Leader–member exchange,organizational identification,and knowledge hiding: The moderating role of relative leader–member exchange

In this article, we sought to identify a new interpersonal antecedent of knowledge hiding, namely, leader–member exchange (LMX). Drawing on the group engagement model (an extension of social identity theory within the group/organization context), we built a theoretical model linking LMX and knowledge hiding. This model focuses on the mediating role of organizational identification and the moderating role of relative LMX in influencing the mediation. Using two time‐lagged studies (Study 1: n = 317; Study 2: n = 248) conducted in China, we examined our research model. Study 1 provided support for the proposed hypotheses for evasive hiding and playing dumb but not for rationalized hiding. Study 2 replicated and extended our findings. Results revealed that (a) LMX was negatively related to evasive hiding and playing dumb but not to rationalized hiding; (b) organizational identification mediated the influence of LMX on evasive hiding and playing dumb but not on rationalized hiding; and (c) relative LMX not only moderated the relationship between LMX and organizational identification but also reinforced the indirect effect of LMX on evasive hiding and playing dumb but not on rationalized hiding (via organizational identification). The implications, limitations, and future research directions are also discussed.     

Methane Emissions and Production Potentials of Forest Swamp Wetlands in the Eastern Great Xing’an Mountains, Northeast China

Measurements of methane flux at a few inundated sites in China have been extrapolated to obtain estimates on a national scale. To enable those national estimates to be refined and to compare flux from geographically separated sites comprising the same wetland types, we used a closed chamber method to measure methane flux in uninundated Betula platyphylla—and Larix gmelinii—dominated peatlands in the Northeast China. Our measurements were taken from both vegetated and bare soil surfaces, and we compared flux with environmental measures including vegetation biomass, soil temperature and soil characteristics. We found that methane flux was low, and that there were no significant differences between wetland types, indicating that environmental influences were dominant. We found that flux was positively correlated to temperature in the surface layers of the soil, the above-ground biomass of the shrub and herb layers, total soil carbon and total soil nitrogen; and we suggest that emissions may be due to anaerobic microcosms in the surface layers. The methane production potentials of the soils were low and similar between both sites but inconsistent with the differences between fluxes, and inconsistent with production potentials and fluxes reported from the same wetland types elsewhere, indicating that there were subtle environmental differences between wetlands classed as being of the same type. Differences between fluxes in vegetated chambers with bare soil chambers were insignificant, indicating that no methane emission through aerenchyma occurred at our sites. We concluded that wetland type was not an accurate predictor of methane flux.     

Manganese-catalyzed cross-coupling of primary alcohols with biomass-derived ethanol for upgrading to linear alcohols under solvent-free conditions

Environmental Chemistry Letters - Bioethanol is a major raw chemical produced in large quantities by the fermentation of sugar-containing crops and lignocellulosic materials. As a consequence,...     

咸阳市温室气体排放的动态分析及等级评估

通过采用《2006年IPCC国家温室气体清单指南》和中国《省级温室气体编制指南》推荐的方法,分析了咸阳市温室气体排放的动态变化,并提出基于全球标准的温室气体排放等级评价方法,对咸阳市温室气体进行了排放等级评估.结果表明:1995—2011年,咸阳市温室气体排放量从1253.21×104t上升为5531.06×104t,年均增高9.72%,呈快速上升趋势.工业(年均增高21.34%)为增幅最高的部门,其次依次为能源(9.62%)、废弃物(7.90%)、农业(2.45%).从温室气体构成看,能源占84.73%~91.81%,工业占1.46%~8.55%,农业占3.11%~9.32%,林业碳减排占-0.53%~-2.36%,废弃物处理占1.31%~8.39%.由此可见,咸阳市温室气体排放增长的主要原因是能源消费的增加以及工业生产的大幅增长.万元GDP温室气体排放量波动下降,年均降低4.53%;人均、单位面积温室气体排放量和温室气体排放指数快速升高,年均增幅分别达9.31%、9.72%和9.48%.16年间,咸阳市温室气体排放等级从较低(Ⅰc)持续升高至中上等级(Ⅱc),已高出应对全球气候变暖目标(Ⅰb)4个亚级,温室气体减排工作刻不容缓.     

钢厂石灰窑烟气CO_2的回收利用

简述了某钢厂将石灰窑烟气中的CO2回收,制成食品级CO2的工艺概况及其综合利用效益,为工业尾气CO2资源化循环利用提供了示范。     

溴代阻燃剂在中国川藏地区的污染和分布特征

利用气质联用仪(GC-NCI-MS)对中国川藏地区饮用水、表土和青稞样品中PBDEs(包括十溴联苯醚在内)和TBBPA的含量进行了检测,分析了PBDE同系物的分布模式,比较研究了不同区域的溴系阻燃剂(BFRs)的污染水平、可能来源和环境影响因素.结果显示,西藏地区饮用水中均未检出PBDEs和TBBPA.表土样品中∑13PBDEs的含量范围为0.87~10.56 ng·kg-1(以干重计),PBDE主要同系物为BDE-15、209、47和99(所有样品中100%检出),分别占∑13PBDE含量的39.0%、16.5%、10.5%和10.5%.另外,研究发现,土壤中∑13PBDEs与TBBPA的含量显著相关,暗示了它们相似的空间分布,且PBDEs和TBBPA均与TOC值显著相关,PBDEs和TBBPA与海拔高度呈显著线性关系.这表明川藏地区土壤中PBDEs和TBBPA的污染为同一来源,且其含量不仅受TOC值和海拔高度的影响,也可能受与PBDE和TBBPA有关的大气传输、稀释或吸附、沉降多种因素影响.在偏远地区的农作物青稞中检测到了PBDEs和TBBPA,可能是通过大气沉降到农作物表面,被生物富集和吸收.青稞为该地区居民主食的原料,尽管PBDEs和TBBPA的含量非常低,但可能对当地居民健康产生影响.     

冰封期呼伦湖浮游藻类群落结构及其与水环境因子的关系

为探讨冰封状态下呼伦湖的水生态系统演变过程,2015年12月—2016年3月环湖设置6个采样点进行浮游藻类及湖水水质的监测。浮游藻类以绿藻门Chlorophyta种类最多(52.5%),其次为硅藻门Bacillariophyta(29.8%),蓝藻门Cyanophyta(10.5%)。物种丰富度和3种生物多样性指数(Shannon-Wiener多样性指数、Margalef丰富度指数、Pielou均匀度指数)从12月至次年3月呈下降趋势。浮游藻类丰度自12月至次年3月呈现上升趋势。典范对应分析(CCA)排序结果表明:NH₃-N、TN、TP、电导率、DO、BOD₅、CODMn和pH是影响呼伦湖浮游藻类群落结构特征的主要环境因子,其中,NH₃-N、TN和TP分别对硅藻门、绿藻门和蓝藻门的影响较大。     

复合混凝剂的制备及活性染料的去除

以马铃薯淀粉、丙烯酰胺（AM）和二甲基二烯丙基氯化铵（DADMAC）为原料进行接枝反应,将接枝产物（TSI）与聚合氯化铝铁（PAFC）复配,制得新型复合混凝剂PAFC-TS1。优化了复合混凝剂制备的工艺条件。研究结果表明,复合混凝剂PAFC-TS1的优选制备条件为：OH^-浓度与铝铁总浓度的比（r）为0.5,铝铁总浓度与TS1的质量浓度比（R_m）为0.5 mol/g,铝铁摩尔比9∶1。在此条件下处理质量浓度为100 mg/L的活性染料废水,当混凝剂投加量为24 mL/L时,染料去除率可达97%以上。相同条件下,使用PAFC-TS1比单独使用PAFC或PAFC-PAM的染料去除率更高。     

有机磷降解酶的固定化及其工业化应用初探

采用一种新型的酶固定化方法,在大孔微球中对有机磷降解酶（OPHC2）固定化,制备固相载体化的交联酶聚集体固定化酶。对具有实际应用意义的参数：热稳定性、牢固度和连续反应批次进行了重点研究。结果表明,有机磷降解酶固定化酶的半衰期在70℃时比游离酶提高了2.1倍。固定化酶分别在37℃的摇床中经14 h高速振荡,以及在pH 8、37℃条件下循环反应49个批次降解甲基对硫磷后,均未发现固定化酶酶活力下降。在37℃,有机磷降解酶固定化酶柱以每小时3倍柱床体积的速率对甲基对硫磷农药乳油的稀释液（甲基对硫磷含量为216 mg/L）进行降解处理,系统连续工作156 h,甲基对硫磷的降解率保持在98.4%～99.9%。