基于多种培养基和不同培养温度的马里亚纳海沟异养细菌多样性分析     

王震  朱祥杰  苑志欣  郝建华  郑兰红 《海洋湖沼通报》2021,(1):91-100

马里亚纳海沟具有低温、高压、永久黑暗以及营养匮乏等深海环境特征,其中的细菌多样性对深海环境具有极为重要的作用.为研究马里亚纳海沟海水中异养细菌的物种多样性,采用多种培养基、不同培养温度同步筛选,单菌落16S rRNA基因序列鉴定,邻近法系统发育树构建分析等方法,对25个海水样品进行异养细菌多样性分析.共获得细菌531株...  相似文献   

东莞市交通路网格局对城市空间扩张影响研究   总被引：2，自引：0，他引：2  

冯志新  陈颖彪  千庆兰  王帅帅 《地球信息科学学报》2014,(1):79-86

城市化进程中,交通路网格局的发展与土地利用变化有着密切关系,交通系统的发展引起城市空间形态、土地利用开发、土地利用价格和用地布局特征的变化,反之,土地利用变化也引起了交通路网格局、路网密度的改变。本文以东莞市为例,对其交通路网密度与新增城市用地变化强度作了定量分析。根据TM遥感影像提取2001、2005和2009年3期的城市用地,采用核密度估算(KDE)新增城市用地变化强度,探讨区域内交通路网格局与新增城市用地变化强度的关系。结果表明,在2001-2005年间,路网格局变化较大,新增道路类型主要为高速路,新增城市用地总量较大、扩张速度快,特别是交通路网密度大的边缘区域。在2005-2009年间,随着路网发育不断成熟,路网密度内部差异减少,新增道路类型主要为县乡道路,新增城市用地速度明显放缓。经相关系数显著性检验后表明:2001-2009年间,在置信度为95%时,东莞市道路网密度、加权密度(x)与新增城市用地核密度(y)的相关系数Rxy均大于0.1946,证明东莞市道路网密度、加权密度与新增城市用地核密度高度相关。  相似文献   

Flood disasters and social resilience during the decline of the Qing Dynasty: Case studies of 1823 and 1849     

Zhixin Hao  Danyang Xiong  Jingyun Zheng 《水文研究》2021,35(7):e14295

Based on historical records and crop harvest scores extracted from historical documents, this study reconstructed the spatial–temporal distribution and severities of floods in the Yangtze-Huai River valley (YHRV) in 1823 and 1849. We also summarized the effects of the floods on society and identified government measures taken to cope with the floods in the context of the economic recession in the period of 1801–1850. The 1823 flood, which was caused by the heavy precipitation of the Meiyu period and typhoons, severely affected areas in the lower reaches of the Yangtze River. Meanwhile, the 1849 flood, triggered by long-term, high-intensity Meiyu precipitation in the middle and lower reaches of the Yangtze River, mainly affected areas along the Yangtze River. The 1849 disaster was more serious than the one in 1823. In the lower reaches of the Yangtze River, the 1849 flood caused the worst agricultural failure of the period 1730–1852. To deal with the disasters, the Qing government took relief measures, such as exempting taxes in the affected areas, distributing grain stored in warehouses, and transferring grain to severely afflicted areas. These relief measures were supplemented by auxiliary measures, such as exempting commodity taxes on grain shipped to disaster areas and punishing officials who failed to provide adequate disaster relief. The flood disasters disrupted the water system of the Grand Canal and forced the Qing government to transport Cao rice by sea beginning in 1826. This laid the groundwork for the rise of coastal shipping in modern China. With the economic recession of the 19th century, Chinese society was not as resilient to floods as it was in the 18th century. Compared to droughts, floods are more difficult to deal with and pose greater threats to infrastructure and normal life and work in the cities.  相似文献   

粉喷桩加固软土地基的认识   总被引：2，自引：0，他引：2  

杨顺安  刘志欣  张迎春  蒙庆辉 《地质科技情报》1999,18(3):75-78

通过对广州－佛山高速公路扩建工程及北京－珠海高速公路土地基处理工程的研究,分析了了喷粉桩,土应力转化及相互作用,进而对桩的轴向应力,复合基沉降,作用机理进行了研究,并提出了用粉喷桩复合地基加固软土地基的几点看法。  相似文献   

OMNIPHONE 54°三分量检波器分量之间串扰的测试     

贾志新 《世界地质》1999,(1)

针对目前国内外５４°三分量检波器串扰测试方法存在的许多问题,着重介绍了三分量检波器测试方法。该方法在不降低精度的前提下,可大大简化电路,节省费用。  相似文献   

塔克拉玛干沙漠腹地晴天与沙尘暴天气大气边界层对比分析     

张建涛  王敏仲  何清  王延慧  潘红林  张志新 《沙漠与绿洲气象(新疆气象)》2024,18(1):50-58

根据2017、2019年7月塔克拉玛干沙漠腹地GPS探空和地面观测数据,利用位温廓线法等方法,对比分析了沙漠腹地夏季晴天和沙尘暴天气大气边界层结构变化特征。结果表明：晴天和沙尘暴天气大气边界层结构特征显著不同。晴天大气边界层各气象要素垂直分布较为均一,白天对流边界层深厚,高度接近5 km,夜间稳定边界层一般在500 m左右。沙尘暴天气边界层内位温和比湿垂直变化较小,风速较大,可达24.0 m/s,其白天对流边界层在1.5 km左右,夜间稳定边界层在1 km左右。晴天辐射强烈,地表升温迅速,湍流旺盛,是形成晴天深厚对流边界层的主要因素。大尺度天气系统冷平流的动力条件,以及云和沙尘减弱了到达地表的辐射强度是形成沙尘暴天气独特的大气边界层结构的主要因素。  相似文献   

渭河盆地地裂缝发育基本特征   总被引：3，自引：0，他引：3  

陈志新  袁志辉  彭建兵  李喜安  毛少力  惠旭辉 《工程地质学报》2007,15(4):441-447

渭河盆地由于其特殊的地质环境,是地裂缝发育较多的地区。本文在渭河盆地地裂缝详细调查的基础上,简要论述了地裂缝的分布概况,详细研究了渭河盆地地裂缝的发育基本特征,并初步探讨了地裂缝的成因。渭河盆地196条地裂缝大都密集分布在断层近侧,与断层走向有明显的一致性和相关性。地裂缝基本特征主要是形态特征和空间分布。地裂缝平面形态有直线、S型和锯齿状;剖面形态为上宽下窄,并逐渐消失;倾角较陡。地裂缝空间分布上有方向性、开启性和网络性。渭河盆地地裂缝主要是构造地裂缝,受构造断裂控制;地下水、地表水、采空和黄土湿陷性只是诱导因素。  相似文献   

Estimation of agricultural greenhouse gases emission in interprovincial regions of China during 1996–2014     

Li  Nan  Shang  Liwei  Yu  Zhixin  Jiang  Yuqing 《Natural Hazards》2020,100(3):1037-1058

Natural Hazards - Agriculture is an important component of national economy in China, and agricultural production is also an important source of greenhouse gas emission. Based on the methods of...  相似文献   

An Overview on Changes of Dry/Wet Pattern in China in Decadal to Centennial Warm and Cold Periods During the Past Millennium     

Zhixin Hao  Maowei Wu  Xuezhen Zhang  Yang Liu  Jingyun Zheng 《地球科学进展》2020,35(1):18-25

Revealing the multi-scale variation characteristics of the drought/flood patterns for the past millennium has been a hot spot in climate change research in recent years. It has significance for understanding and predicting the temporal and spatial differences of precipitation changes in the context of future climate warming. Based on publications on the peer-reviewed journals, here, we summarized and compared the combinations between cold/warm periods and dry/wet spatial patterns at multi-scales in China over the past millennium. The main conclusions are: although there are differences in China's dry/wet patterns in different cold and warm periods for the past millennium, the ensemble mean shows that the dry/wet patterns in eastern China in decadal or centennial warm periods are approximately "dry (South China)-wet (middle and lower reaches of the Yangtze River)-dry (Huanghuai Area)" from south to north, while in the relatively cold periods it mainly shows a "wet in east and dry in west" pattern. The climate changes from cold to warm usually lead to a drying trend in the Huanghuai Area, and a wetting trend in the Jiangnan area (especially the Yangtze River basin in Hunan and Jiangxi provinces). This shows that the "flood in south and drought in north" pattern in eastern China since the 1970s under the background of global warming may be a re-occurrence of the matching characteristics of cold/warm climate and dry/wet patterns in China for the past millennium. However, from the perspective of the longer-scale cold and warm stages, the dry/wet pattern in China tend to be "dry in the arid and semi-arid areas in western China; wet in southwestern, northern, and northeastern China; and dry in southeastern China" in the Medieval Climate Anomaly, and an opposite pattern shows in the Little Ice Age. It suggests that there are still uncertainties in the current climate reconstructions, and it also shows that the mechanism of dry/wet pattern responding to multi-scale temperature fluctuations might be extremely complicated.  相似文献   

新疆蛇绿岩时空分布特征及对增生造山过程的制约     

赵同阳  朱志新 《新疆地质》2021,(1):21-29

聚焦新疆区内集中出露的61处蛇绿岩,据其物质组成、构造属性、形成时代、空间分布等特征,将其划分为14条蛇绿混杂岩带,其中多处发育洋岛海山、洋内弧等大洋岩石圈岩石组合,并以塔里木-敦煌地块为界,提出以北属古亚洲洋构造域、以南属特提斯洋构造域.结合俯冲增生造山过程中不同阶段的岩石学记录,确认古亚洲洋形成于新元古代末期至晚石...  相似文献