排序方式: 共有63条查询结果,搜索用时 46 毫秒
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天山乌鲁木齐河源1号冰川面积变化对物质平衡计算的影响 总被引:4,自引:5,他引:4
应用天山乌鲁木齐河源1号冰川8期不同时期测绘的冰川地形图,结合冰川物质平衡的实测资料,研究了1号冰川的面积变化及其对物质平衡计算的影响.结果表明:自1962年以来,1号冰川面积处于持续的退缩状态.到2008年8月为止,1号冰川东、西支已经分别退缩了208.2m和110.5m,同时冰川面积退缩为1.645km2,比196... 相似文献
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吕梁山西麓中上新世的一套厚层红黏土层记录了吕梁山前盆地的演化和吕梁山新近纪的隆升。山前不同的构造部位,各异的古地貌特征导致红黏土的堆积特征差别较大,柳林复兴地区黏土层的下部常含有数层化石层和薄厚不等的砾石层。本文对复兴地区的红黏土进行了岩石磁学和磁性地层学研究,得出了复兴地区红黏土及所含砾石层和化石层的古地磁年龄,并通过野外沉积特征以及粒度等指标探讨了复兴地区红黏土的形成过程。岩石磁学结果表明,红黏土中特征剩磁的载体为磁铁矿和赤铁矿。古地磁和生物化石显示复兴剖面的年龄为7.1~2.6Ma。其中所含厚层砾石层的古地磁年龄约为5.2Ma。两层化石层的年龄分别为~6.8Ma和~7.1Ma。剖面野外沉积特征和粒度变化显示柳林复兴地区红黏土堆积初期有水流作用的参与。 相似文献
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黄陵背斜、秭归向斜是三峡地区构造地质研究热点之一,前人将其划归于秦岭造山带的组成部分,认为是东西向构造后期改造的结果;分布于此区的仙女山断裂是否穿越长江也是争论的焦点问题之一.这些问题的解决对澄清研究区地质灾害分布特征具有重要意义.笔者在前人研究的基础上,从沉积学、构造地质学角度,在大量野外地质研究工作的基础上,提出了新的看法:黄陵背斜、秭归向斜、当阳向斜、仙女山断裂同属统一的构造体系,其形成和演化与中国东西部构造格局的变迁一致,黄陵背斜具有断层相关褶皱的特点,秭归向斜具有前陆挠曲型盆地构造属性;仙女山断裂形成之初具有传递断层的属性,后期又经历了引张、挤压演化过程,不存在跨越长江向北延伸的问题;受秭归向斜沉降幅度以及东西向构造与南北向构造复合影响,在研究区形成3个滑坡聚集区,分别为贾家店滑坡聚集区、八字门向家店滑坡聚集区、兴山县城附近滑坡聚集区. 相似文献
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新疆乌鲁木齐地区积雪深度演变规律及对气候变化的响应 总被引:2,自引:0,他引:2
积雪深度D是水文模型和气象预测中的重要参数之一.基于新疆乌鲁木齐站1961-2013年积雪深度D及气象资料,分析了积雪起止日期、持续期特征和D的时间变化规律,并对比了不同模型对于D过程变化的适配效果.此外,对最大积雪深度Dmax进行了趋势检验,并简要分析了气象要素对D和Dmax的影响.结果表明:乌鲁木齐积雪的持续期在73~207 d范围变化,平均持续141 d,积雪开始日期和终止日均呈推迟趋势,积雪持续期呈增加趋势,但其趋势均不显著.可将积雪年内的D变化类型分为多峰缓变型、右偏型、尖峰型以及平峰型4种,分别用不同模型适配后发现整体上模拟效果较好的是Gaussian函数.在1961-2013年53 a期间的Dmax不具有自相似结构,但有显著上升趋势.气温尤其是最低气温与的D相关性最好,冷季降水总量与Dmax有的正相关关系,表明气温和同时期降水与积雪变化关系密切.春季迅速升温过程及一定的累积积雪深度可能令融雪型洪水爆发,其对应的年型为尖峰型和平峰型. 相似文献
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Indicating the Trophic State of Running Waters by Using TIM (Trophic Index of Macrophytes) – Exemplary Implementation of a New Index in the River Inninger Bach The river Inninger Bach represents the outflow of the lake Wörthsee (Bavaria). The mean pH of the calcareous river has a value of ca. 8 during the vegetation period, the mean conductivity is about 350 to 400 μS/cm. The macrophyte vegetation of the river course was mapped and the nutrient concentrations of both the water body and the sediment were measured. In every mapping section the Trophic Index of Macrophytes (TIM) was calculated. By cluster analysis the mapping sections were grouped into three zones which differed in macrophyte vegetation. These differences are not associated with varying nutrient concentrations but are mainly due to differences in the degree of shading. In spite of the characterisation of the lake Wörthsee as oligo‐mesotrophic the river Inninger Bach, which represents the outflow of the lake Wörthsee, is classified as meso‐eutrophic by the Trophic Index of Macrophytes TIM. The increased trophic state of the river compared to the lake is caused by the river Krebsbach, a small tributary flowing into the river Inninger Bach only a short stretch downstream of its outflow of the lake Wörthsee. The river Krebsbach shows a total phosphorus concentration of about 56 μg/L P. The input of diaspores of submerged macrophytes both from the oligo‐mesotrophic lake Wörthsee and the eutrophic river Krebsbach leads to a submerged vegetation comprising species with different optima in regard to the trophic situation. This is one of the main reasons why many values of the TIM have to be labeled as “not sure”. 相似文献
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Rapid source inversions of the 2023 SE Türkiye earthquakes with teleseismic and strong-motion data
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Chenyu Xu Yong Zhang Sibo Hua Xu Zhang Lisheng Xu Yuntai Chen Tuncay Taymaz 《地震科学(英文版)》2023,36(4):316-327
We conducted rapid inversions of rupture process for the 2023 earthquake doublet occurred in SE Türkiye, the first with a magnitude of MW7.8 and the second with a magnitude of MW7.6, using teleseismic and strong-motion data. The teleseismic rupture models of the both events were obtained approximately 88 and 55 minutes after their occurrences, respectively. The rupture models indicated that the first event was an asymmetric bilateral event with ruptures mainly propagating t... 相似文献
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在凡纳滨对虾((Litopenaeus vannamei)育苗水体中引入不同浓度的牟氏角毛藻(Chaetoceros muelleri),检测主要水质因子,测定凡纳滨对虾对主要环境因子抗逆性,研究微藻对水质和凡纳滨对虾抗逆性的影响。结果表明,不同浓度牟氏角毛藻可明显改善对虾育苗水体的水质,提高幼虾的抗逆性(P<0.05)。牟氏角毛藻浓度为0.6×108~1×108/L时,实验组氨氮含量比对照组降低37.29%~46.32%,亚硝酸氮含量降低48.65%~62.70%,化学耗氧量(COD)值降低9.99%~12.19%;实验组育苗成活率达78.7%~84.0%,对照组育苗成活率46.0%;在氨氮、亚硝酸盐氮、硫化氢、甲醛抗逆性实验中,实验组幼虾成活率分别为75%~80%、75%、75%~85%、65%~70%,均显著高于对照组(P<0.05)。 相似文献