capillary retention in saline aquifers

Capillary trapping is a physical mechanism by which carbon dioxide (CO₂) is naturally immobilized in the pore spaces of aquifer rocks during geologic carbon sequestration operations, and thus a key aspect of estimating geologic storage potential. Here, we studied capillary trapping of supercritical carbon dioxide (scCO₂), and the effect of initial scCO₂ saturation and flow rate on the storage/trapping potential of Berea sandstone. We performed two‐phase, scCO₂‐brine displacements in two samples, each subject to four sequential drainage–imbibition core‐flooding cycles to quantify end‐point saturations of scCO₂ with the aid of micro‐ and macro‐computed tomography imaging. From these experiments, we found that between 51% and 75% of the initial CO₂ injected can be left behind after the brine injection. We also observed that the initial scCO₂ saturation influenced the residual scCO₂ saturation to a greater extent than the rate of brine injection under the experimental conditions examined. In spite of differences in the experimental conditions tested, as well as those reported in the literature, initial and residual saturations were found to follow a consistent relationship.     

日本右翼势力支持"台独"的历史考察

日本右翼势力对“台独”的支持大体经历了三个时期:战后初期,日本右翼势力是“台独”逆流的始作俑者和首开“台独”运动先河的罪魁祸首;冷战时期,日本右翼势力不仅在中日复交前使本国成为“台独”势力的大本营,而且在中日复交后仍一如既往、不遗余力地支持“台独”;后冷战时期,日本右翼势力支持“台独”不仅变本加厉,而且呈现出民间与政界配合、右翼与政府呼应之特点。     

“本土安全”思想对中国近代海疆安全战略的影响

本土安全是近代中国海疆安全战略的终极目标。由于战略目标的局限,中国虽然拥有具备远洋作战能力的海军,但却无法在海军军备建设、军力部署,以及战略战备等方面摆脱海岸防御战略的影响。受本土安全思想的影响,中国的战略决策者在甲午战争中屡失战机,而近代中国海疆安全战略体系也因此崩溃。     

Gas breakthrough experiments on fine-grained sedimentary rocks

The capillary sealing efficiency of fine‐grained sedimentary rocks has been investigated by gas breakthrough experiments on fully water saturated claystones and siltstones (Boom Clay from Belgium, Opalinus Clay from Switzerland and Tertiary mudstone from offshore Norway) of different lithological compositions. Sand contents of the samples were consistently below 12%, major clay minerals were illite and smectite. Porosities determined by mercury injection lay between 10 and 30% while specific surface areas determined by nitrogen adsorption (BET method) ranged from 20 to 48 m² g ^{? 1}. Total organic carbon contents were below 2%. Prior to the gas breakthrough experiments the absolute (single phase) permeability (k_abs) of the samples was determined by steady state flow tests with water or NaCl brine. The k_abs values ranged between 3 and 550 nDarcy (3 × 10^?21 and 5.5 × 10^?19 m²). The maximum effective permeability to the gas‐phase (k_eff) measured after gas breakthrough on initially water‐saturated samples extended from 0.01 nDarcy (1 × 10^?23 m²) up to 1100 nDarcy (1.1 × 10^?18 m²). The residual differential pressures after re‐imbibition of the water phase, referred to as the ‘minimum capillary displacement pressures’ (P_d), ranged from 0.06 to 6.7 MPa. During the re‐imbibition process the effective permeability to the gas phase decreases with decreasing differential pressure. The recorded permeability/pressure data were used to derive the pore size distribution (mostly between 8 and 60 nm) and the transport porosity of the conducting pore system (10^‐5–10^‐2%). Correlations could be established between (i) absolute permeability coefficients and the maximum effective permeability coefficients and (ii) effective or absolute permeability coefficients and capillary sealing efficiency. No correlation was found between the capillary displacement pressures determined from gas breakthrough experiments and those derived theoretically by mercury injection.     

Capillary Active Interior Insulation Systems for Wall Retrofitting: A More Nuanced Story

To thermally upgrade exterior masonry walls, interior insulation is often the only possible retrofitting technique, especially when dealing with historic buildings. Unfortunately, it is also the riskiest post-insulation technique, as frost damage, interstitial condensation, and other damage patterns might be induced. To diminish those risks, nowadays so-called capillary active interior insulation systems are often promoted. These systems aim a minimal reduction of the inward drying potential, while interstitial condensation is buffered.

Currently, several capillary active systems are on sale. These different types have, however, widely varying properties. In this article, a closer look at the hygrothermal properties and the working principle of a number of “capillary active” interior insulation systems is made. The spread in capillary absorption coefficients and the vapor diffusion resistances of the different systems is discussed and their influence is illustrated. Based on all this, a more nuanced view on capillary active insulation systems is pursued.

Abbreviations: AC: aerated concrete; CaSi: calcium silicate; GM: glue mortar; GB: gypsum board; HAMFEM: Heat Air and Moisture Finite Element Method; MW: mineral wool; PE: polyethylene; PIR: polyisocyanurate; PUR: polyurethane; VIP: vacuum insulation panel; WFB: wood fiber board; XPS: extruded polystyrene; sd_dry: dry vapor diffusion resistance factor; µ_dry: dry vapor diffusion resistance     

"台独"势力的"日本情结"问题

“台独”分子有一个共同的特性,就是都具有浓厚的“日本情结”,这也是驱动“台独”势力长期不遗余力从事分裂祖国活动和造成台湾问题久拖不决的重要因素。究其原因,主要有二：1、日本对台湾50年的殖民统治,特别是它所发动的“皇民化运动”的久远影响,是导致“台独”势力“日本情结”产生的历史原因;2、“台独”势力出于台湾“独立”的欲求,急需取得外部势力特别是与台湾渊源甚深的日本右翼势力的支持,这是“台独”势力“日本情结”产生的现实原因,也是主要原因。     

In situ decarboxylation of acetic and formic acids in aqueous inclusions as a possible way to produce excess CH4

Accurate reconstruction of diagenetic P‐T conditions in petroleum reservoirs from fluid inclusion data relies on valid measurements of methane concentration in aqueous inclusions. Techniques have been developed (Raman spectrometry) to provide sufficiently accurate data, assuming measured methane concentration has not been modified after aqueous inclusion entrapment. This study investigates the likelihood that organic acids derived from petroleum fluids and dissolved in formation water might suffer decarboxylation upon postentrapment heating within the fluid inclusion chamber, thereby generating excess CH₄ in the inclusions. Four different experiments were conducted in fused silica capillary capsules (FSCCs), mimicking fluid inclusions. The capsules were loaded with acetic (CH₃COOH) or formic (HCOOH) acid solution and were heated to 250°C for short durations (<72 h) in closed‐system conditions, with or without applying a fixed P_H2. Reaction products were characterized by Raman and FT‐IR spectrometry. Results indicate that decarboxylation reactions did take place, at variable degrees of progress, and that measurable excess CH₄ was produced in one experiment using acetic acid. This suggests that methane may be produced from dissolved organic acids in natural aqueous inclusions in specific situations, possibly inducing errors in the thermodynamic interpretation.     

部落与民族主义的竞逐——1953年法国在摩洛哥的政变与格拉维部落的兴衰

部落构成了中东社会生活的一个重要层面,是理解中东国家必不可少的视角。1953年,法国在摩洛哥发动政变,废黜了支持民族主义力量的苏丹穆罕默德五世。格拉维部落在此期间经历了兴衰起落。此次政变集中反映了摩洛哥国内部落和民族主义力量对国家政权的竞逐,是观察中东地区部落和国家间复杂逻辑关系的典型个案。摩洛哥传统势力的代表格拉维部落与国家间关系表现出复杂形态:部落利用国家力量实现崛起,部落对抗民族主义力量发动政变企图控制国家,最后部落被国家抛弃而衰落。在部落和民族主义竞逐国家政权的过程中,法国殖民者成为二者沉浮的决定性因素和制衡力量。由于部落对国家认同的脆弱性,殖民主义政权得以通过玩弄部落认同对殖民地进行分而治之。     

Out of Arabia: British Strategy and the Fate of Local Forces in Aden,South Yemen,and Oman, 1967–76

The British engagement with Oman from 1967–76 came at a time when other imperial and defence commitments were being reduced in the Gulf region and elsewhere. Following the ignominious retreat from Aden, the British chose to support the Omani regime in its conflict with Communist-inspired insurgents (1970–6). This article gives context to the dichotomy of outcomes in southern Arabia and examines the role of local military forces in the counter-insurgencies. It demonstrates that Britain's domestic political considerations, regional strategic requirements, and concerns for its global reputation, rather than counterinsurgency operations and the local forces, were the main drivers of outcomes. Insurgents and local actors nevertheless responded to changes taking place in and around Oman, recalibrating their decision to co-operate or resist on their own terms, and changes in the international support for the insurgents were decisive. The key argument is that the dynamic combinations of international support, British strategic assumptions and miscalculations, and local agency, were crucially important to the outcomes in the region. The ‘fate’ of those who had allied with, or resisted, the British, needs to be set in this context.