Present-day Upper-crustal Strain Rate Field in Southeastern Tibet and its Geodynamic Implications:Constraints from GPS Measurements with ABIC Method

The Earth’s surface kinematics and deformation are fundamental to understanding crustal evolution.An effective research approach is to estimate regional motion field and deformation fields based on modern geodetic networks.If the discrete observed velocity field is obtained,the velocity related fields,such as dilatation rate and maximum shear strain rate,can be estimated by applying varied mathematical approaches.This study applied Akaike's Bayesian Information Criterion(ABIC)method to calculate strain rate fields constrained by GPS observations in the southeast Tibetan Plateau.Comparison with results derived from other three methods revealed that our ABIC-derived strain rate fields were more precise.The maximum shear strain rate highlighted the Xianshuihe–Xiaojiang fault system as the main boundary for the outward migration of material in southeastern Tibet,indicating rotation of eastern Tibet material around the eastern Himalaya rather than whole extrusion along a fixed channel.Additionally,distinct dilatation rate patterns in the northeast and southwest regions of the fault system were observed.The northeast region,represented by the Longmenshan area,exhibited negative dilatational anomalies;while the southwest region,represented by the Jinsha River area north of 29°N,displayed positive dilatational anomalies.This indicates compression in the former and extension in the latter.Combined with deep geophysical observations,we believe that the upper and lower crusts of the Jinsha River area north of 29°N are in an entire expanding state,probably caused by the escape-drag effect of material.The presence of a large,low-viscosity region south of 29°N may not enable the entire escape of the crust,but instead result in a differential escape of the lower crust faster than the upper crust.

Multiple Uplift and Exhumation of the Southeastern Tibetan Plateau:Evidence from Low-Temperature Thermochronology

Since the Cenozoic,the Tibetan Plateau has experienced large-scale uplift and outgrowth due to the India-Asia collision.However,the mechanism and timing of these tectonic processes still remain debated.Here,using apatite fission track dating and inverse thermal modeling,we explore the mechanism of different phases of rapid cooling for different batholiths and intrusions in the southeastern Tibetan Plateau.In contrast to previous views,we find that the coeval granitic batholith exposed in the same tectonic zone experienced differential fast uplift in different sites,indicating that the present Tibetan Plateau was the result of differential uplift rather than the entire lithosphere uplift related to lithospheric collapse during Cenozoic times.In addition,we also suggest that the 5-2 Ma mantle-related magmatism should be regarded as the critical trigger for the widely coeval cooling event in the southeastern Tibetan Plateau,because it led to the increase in atmospheric CO_(2)level and a hotter upper crust than before,which are efficient for suddenly fast rock weathering and erosion.Finally,we propose that the current landform of the southeastern Tibetan Plateau was the combined influences of tectonic and climate.

Quantifying Contribution of Recycled Moisture to Precipitation in Temperate Glacier Region,Southeastern Tibetan Plateau,China

Recycled moisture is an important indicator of the renewal capacity of regional water resources.Due to the existence of Yulong Snow Mountain,Lijiang in Yunnan Province,southeast of the Qinghai-Tibet Plateau,China,is the closest ocean glacier area to the equator in Eurasia.Daily precipitation samples were collected from 2017 to 2018 in Lijiang to quantify the effect of sub-cloud evaporation and recycled moisture on precipitation combined with the d-excess model during monsoon and non-monsoon periods.The results indicated that the d-excess values of precipitation fluctuated between–35.6‰and 16.0‰,with an arithmetic mean of 3.5‰.The local meteoric water line(LMWL)wasδD=7.91δ^(18)O+2.50,with a slope slightly lower than the global meteoric water line(GMWL).Subcloud evaporation was higher during the non-monsoon season than during the monsoon season.It tended to peak in March and was primarily influenced by the relative humidity.The source of the water vapour affected the proportion of recycled moisture.According to the results of the Hybrid Single-Particle Lagrangian Integrated Trajectory(HYSPLIT)model,the main sources of water vapour in Lijiang area during the monsoon period were the southwest and southeast monsoons.During the non-monsoon period,water vapour was transported by a southwesterly flow.The recycled moisture in Lijiang area between March and October 2017 was 10.62%.Large variations were observed between the monsoon and non-monsoon seasons,with values of 5.48%and 25.65%,respectively.These differences were primarily attributed to variations in the advection of water vapour.The recycled moisture has played a supplementary role in the precipitation of Lijiang area.

Hydrothermal Systems Characterized by Crustal Thermally-dominated Structures of Southeastern China

Southeastern China(SE China)is located in the Pacific tectonic domain and has experienced a series of tectono-magmatic events induced by the subduction of the Paleo-Pacific Plate since the late Mesozoic.The subduction formed a series of NE-NNE oriented faults under a NW-SE regional stress field,along which a number of thermal springs occur.Previous studies have focused on the genesis mechanism of specific geothermal fields in SE China,but the general characteristics of hydrothermal systems in SE China remains unclear.In this study,we investigate the correlation between geothermal activity,hydrochemical type and regional faults by studying the distribution of hydrothermal activity and geochemical properties of typical hydrothermal systems in SE China.The hydrothermal systems in SE China have a crustal thermally-dominated structural origin unique to the specific geological and tectonic conditions of the Eurasian Plate margin.The upwelling of the asthenosphere and the widespread granitoids with high radiogenic heat production in SE China provide major heat sources for regional geothermal anomalies.The NE-oriented crustal thermally-dominated faults are critical for the formation of geothermal anomalies and NW-oriented extensional faults have created favorable conditions for meteoric water infiltration,transportation and the formation of thermal springs.

Spatiotemporal distribution of regional landslides and erosion rates in Southeastern Tibet

The difficulty in estimating ages of regional landslides hampers to assess frequency of landslides and hence to quantitatively assess regional landslide hazard.In this study,we used radiocarbon dating of organic sediment on boulder rock varnish to estimate landslide ages in Langxian(LX)arid region in southeastern Tibet.Samples of rock varnish with organic sediment were collected on site for radiocarbon dating,leading to landslide ages from 1880±30 to 18,430±30 yr B.P.To measure surface roughness characteristics of 109 remotely-mapped large bedrock landslide deposits,we estimated average standard deviation of slope(SDS)over an area of~640 km^(2) by calculating the slope gradient of each raster cell and using a rectangular moving window method in Arc Map from a 5 m-resolution Digital Elevation Model generated from helicopterobtained photographs.Combing estimated landslide ages(t)with average surface roughness of mapped landslide deposits(R)quantified by SDS,we fit an exponential landslide deposits surface roughness-age function(t=1.47×10^(6)×e^(-1).46R,r2=0.63)that was used to estimate regional landslide ages in LX.We conclude that three periods with clusters of regional landslides in LX were revealed by different surface roughness of landslide deposits combing roughness-age function,with the values of 5563-7455 yr B.P.,1724-4151 yr B.P.,and 960-1287 yr B.P..Furthermore,we used our estimates of landslide ages to quantify landslide erosion rates of three corresponding hillslopes in LX ranging from 0.50 to 2.42 mm yr-1.Although rock varnish radiocarbon dating provides us a feasible option for timing regional landslides of arid regions,the epistemic uncertainty in the dating method should arouse our attention,which could be reduced by increasing the number of samples.

Insights into some large-scale landslides in southeastern margin of Qinghai-Tibet Plateau

The southeastern margin of Qinghai-Tibet Plateau(SMQTP)is of a typical large landslide-prone area due to intense tectonic activity,deeply incised valleys,high geostress and frequent earthquakes.To gain insights into large landslides in southeastern margin of Qinghai-Tibet Plateau,an area covering 3.34×105 km2 that extends 80e150 km on both sides of the Sichuan-Tibet traffic corridors(G318)was used to examine the spatial distribution and corresponding characteristics of landslides.The results showed that the study area contains at least 629 large landslides that are mainly concentrated on 7 zones(zones IeVII).Zones IeVII are in the southern section of the Longmenshan fault zone(with no large river)and sections with Dadu River,Jinsha River,Lancang River,Nujiang River and Yarlung Zangbo River.There are more landslides in the Jinsha River section(totaling 186 landslides)than the other sections.According to the updated Varnes classification,408 large landslides(64.9%)were recognized and divided into 4 major types,i.e.flows(275 cases),slides(58 cases),topples(44 cases)and slope deformations(31 cases).Flows,which consist of rock avalanches and iceerock avalanches,are the most common landslide type.Large landslide triggers(178 events,28.3%)are also recognized,and earthquakes may be the most common trigger.Due to the limited data,these landslide type classifications and landslide triggers are perhaps immature,and further systematic analysis is needed.

Combining RUSLE model and the vegetation health index to unravel the relationship between soil erosion and droughts in southeastern Tunisia

Droughts and soil erosion are among the most prominent climatic driven hazards in drylands,leading to detrimental environmental impacts,such as degraded lands,deteriorated ecosystem services and biodiversity,and increased greenhouse gas emissions.In response to the current lack of studies combining drought conditions and soil erosion processes,in this study,we developed a comprehensive Geographic Information System(GIS)-based approach to assess soil erosion and droughts,thereby revealing the relationship between soil erosion and droughts under an arid climate.The vegetation condition index(VCI)and temperature condition index(TCI)derived respectively from the enhanced vegetation index(EVI)MOD13A2 and land surface temperature(LST)MOD11A2 products were combined to generate the vegetation health index(VHI).The VHI has been conceived as an efficient tool to monitor droughts in the Negueb watershed,southeastern Tunisia.The revised universal soil loss equation(RUSLE)model was applied to quantitatively estimate soil erosion.The relationship between soil erosion and droughts was investigated through Pearson correlation.Results exhibited that the Negueb watershed experienced recurrent mild to extreme drought during 2000–2016.The average soil erosion rate was determined to be 1.8 t/(hm2•a).The mountainous western part of the watershed was the most vulnerable not only to soil erosion but also to droughts.The slope length and steepness factor was shown to be the most significant controlling parameter driving soil erosion.The relationship between droughts and soil erosion had a positive correlation(r=0.3);however,the correlation was highly varied spatially across the watershed.Drought was linked to soil erosion in the Negueb watershed.The current study provides insight for natural disaster risk assessment,land managers,and stake-holders to apply appropriate management measures to promote sustainable development goals in fragile environments.

Characteristics and mechanisms of the intraseasonal variability of sea surface salinity in the southeastern Arabian Sea during 2015-2020

Based on Soil Moisture Active Passive sea surface salinity(SSS)data from April 2015 to August 2020,combined with Objectively Analyzed Air-Sea Heat Flux and other observational data and Hybrid Coordinate Ocean Model(HYCOM)data,this work explores the characteristics and mechanisms of the intraseasonal variability of SSS in the southeastern Arabian Sea(SEAS).The results show that the intraseasonal variability of SSS in the SEAS is very significant,especially the strongest intraseasonal signal in SSS,which is located along the northeast monsoon current(NMC)path south of the Indian Peninsula.There are remarkable seasonal differences in intraseasonal SSS variability,which is very weak in spring and summer and much stronger in autumn and winter.This strong intraseasonal variability in autumn and winter is closely related to the Madden-Julian Oscillation(MJO)event during this period.The northeast wind anomaly in the Bay of Bengal(BOB)associated with the active MJO phase strengthens the East India Coastal Current and NMC and consequently induces more BOB low-salinity water to enter the SEAS,causing strong SSS fluctuations.In addition,MJO-related precipitation further amplifies the intraseasonal variability of SSS in SEAS.Based on budget analysis of the mixed layer salinity using HYCOM data,it is shown that horizontal salinity advection(especially zonal advection)dominates the intraseasonal variability of mixed layer salinity and that surface freshwater flux has a secondary role.

Subthermocline eddies carrying the Indonesian Throughflow water observed in the southeastern tropical Indian Ocean

We observed a subthermocline eddy(STE)with a cold and fresh core during an observation cruise along a transect of 10°S in the southeastern tropical Indian Ocean(SETIO)in December 2017.The vertical scale,speed radius,and maximum swirl velocity of the STE were about 200 m,55 km,and 0.5 m/s,respectively.The mean Rossby number and Burger number of the STE were then estimated to be about−0.7 and 2.4,indicating the STE was a submesoscale coherent vortex.The STE core water had characteristics of the Indonesian Throughflow(ITF)water and was distinct from that of surrounding areas.By examining Argo float data,another STE was well captured by five successive profiles of the same Argo float.Both STEs showed significant temperature and salinity anomalies at theσ0=26.0-26.5 kg/m3 surfaces.With the assumption that the low-salinity ITF water parcels could be carried only by surface eddies and the STEs,the Argo profiles,which detected low-salinity ITF water and were located outside a surface eddy,were believed to be inside an STE and were used to analyze the distribution,origin,and generation mechanism of the STE.The results suggested that the STEs carrying ITF water may be generated under topography-current interaction at the eastern coastal waters or under front-induced subduction in the area away from coastal waters.Those STEs may be widely distributed in the SETIO and may play a role in ITF water parcel transport.

Mixed layer warming by the barrier layer in the southeastern Indian Ocean

The southeastern Indian Ocean is characterized by the warm barrier layer(BL)underlying the cool mixed layer water in austral winter.This phenomenon lasts almost half a year and thus provides a unique positive effect on the upper mixed layer heat content through the entrainment processes at the base of the mixed layer,which has not been well evaluated due to the lack of proper method and dataset.Among various traditional threshold methods,here it is shown that the 5 m fixed depth difference can produce a reliable and accurate estimate of the entrainment heat flux(EHF)in this BL region.The comparison between the daily and monthly EHF warming indicates that the account for high-frequency EHF variability almost doubles the warming effect in the BL period,which can compensate for or even surpass the surface heat loss.This increased warming is a result of stronger relative rate of the mixed layer deepening and larger temperature differences between the mixed layer and its immediate below in the daily-resolving data.The interannual EHF shows a moderately increasing trend and similar variabilities to the Southern Annular Mode(SAM),likely because the mixed layer deepening under the positive SAM trend is accompanied by enhanced turbulent entrainment and thus increases the BL warming.

Hydrocarbon accumulation conditions and exploration targets of the Sinian Dengying Formation in the Southeastern Sichuan Basin

No breakthrough has been made in petroleum exploration of the Sinian Dengying Formation in the southeastern Sichuan Basin as the major factors controlling the hydrocarbon accumulation of the Dengying Formation have not been well established,including the development period and distribution of the platform margin,the effectiveness of the source-reservoir combination and the reliability of the Cambrian pre-salt structural trap.Based on the interpretation of seismic data and hydrocarbon-source correlation,the distribution of the platform margin of the Sinian Dengying Formation in the southeastern Sichuan Basin was mapped.Moreover,the gas source rocks of the Dengying Formation were clarified according to geochemical characteristics of fluid inclusions,and the pre-salt structures were further confirmed by seismic forward modeling and experiments of prestack depth migration.Results showed that the sedimentary facies of the 4th member of Dengying Formation in the southeastern Sichuan Basin was platform margin of gentle slope type.The platform margin reservoir of the Dengying Formation and the Lower Cambrian source rocks constitute a favorable source-reservoir combination.The carbon isotope characteristics of gas in fluid inclusions indicate that some of the oil/gas in the Dengying Formation were contributed by the Doushantuo Formation source rocks.As the difference in seismic velocities between carbonate rocks and gypsum/salt beds may cause a reduction in the amplitude of pre-salt structures,the low-amplitude structures identified on current seismic profiles are underestimated instead of overestimated.Accordingly,the Sinian structural traps are confirmed to develop in the deep pre-salt sequences in the low-steep anticline belt,southeastern Sichuan Basin.On the basis of the above new understanding,we propose two types of hydrocarbon migration modes for the Sinian Dengying Formation in southeastern Sichuan Basin,including lateral migration of hydrocarbons generated from the Cambrian Qiongzusi Formation and vertical migration of hydrocarbons derived from the Sinian Doushantuo Formation.Lithologic traps at the platform margin and pre-salt structural traps within the platform are favorable targets for natural gas exploration.

河南省三级公立医院智慧管理建设现状调查与分析

目的:调查分析河南省三级公立医院智慧管理建设现状,为公立医院推动智慧管理建设提供参考。方法:对河南省143所三级公立医院信息管理部门的主管人员和负责管理信息化建设的院领导进行调查。结果:80%的受访医院已开始推进智慧管理建设工作,但仍面临资金和资源不足、技术能力储备不足和业务系统协同困难等挑战。虽然医院智慧管理各业务域的信息化系统建设已有所进展,但在设备设施管理、运营管理、运行保障管理和教学科研管理等方面信息系统建设率相对较低。结论:医院智慧管理建设应实事求是,强化顶层设计与组织管理,进一步提升信息化建设水平,加强数据治理与决策支持。

中国东西部陆相页岩油地质特征差异性分析及其对富集规律影响——以胜利探区为例

以胜利探区为例,系统对比研究了中国东西部陆相湖盆页岩油地质特征差异性及其对富集规律的影响。济阳坳陷沙四段上亚段—沙三段下亚段在古地貌、古气候、古水体介质等因素共同控制下,富有机质纹层状碳酸盐页岩大规模分布,富有机质黏土纹层成烃与富碳酸盐纹层成储协同演化为游离烃规模富集提供了有利条件。准噶尔盆地西北缘哈山地区风城组强裂陷作用导致强烈火山活动,在火山喷发物质与古气候共同影响下,富有机质纹层状含碱长英页岩相大规模分布,且成烃成储演化过程中形成较多的长英质矿物,并伴生大量的基质溶蚀孔和晶间孔,为页岩油富集奠定了重要基础。哈山地区在多期逆冲推覆过程中,准原地系统持续生烃、油多气少和相对较好的保存条件以及构造覆压、生烃增压作用产生的异常高压为页岩油高产提供了必要条件。准噶尔盆地东南缘(准东南)芦草沟组在海迹湖咸水环境下,受火山凝灰质与微生物作用影响,形成了富有机质纹层状页岩相夹贫有机质层状白云岩相的主要岩相组合类型。博格达山周缘山前构造带芦草沟组富有机质页岩均进入成熟演化阶段,胜利探区构造相对稳定区具备页岩油勘探前景。

“胡焕庸线”两侧高中生健康素养与静坐时长态势特征调查研究

背景目前“胡焕庸线”的学术价值已经延伸至其他相关学科,考虑到我国人口众多且分布差异较为明显的特点,本研究借鉴人口地理学的研究成果,旨在探索按照“胡焕庸线”的人口密度分布界定标准,深入研究了“胡焕庸线”两侧城乡高中生的健康素养和静坐时长的态势特征。目的调查分析“胡焕庸线”两侧东南半壁与西北半壁的城乡高中生健康素养与静坐时长的现状态势特征,为改善我国高中生的身心健康水平提供依据。方法采用分层整群随机抽样方法,于2019年1—3月对我国31个省(直辖市、自治区)在内的62所学校高一、高二学生进行健康素养与静坐时长的调研(统一提前邮寄配发健康素养调查问卷与静坐时间调查问卷各12400份)。采用多元线性回归模型分析方差膨胀系数,校正混杂因素后分析“胡焕庸线”两侧东南半壁与西北半壁高中生静坐时长的影响因素。结果最后纳入健康素养调查问卷9057份,其中东南半壁7489份(82.7%),西北半壁1568份(17.3%);纳入静坐时间调查问卷8031份,其中东南半壁6614份(82.4%),西北半壁1417份(17.6%)。东南半壁高中生健康素养评分、静坐时长均高于西北半壁(Z=-4.009、-9.198,P<0.001)。东南半壁年龄为17、18岁,女性,城乡,父亲学历为大专以下、大专,母亲学历为大专、本科,家庭年收入为1~万、5~万、8~万、>10万元,家庭人口数为1、3、7、9、≥10人的高中生健康素养评分均高于西北半壁(P<0.05);东南半壁年龄为15、16、18岁,男女,城乡,父亲学历为大专以下、大专,母亲学历为大专以下,家庭年收入为<1万、2.5~万、5~万、8~万、>10万元,家庭人口数为3、4、5、6人的高中生静坐时长均长于西北半壁(P<0.05)。多元线性回归模型分析结果显示,校正混杂因素后,东南半壁高中生静坐时长与家庭年收入(β=0.324)和母亲学历(β=0.644)均呈正相关,但与健康素养评分(β=-0.015)和父亲学历(β=-0.212)均呈负相关(P<0.05);标准化回归系数β比较,家庭年收入(0.164)>母亲学历(0.131)>父亲学历(-0.056)>健康素养评分(-0.050)。西北半壁高中生静坐时长与健康素养评分(β=0.017)、父亲学历(β=0.789)、母亲学历(β=0.540)均呈正相关(P<0.05);标准化回归系数β比较,父亲学历(0.163)>母亲学历(0.111)>健康素养评分(0.056)。结论东南半壁高中生健康素养评分、静坐时长均高于西北半壁。东南半壁高中生静坐时长与家庭年收入和母亲学历呈正相关,但与健康素养评分和父亲学历呈负相关;西北半壁高中生静坐时长与健康素养评分父母亲学历均呈正相关。家庭年收入对东南半壁高中生静坐时长影响的权重最高,父亲学历对西北半壁高中生静坐时长影响的权重最高。

滇东南薄竹山花岗岩年代学、地球化学特征及地质意义

滇东南薄竹山地区W-Sn-Pb-Zn多金属矿床与该区大型复式花岗岩体有密切的成因联系。为了探讨该花岗岩体的侵位时代、岩石成因及形成背景,对薄竹山花岗岩开展了岩石地球化学、锆石U-Pb定年及Hf同位素测试。结果表明,该花岗岩可划分为两期,其中晚期花岗岩LA-ICP-MS锆石U-Pb年龄为(87.08±0.55)~(87.29±0.69)Ma。两期花岗岩均具高的SiO_(2)(63.37%~72.07%)、K_(2)O(4.96%~6.19%),贫Fe、Mg的特征,A/CNK值为1.03~2.42,轻重稀土元素分异明显(LREE/HREE=14.0~26.5),Eu明显负异常(δEu=0.38~0.62),富含大离子亲石元素Rb、Th、U及稀土元素La、Ce、Nd,亏损Ba、Ta、Nb、Sr、Y和Yb,ε_(Hf)(t)值为−9.31~−5.14,具有高钾钙碱性过铝质S型花岗岩的地球化学和同位素特征;Hf同位素二阶段模式年龄(t_(DM2))为1476~1737 Ma,说明岩浆可能来源于早中元古代下地壳部分熔融。综合研究认为,薄竹山花岗岩是白垩纪伸展背景下软流圈地幔上涌导致的早中元古代下地壳物质部分熔融所形成。

华南陆缘火成岩区差异性地壳热结构及地热意义

高产热花岗岩是重要的壳内热源之一,我国华南陆缘花岗岩体分布广泛,为该区浅表热量的生成及聚集提供了可能。本文在简述区内花岗岩资源分布的基础上,系统分析了区内主要花岗岩体的放射性生热特征,并结合区内近些年施工的地热勘探深钻,对重点地热勘查区的深部地温场分布、地热通量、地壳热结构等进行了对比分析,提出了华南陆缘浅表地热资源的聚热模式。分析认为,华南陆缘地区具有“幔源供热-壳内生热-断裂传热-盖层保热”的四元聚热模式,其中,花岗岩体的放射性生热率是影响区内浅部地温场的主要因素之一,粤北—赣南岩体的生热率明显高于漳州地区的花岗岩体,其近似“热壳冷幔”型或“温壳温幔”型岩石圈热结构与漳州“热幔冷壳”型岩石圈热结构有一定的差异;断裂构造及盖层条件对于地下热量聚集及散失具有明显的控制作用。研究成果对于深入理解华南陆缘地热资源的成因、控热因素,以及今后该地区地热资源勘探开发实践具有一定的理论与指导意义。

河南省生态文明示范创建工作研究

生态文明示范创建是生态环境部门推进生态文明建设的重要载体和平台,也是河南省各市(区、县)开展生态文明建设工作的重要抓手。本文系统梳理了国家生态文明示范区、省级生态县创建要求,总结了河南省各市(区、县)国家生态文明示范区、省级生态县创建工作,分析了创建国家生态文明示范区、省级生态县时容易出现的共性问题,并提出针对性建议,以期为国家生态文明示范区、省级生态县的创建提供一定借鉴。

古代云南东南部的变迁

古代的云南东南部,包括今红河哈尼族彝族自治州、文山壮族苗族自治州及附近一些地区。云南东南部的演变有以下特点:一是这一地区距滇池、洱海流域两大区域中心较远,同时未形成强大的地方势力,在政治舞台上便显落寞;二是云南中部至越南的交趾道经过这一地区,云南东南部的发展与交趾道兴衰密切相关;三是云南东南部与越南毗连,越南与中国历代王朝关系的改变,深刻地影响云南东南部;四是云南东南部的变化经历先慢后快的过程。自元代起,云南东南部获得较快发展,清代尤为明显。

抗战时期东南地区的文艺民族形式讨论

抗战时期,闽浙赣粤四省毗连的东南地区,是一块相对独立的抗战区域。发生在这一区域的文艺民族形式讨论,规模足以与以延安为中心的西北地区和以重庆、桂林为中心的西南地区的讨论鼎足而三。东南地区的文艺民族形式讨论,没有形成讨论的焦点,但形成了几个较为固定的论域,且取得了一些较为相近的意见,在“孤悬东南”“区自为战”的情况下,还形成了自己的区域性特征,做出了自己独特的贡献。

鄂东南传统民居室内热环境评价及围护结构优化设计研究——以赤壁市安丰村但耔臾宅为例

文章以湖北省赤壁市安丰村但耔臾宅为研究对象,对民居现场温湿度、风速、围护结构热工性能进行实测,通过软件仿真模拟及预计适应性平均热感觉指标(APMV)对其室内热环境进行评价。实测与模拟分析表明:民居夏季闷热(室内平均温度为33.41℃,峰值温度达37.20℃,平均风速为0.073m/s),冬季湿冷(室内平均温度为6.90℃,相对湿度为68.8%);屋顶和窗户材料单一,构造做法简易,热工性能较差;全年热环境时间占比分别为Ⅰ级22.0%、Ⅱ级41.8%和Ⅲ级36.2%,整体热环境质量较低。因此,提出屋顶增设2mm厚沥青卷材作防水层,40mm厚聚苯乙烯泡沫(XPS)板作保温层;窗户改用空气层厚度9mm的普通双层中空玻璃窗;北墙调整窗户尺寸为1000mm×1200 mm,东墙增设安装遮阳装置的800mm×1000mm小尺寸窗户等优化策略,并模拟验证其优化效果。为鄂东南地区传统民居的室内热环境改善提供了实用的参考依据。