南北疆区域经济差异化三维生态足迹自然资本利用的时空演变

如何刻画自然资源消费在区域间的流转机制及其对生态的影响,是测度区域可持续发展的难点。采用改进后的三维生态足迹模型并引入存量流量利用比和资本流量占用率,对2003—2018年新疆区域三维生态足迹进行核算,并分别测度新疆各地州市自然资本利用的程度,聚焦南北疆地区自然资本利用的差异性,利用偏最小二乘法(PLS)找出影响生态足迹变化的动因,最后结合基尼系数及差异系数量化南北疆经济差异程度,从自然和经济视角探究南北疆可持续发展态势与差异。结果表明:①2003—2018年新疆人均生态足迹持续增长,增长幅度为119.94%,人均生态承载力基本保持在1.7 hm~2左右,流量资本占用强度不断增加,生态赤字问题愈发严重。②研究期内,南北疆地区生态足迹的增长幅度和速度存在明显空间差异,呈现"北高快,南低慢"的态势。各地州市生态赤字情况呈现不同程度的增长趋势,高值区为北疆的克拉玛依市及天山北坡经济带。③第一产业增加值对生态足迹正向驱动作用最为显著,第三产业增加值对生态足迹起到逆向驱动作用。④2003—2018年间,南北疆地区基尼系数维持在0.4—0.5之间,处于中警警度水平,南北疆区域经济差异系数变化波动不大,北疆区域经济差异系数明显高于南疆区域。     

High expression of NEK2 promotes lung cancer progression and drug resistance and is regulated by mutant EGFR

Molecular and Cellular Biochemistry - An increasing amount of research showed that endothelial cells (ECs) play crucial role in vascular disorders such as atherosclerosis (AS). LncRNA OIP5-AS1 and...     

黑河中游湿地景观破碎化过程及其驱动力分析

在遥感和GIS技术支持下,基于1975-2010年长时间序列遥感影像,选取斑块密度指数(PD)、景观内部生境面积指数(IA)、斑块平均面积指数(MPS)、斑块形状破碎化指数(FS1、FS2)等具有典型生态意义的景观指数模型,系统分析了黑河中游湿地景观的破碎化过程,并结合灰色关联分析、主成分分析等方法,探讨了影响研究区湿地景观破碎化过程的各驱动因子.结果表明:近35年来,研究区湿地景观破碎化主要表现为斑块平均面积的萎缩,斑块密度的上升以及斑块形状破碎化指数的增大.整个研究时段内,研究区湿地斑块平均面积减少了48.95hm2,斑块密度的上升0.006个/hm2;导致黑河中游湿地景观破碎化发生和发展的驱动力包含自然和人文两个方面.自然因子对湿地景观破碎化进程的影响则主要体现在气温和降水上,而且气温对湿地景观破碎化进程的影响程度明显大于降水.但在1975-2010年间的这一较小时间尺度上,人类活动对湿地景观破碎化的贡献率明显高于自然因子,人类活动能力的增强以及影响范围的不断扩大是引发黑河中游湿地景观破碎化的主因.     

低温下抗氧化酶活性与冬油菜根细胞结冰关系的初步研究

以4个抗寒性不同的油菜品种的根为材料,于低温试验箱内连续降温处理(4℃/24 h,0℃/24 h,-3℃/24 h,-6℃/24 h,-9℃/24 h,-15℃/24 h,-21℃/24 h),检测其抗氧化酶(POD、CAT)活性,并结合POD同工酶电泳和冷冻前后幼苗的形态变化特征,探讨油菜根部抗氧化酶活性变化与细胞冰冻状态间的相关性以及油菜根的抗冻机理.结果显示:(1)弱抗寒性油菜品种(‘临油7号’和Vision)在低温冷冻后,叶面出现大量水渍,之后叶片萎缩直至焦枯,根部出现水渍后软化直至干枯死亡;强抗寒性品种(‘陇油6号’和‘陇油8号’)在冷冻后不产生水渍或水渍极少,其根在冻后损伤也较轻微.(2)在连续冷冻条件下,弱抗寒性油菜根部POD和CAT活性在降温初期有较大幅度的变化,之后就保持恒定,说明根部细胞已完全结冰;而强抗寒性油菜根部POD和CAT活性在降温初期变化较小,后期持续大幅增加,表明根部细胞仍保持溶液状态;POD同工酶分析也反映出类似的变化规律.研究表明,低温下冬油菜根部抗氧化酶活性变化和细胞冰冻状态之间存在相关性;细胞结冰通常会给植物造成致死性伤害,强抗寒油菜品种能安全越冬的关键就是能通过某种机制避免细胞内结冰,其结冰温度越低,抗寒性越强.     

Effect of Xanthan Gum on the Freeze-Thaw Stability of Wheat Gluten

Food Biophysics - The effect of xanthan gum on the freeze-thaw stability of wheat gluten was evaluated during a 60-day storage period at −18 °C with thawing every...     

Expanded Expression Landscape and Prioritization of Circular RNAs in Mammals

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Community structure,distribution pattern,and influencing factors of soil Archaea in the construction area of a large-scale photovoltaic power station

International Microbiology - The photovoltaic power station in Qinghai has been built for 8 years; however, its impact on the regional soil ecological environment has not been studied in...     

Spatiotemporal Distribution,Sources, and Photobleaching Imprint of Dissolved Organic Matter in the Yangtze Estuary and Its Adjacent Sea Using Fluorescence and Parallel Factor Analysis

To investigate the seasonal and interannual dynamics of dissolved organic matter (DOM) in the Yangtze Estuary, surface and bottom water samples in the Yangtze Estuary and its adjacent sea were collected and characterized using fluorescence excitation-emission matrices (EEMs) and parallel factor analysis (PARAFAC) in both dry and wet seasons in 2012 and 2013. Two protein-like components and three humic-like components were identified. Three humic-like components decreased linearly with increasing salinity (r>0.90, p<0.001), suggesting their distribution could primarily be controlled by physical mixing. By contrast, two protein-like components fell below the theoretical mixing line, largely due to microbial degradation and removal during mixing. Higher concentrations of humic-like components found in 2012 could be attributed to higher freshwater discharge relative to 2013. There was a lack of systematic patterns for three humic-like components between seasons and years, probably due to variations of other factors such as sources and characteristics. Highest concentrations of fluorescent components, observed in estuarine turbidity maximum (ETM) region, could be attributed to sediment resuspension and subsequent release of DOM, supported by higher concentrations of fluorescent components in bottom water than in surface water at two stations where sediments probably resuspended. Meanwhile, photobleaching could be reflected from the changes in the ratios between fluorescence intensity (F_max) of humic-like components and chromophoric DOM (CDOM) absorption coefficient (a355) along the salinity gradient. This study demonstrates the abundance and composition of DOM in estuaries are controlled not only by hydrological conditions, but also by its sources, characteristics and related estuarine biogeochemical processes.