Ecosystem carbon storage and sink/source of temperate forested wetlands in Xiaoxing’anling, northeast China

Wetlands play an important role in the global carbon cycle, but there are still considerable uncertainties in the estimation of wetland carbon storage and a dispute on whether wetlands are carbon sources or carbon sinks. Xiaoxing’anling are one of several concentrated distribution areas of forested wetland in China, but the carbon storage and carbon sink/source of forested wetlands in this area is unclear. We measured the ecosystem carbon storage (vegetation and soil), annual net carbon sequestration of vegetation and annual carbon emissions of soil heterotrophic respiration of five typical forested wetland types (alder swamp, white birch swamp, larch swamp, larch fen, and larch bog) distributed along a moisture gradient in this area in order to reveal the spatial variations of their carbon storage and quantitatively evaluate their position as carbon sink or source according to the net carbon balance of the ecosystems. The results show that the larch fen had high carbon storage (448.8 t ha^(−1)) (6.8% higher than the larch bog and 10.5–30.1% significantly higher than other three wetlands (P < 0.05), the white birch swamp and larch bog were medium carbon storage ecosystems (406.3 and 420.1 t ha^(−1)) (12.4–21.8% significantly higher than the other two types (P < 0.0 5), while the alder swamp and larch swamp were low in carbon storage (345.0 and 361.5 t ha^(−1), respectively). The carbon pools of the five wetlands were dominated by their soil carbon pools (88.5–94.5%), and the vegetation carbon pool was secondary (5.5–11.5%). At the same time, their ecosystem net carbon balances were positive (0.1–0.6 t ha^(−1) a^(−1)) because the annual net carbon sequestration of vegetation (4.0–4.5 t ha^(−1) a^(−1)) were higher than the annual carbon emissions of soil heterotrophic respiration (CO_(2) and CH_(4)) (3.8–4.4 t ha^(−1) a^(−1)) in four wetlands, (the alder swamp being the exception), so all four were carbon sinks while only the alder swamp was a source of carbon emissions (− 2.1 t ha^(−1) a^(−1)) due to a degraded tree layer. Our results demonstrate that these forested wetlands were generally carbon sinks in the Xiaoxing’anling, and there was obvious spatial variation in carbon storage of ecosystems along the moisture gradient.

Classification,metallogenesis and exploration of silver deposits in Daxing’anling of Inner Mongolia and its adjacent areas

By the end of 2020,83 silver deposits(or ore occurrences),including four super-large-scale deposits,nine large-scale deposits,33 medium-scale deposits and 37 small-scale deposits or ore occurrences,have been proved.The amount of silver metal exceeds 86000 t with average grade of 100 g/t,which makes Daxing’anling region one of the the most important silver ore belt in China.However,the metallogenic characteristics and metallogenesis need to be clarified.The silver deposits in the study area are classified into three main types,which are magmatic hydrothermal vein type,continental volcano-subvolcanic type and skarn type,respectively.The supergiant deposits include the Shuangjianzishan deposit(silver metal amount of 15214 t with average grade of 138 g/t),the Baiyinchagandongshan deposit(silver metal amount of 9446 t with average grade of 187 g/t),the Huaobaote deposit(silver metal amount of 6852 t with average grade of 170 g/t),and the Fuxingtun deposit(silver metal amount of 5240 t with average grade of 196 g/t).The silver deposits are mainly distributed in the central and south of the Daxing’anling area,and mainly formed in the Yanshanian period.The silver polymetallic deposits in the Daxinganling area are significantly controlled by regional faults and the junction zone of volcanic rock basins and their margins.The north-east trending deep faults are the most important ore-controlling structures in this area.The distribution of silver polymetallic deposits along the main faults is obvious,and the intersection area of multiple groups of faults often form important mine catchments.The Permian is the most important ore-bearing formation in this area,but some important silver polymetallic deposits occur in Mesozoic volcanic basins or pre-Mesozoic strata.The magmatic rocks related to mineralization are mainly intermediate acidic or acidic intrusions,intermediate acidic lavas,pyroclastic rocks,and small intrusions of ultra-shallow or shallow facies of the Yanshanian Period.The mineralization element combination is mainly determined by the elemental geochemical background of surrounding rocks or source layers.In addition,the type of deposit,the distance from the mineralization center,and the degree of differentiation of ore-forming rock mass are also important influence factors.The article analyzes the prospecting prospects of each silver deposit type in the study area,discusses the relationship between mineralization center and deep prospecting,and proposes that porphyry silver deposits should be paid attention to.In the prospecting and exploration of silver deposits,comprehensive evaluation and multi-target prospecting need to be strengthened because silver can coexist or be associated with a variety of metals.

Argillization mechanics of rock from the Xing’anling Group in the Beier depression of the Hailar basin

The reservoir of the Xing'anling Group in the Beier depression of the Hailar basin is loosely cemented with many tuffaceous grains.This causes argillization and collapse of the grain framework of the reservoir sandstones.A detailed study on the characteristics of rocks and minerals was carried out through polarized microscope,X-ray diffraction,X-ray fluorescence,SEM and energy spectrum analysis.The results indicate that the reason for argillization is the abundant pyroclastic,and especially tuffaceous,grains in the reservoir.The alkaline component is relatively high in some strata.These are easily altered to montmorillonite in diagenesis.Na+montmorillonite swells strongly when exposed to water.This is the fundamental reason for the reservoir's argillization and plugging.

Anle138b对oAβ_(1-42)诱导大鼠海马神经元线粒体功能损伤的影响

目的探究Anle138b对慢性β淀粉样蛋白(Aβ)诱导的海马神经元线粒体功能损伤的影响。方法取出生24 h以内的SD乳鼠,原代培养海马神经元,待细胞成熟将其分为对照组(不进行任何处理)、oAβ_(1-42)组(100 nmol/L oAβ_(1-42)处理7 d)、oAβ_(1-42)+Anle138b组(100 nmol/L oAβ_(1-42)+100 nmol/L Anle138b共处理7 d)、Anle138b组(100 nmol/L Anle138b处理7 d)。各组处理结束后,应用流式细胞术检测活性氧(ROS)和线粒体膜电位(Δψm)阳性细胞的变化。结果析因设计的方差分析显示,oAβ_(1-42)和Anle138b的主效应明显(F_(oAβ1-42)=14.149、38.209,F_(Anle138b)=1.942、24.871,P<0.01),oAβ_(1-42)和Anle138b之间有交互性作用(F_(交互)=18.425、21.904,P<0.01)。单独效应分析显示,用oAβ_(1-42)处理时,Anle138b的处理效应明显(F=16.483、19.148,P<0.01);不用Anle138b处理时,oAβ_(1-42)的处理效应明显(F=14.149、38.209,P<0.01)。结论Anle138b可以减轻oAβ_(1-42)引起的海马神经元氧化应激和线粒体损伤,抑制oAβ_(1-42)对海马神经元的损伤。

Study of seasonal snow cover influencing the ground thermal regime on western flank of Da Xing'anling Mountains,northeastern China

Although many studies relevant to snow cover and permafrost have focused on alpine, arctic, and subarctic areas, there is still a lack of understanding of the influences of seasonal snow cover on the thermal regime of the soils in permafrost regions in the mid-latitudes and boreal regions, such as that on the westem flank of the Da Xing＇anling （Hinggan） Mountains, northeastern China. This paper gives a detailed analysis on meteorological data series from 2001 to 2010 provided by the Gen＇he Weather Station, which is located in a talik of discontinuous permafrost zone and with sparse meadow on the observation field. It is inferred that snow cover is important for the ground thermal regime in the middle Da Xing＇anling Mountains. Snow cover of 10-cm in thickness and five to six months in duration （generally November to next March） can reduce the heat loss from the ground to the atmosphere by 28%, and by 71% if the snow depth increases to 36 cm. Moreover, the occurrence of snow cover resulted in mean annual ground surface temperatures 4.7-8.2℃ higher than the mean annual air temperatures recorded at the Gen＇he Weather Station, The beginning date for stable snow cover establishment （SE date） and the initial snow depth （SDi） also had a great influences on the ground freezing process. Heavy snowfall before ground surface freeze-up could postpone and retard the freezing process in Gen＇he. As a result, the duration of ground freezing was shortened by at least 20 days and the maximum depth of frost penetration was as much as 90 cm shallower.

固定化脂肪酶ANL-MARE催化酸解合成1-油酸-2-棕榈酸-3-亚油酸甘油三酯

1-油酸-2-棕榈酸-3-亚油酸甘油三酯(OPL)是人乳中主要的脂质组成,为满足婴幼儿配方食品母乳化需求,该试验探究了新型固定化脂肪酶ANL-MARE催化制备OPL的方法。试验成功制备和表征了固定化酶ANLMARE,并以ANL-MARE为生物催化剂,建立了一种用三棕榈酸甘油三酯(PPP)、油酸(OA)和亚油酸(LA)高效酶催化制备富含OPL结构脂的方法。经单因素和响应面试验优化,获得OPL最优合成工艺为:PPP与总脂肪酸的摩尔比1:14.27,OA与LA摩尔比为1:0.76,脂肪酶添加量12.70%,反应温度50℃,反应4 h,此条件下产物中OPL相对含量为47.93%,2位棕榈酸(sn-2 PA)占总棕榈酸(PA)的质量分数(sn-2 PA相对含量)为71.69%。此外,固定化酶ANL-MARE与商业脂肪酶相比,表现出较好的催化合成OPL的活性。综上所述,固定化酶ANL-MARE具有催化制备OPL结构脂的重大潜力,为人乳脂替代脂的高效制备提供了新策略和理论基础。

Geochemistry and tectonic significance of Early Cretaceous granites in Highland 1248 of Daxing'anling

The Early Cretaceous granitic complex in Highland 1248 of Daxing'anling successively consists of intruded granodiorite,monzonite granite and syenite granite. Through test analysis on the major,trace and rare earth elements of the intrusive complex,this study focuses on the source characteristics and tectonic environment of the original magma of intrusive complex. The results show that the intrusive rocks in Highland 1248 are meta-aluminous-peraluminous rocks in calc-alkaline series with homologous characteristics in δEu negative anomalies; the complex is enriched in LILE( Rb,Cs and K) and depleted in HFSE( lanthanide,Sc,Y,U,Nb and Ta),displaying the geochemical characteristics of I-type granites in active continental-margin subduction zones. The complex also has the characteristics of granites after the collision of plate with rich aluminum and high potassium,but significantly depleted Nb,Ta,Ti,P and other elements,i. e. in the orogenic evolutionary stage. The zircon U-Pb SHRIMP isotopic apparent age of the complex in Highland 1248 is 140. 0--141. 0Ma,and the formation time is in Early Cretaceous.

Spatial-temporal distribution and geochemistry of highly evolved Mesozoic granites in Great Xing’an Range,NE China:Discriminant criteria and geological significance

Highly evolved granite is an important sign of the mature continent crust and closely associated with deposits of rare metals.In this work,the authors undertake systematically zircon U-Pb ages and whole rock elemental data for highly evolved granitic intrusions from the Great Xing’an Range(GXR),NE China,to elucidate their discriminant criteria,spatial-temporal distribution,differentiation and geodynamic mecha-nism.Geochemical data of these highly evolved granites suggest that high w(SiO_(2))(>70%)and differentiation index(DI>88)could be quantified indicators,while strong Eu depletion,high TE_(1,3),lowΣREE and low Zr/Hf,Nb/Ta,K/Rb could only be qualitative indicators.Zircon U-Pb ages suggest that the highly evolved gran-ites in the GXR were mainly formed in Late Mesozoic,which can be divided into two major stages:Late Ju-rassic-early Early Cretaceous(162-136 Ma,peak at 138 Ma),and late Early Cretaceous(136-106 Ma,peak at 126 Ma).The highly evolved granites are mainly distributed in the central-southern GXR,and display a weakly trend of getting younger from northwest to southeast,meanwhile indicating the metallogenic potential of rare metals within the central GXR.The spatial-temporal distribution,combined with regional geological data,indicates the highly evolved Mesozoic granites in the GXR were emplaced in an extensional environ-ment,of which the Late Jurassic-early Early Cretaceous extension was related to the closure of the Mongol-Okhotsk Ocean and roll-back of the Paleo-Pacific Plate,while the late Early Cretaceous extension was mainly related to the roll-back of the Paleo-Pacific Plate.

Anle138b对oAβ_(1-42)诱导海马神经元突触毒性作用影响

目的探究Anle138b对慢性β淀粉样蛋白寡聚体1-42(oAβ_(1-42))诱导的海马神经元突触毒性作用影响。方法培养原代海马神经元细胞,细胞发育成熟后分为对照组(不进行任何处理)、oAβ_(1-42)组(100 nmol/L oAβ_(1-42)处理7 d)、Anle138b组(50 nmol/L Anle138b处理2 d)、oAβ_(1-42)+Anle138b组(100 nmol/L oAβ_(1-42)+50 nmol/L Anle138b共处理7 d)、oAβ_(1-42)+Anle138b 2 d组(100 nmol/L oAβ_(1-42)处理7 d,在oAβ_(1-42)处理的最后2 d加用50 nmol/L Anle138b)。各组处理结束后,应用单细胞膜片钳技术检测自发性兴奋性突触后电流(sEPSCs)的幅值、频率、半衰减时间。结果各组海马神经元细胞sEPSCs幅值、半衰减时间比较差异无统计学意义(F=2.215、1.043,P>0.05)。各组sEPSCs频率比较差异有统计学意义(F=15.490,P<0.001),两两比较显示,oAβ_(1-42)组的sEPSCs频率较对照组明显增加(q=6.507,P<0.001),oAβ_(1-42)+Anle138b组和oAβ_(1-42)+Anle138b 2 d组的sEPSCs频率较oAβ_(1-42)组明显降低(q=9.517、9.471,P<0.001),其他组间比较差异均无统计学意义(P>0.05)。结论Anle138b不仅可以预防慢性oAβ_(1-42)诱导的海马神经元细胞突触毒性作用,还可以消除慢性oAβ_(1-42)诱导的海马神经元细胞突触毒性作用。

基于Fredlund&Xing模型的渗流分析在川东红层梯田滑坡中的应用

四川省巴中市通江县新场镇七家沟村二社水头上滑坡为川东典型红层梯田滑坡,区内类似斜坡覆盖范围广泛,但针对该地区此类滑坡的渗流分析研究较少。在对滑坡区进行大量野外调查、勘查、资料收集的基础上,综合运用卫星遥感、无人机航拍、机载LiDAR、室内试验等技术手段,基于Fredlund&Xing土水特征曲线数学模型,采用Geo-Studio中SEEP/W模块进行渗流分析,将不同时间阶段分析结果与SLOPE/W模块耦合,继而得到稳定系数与降雨、时间之间的动态变化关系,揭示了滑坡的变形过程和形成机理。研究显示:(1)连续降雨促使坡体地下水位升高,稳定性降低,最终导致水头上滑坡整体失稳破坏;(2)滑坡变形过程、地下水出露特征与Geo-Studio计算结果基本吻合,说明基于Fredlund&Xing数值模拟在类似地区能提供较为准确的模拟结果;(3)开垦梯田(水田)会降低坡体稳定性。研究结果可为四川山区类似滑坡灾害进行隐患排查和主动防范提供理论支撑,为防灾减灾提供参考依据。

Zircon U-Pb geochronology,geochemistry and tectonic implication of volcanic rocks from Manketouebo Formation in Keyihe area of northern Great Xing'an Range

Zircon U-Pb isotope dating and whole-rock geochemical analyses were undertaken for the rhyolite,rhyolitic lithic crystal tuff and dacitic tuff from the Manketouebo Formation in the Keyihe area,in order to constrain their genesis and tectonic significance.Zircon LA-ICP-MS U-Pb data indicate that the rhyolite and rhyolitic lithic crystal tuff were formed during 137±5 Ma and 143±1 Ma,respectively.These volcanic rocks have high SiO2(70.03%–76.46%)and K2O+Na2O(8.10%–9.52%)contents,but low CaO(0.03%–0.95%)and MgO(0.07%–0.67%)contents,which belong to the peraluminous and high-K calc-alkaline rocks.They are enriched in light rare earth elements(REEs),and exhibit fractionation of light over heavy REEs,withδEu values of 0.37–0.83.The volcanic rocks are enriched in LILEs(e.g.,Rb,U and K)and depleted in HFSEs(e.g.,Nb,Ti,P and Ta).The chemical composition suggests that these volcanic rocks formed by partial melting of crust material.Combined with previous regional research results,the authors consider that the volcanic rocks of the Manketouebo Formation in the Keyihe area were formed under an extensional environment related to the closure of the Mongolia–Okhotsk Ocean.

醒脑开窍针刺法联合中药治疗脑梗死后轻度认知障碍的疗效观察

目的 观察醒脑开窍针刺法联合补肾益髓汤治疗脑梗死后轻度认知障碍的临床疗效。方法 将80例脑梗死后轻度认知障碍的患者随机分为研究组(40例)和对照组(40例)。两组均予基础治疗,研究组在基础治疗外另予醒脑开窍针刺法联合补肾益髓汤治疗。比较两组临床疗效,观察两组治疗前后简易精神状态检查表(mini-mental state examination,MMSE)、蒙特利尔认知评估(Montreal cognitive assessment,MoCA)和Rivermead行为记忆测验(Rivermead behavioural memory test,RBMT)的评分变化,观察两组治疗前后连线测验-B(trail making test-B,TMT-B)结果、血清淀粉样蛋白A(serum amyloid A,SAA)和β-淀粉样蛋白(amyloid β-protein,Aβ)水平以及脑微循环指标(颈总动脉的平均血流量、最大血流速度、最小血流速度、临界压力、脉搏速度、特性阻抗、外周阻力和动态阻力)的变化。结果 研究组总有效率高于对照组(P<0.05)。治疗后,两组MMSE、MoCA和RBMT评分均高于同组治疗前(P<0.05),且研究组上述评分均高于对照组(P<0.05)。治疗后,两组TMT-B结果以及SAA和Aβ水平均优于同组治疗前(P<0.05),且研究组上述指标优于对照组(P<0.05)。治疗后,两组脑微循环指标均较治疗前改善(P<0.05),且研究组优于对照组(P<0.05)。结论 在基础治疗以上,采用醒脑开窍针刺法联合补肾益髓汤治疗脑梗死后轻度认知障碍可提高临床疗效,能进一步改善患者认知功能,并调节SAA和Aβ水平。

《儒行》篇:戴仁而行,抱义而处——孔子为儒者赋予价值规定的经学文本解读

在早期儒者转型的时点上,孔子致力于“君子儒”的建构,有意把儒者群体带出“小人儒”的困境。《儒行》篇是孔子第一次自觉而系统地为整个阶层的职业行为制定标准,率先为儒者立范立则,赋予仁义价值规定。“待聘”“待问”“待举”“待取”意味着早期儒者群体已经做好心理和行动的积极准备,耐心等候进用。儒者执持操行,面对货财乐好之利却不亏损道义。有道义充塞于心,具有强大的意志力和自制力,儒者无所畏惧,勇往直前,即便献出生命也在所不惜。儒者为道义而生,为道义而死。“往者不悔,来者不豫”则强调儒者须有抓住当下、直击本体的能力和品格。以忠信为甲胄,以礼义为干橹,戴仁而行,抱义而处,则是早期儒者队伍自觉告别“小人儒”的庄重宣言,足见风骨气节。“不临深而为高”则要求儒者不与世沉浮而建构独立的精神人格。

邢窑六世纪晚期制瓷原料的同位素和微量元素分析

白瓷的出现是我国陶瓷历史上较为重要的技术突破,白瓷的烧制成功为后世青花瓷、彩绘瓷的繁荣奠定了重要基础,被誉为中国古陶瓷工艺发展史中的“第四里程碑”。因此,关于白瓷起源的问题就成为考古界和科技考古界关注的重要学术问题,而邢窑2012年考古发掘出土的北朝晚期窑炉和器物遗存自然成为研究白瓷起源的重要实物资料。本研究利用电感耦合等离子体质谱(ICP-MS)和热电离质谱(TIMS)分析技术,对河北内丘城关服务楼窑址出土的北朝晚期至隋朝初期的早期瓷器样品胎釉原料进行分析,为邢窑早期瓷业的发展演变提供科学依据。结果表明邢窑早期瓷胎的微量元素统计模式明显可以分为两类,说明邢窑早期制瓷存在两种不同的胎料来源。邢窑陶工在开发早期白瓷这一新品种的过程中有意识地选择了一种有别于青瓷的更为优质的原料制胎,这种胎料中与锆石、锐钛矿等杂质赋存密切相关的V、Cr、Ni、Nb、Ta、Zr和Hf等微量元素含量普遍小于青瓷胎。锶(Sr)同位素混合模式分析表明,邢窑早期的大部分样品不符合草木灰配以胎料的制釉方式,应该是采用了草木灰混合其他制釉黏土。同时,早期白瓷釉与青瓷釉的锶同位素特征存在一定差异,说明在制作过程中邢窑陶工为了提高釉面白度对制釉工艺也进行了变革,体现了为创烧早期白瓷而做出的努力。这些结果为科学认知邢窑六世纪晚期制瓷原料的特点和来源提供依据,同时也为破解白瓷起源提供新的科技支撑。

中华感兴美学的元美学意义与当代创新

中华感兴美学是以“兴”为枢机,比兴和感兴交织互动、双向拓展、融会贯通的美学理论。“兴”是中华古典艺术和美学最重要的元范畴,感兴美学则是最具中华民族特色和精神气质的元美学。与西方“元美学”术语不同,中华感兴美学的元美学意义表现在“:兴”是中华古典艺术和美学的元范畴、“兴”在中国古典美学史上的地位堪比西方的“逻各斯”、感兴美学是中国古典美学的“开山之纲领”、感兴美学历来被誉为“诗学之正源,法度之准则”、感兴美学凝聚了中华美学独特的精神气质。开展感兴美学的元美学探源性研究和创新性研究,对于深化中国美学史和中华美学精神研究具有重要意义。应当在新的历史条件下复兴和创新中华感兴美学,使之全面进入当代美学、文艺学和艺术学理论。

孟子“乐”与“射”的双重隐喻

孟子乐喻中,金声玉振并非完全对应于奏乐的始终;“终条理”亦可理解为“已条理”“既条理”。“金石以动之”,如同战场之号令,金石之音皆可看作是乐曲的起始,起到节度各音的作用。从我国古代乐器实际演奏过程考虑,后世所理解的“以玉声振扬金声”的观点并不恰当;古人始终在尽量避免镈钟类乐器产生混响,又何需玉音振扬金声。赵岐、俞樾等所认为的“振扬玉音终始如一”、以玉声振扬金声,并非乐师演奏时所追求的和谐之境,仅为经师诠释经典时的意义建构。由于金石的稳定性,孟子乐喻还涉及金石之品质,为众音之准则。金声玉振不仅隐喻孔子兼具圣人之全德,还隐喻孔子为后世之法则。孟子乐、射二喻中,不应将智、圣二分看待。《五行》篇与孟子的不同处,还在于孟子以金玉喻始终条理,兼具圣智;而《五行》篇以金玉喻内外,又强调君子集大成,最终达到合内外的思想旨趣。

新工业诗歌:“新感性”及“西部”多维审美——兼谈马行的诗歌

随着20世纪末“打工诗”的盛行,工业诗歌的语言在市场化、消费化及数字时代发展中不断被标准化、同质化,断开了与人类、世界的密切关联。马行不再囿于集体抒情或个体视角,在勘探队员、诗人的双重维度上,从人性、物性、神性的角度深入工业日常探讨当代“西部”书写所表现出来的多维审美意蕴。诗人感性中的莽苍广阔的荒野,折射出“新感性”的忧虑与省思,在新工业诗歌中反思工业技术的物化、工业中心化,展示了新工业诗歌的开拓性、创造性,从单一诗化的“感性”中重构“新感性”中物与人、自然与现实、工业与新工业的关系,以敏感、活跃及超越意志进行纯净、豁达的哲理观照,从而构筑新工业诗歌中感性与理性、自然与科技的“和美”关系,展现“新工业诗歌”多维审美中建构“西部”大地上诗意栖居可能。

岭南与长江中下游:跨区域贸易背景下的徽商活动与皖南古村落

本文通过整理黟县卢村的相关书信,探讨清代徽商活动对徽州村落社会的影响。从中可见,至迟从盛清时代开始,黟县的经济就与跨区域之贸易活动密切相关。岭南的广州及长江中下游之汉口、九江和大通等,都与僻野山乡的卢村发生了颇为密切的关联。尤其是在茶叶经营中,从茶叶生产到销售过程的诸多环节上皆充满了竞争,理性的商人根据汉口、广州的茶市行情,精心策划营销策略、拟定购销规模,以争取自身利益的最大化。而从频繁的茶叶贸易中获取的利润则源源不断地流入皖南,促进了徽州村落社会的发展。

特殊教育学校职业课程实施困境与纾解之道——基于陶行知特殊教育理论视角

当前我国特殊教育学校职业课程的实施困境主要表征为:特殊教育学校职业课程体系建设不足;特殊教育学校职业教育基础较为薄弱;特殊教育学校职业课程实施相对乏力等。基于陶行知特殊教育理论视角,各特殊教育学校应做到:构建专业化职业教育师资培养体系,夯实课程实施基础;改善职业课程实施内部条件,完善课程实施机制;以人为本,促进特殊教育职业课程体系建设;课程实施面向市场与就业,产教融合推进校企合作等。