枣乡情思

九月的家乡,九月的山野,都像被红葡萄酒灌醉了,到处都淌着甜,流着蜜,那一片一片的枣园都沉浸在馨香之中,每一颗枣树上都挂满了红嘟嘟的枣儿,随手摘一颗放进嘴里,那甜就一直流到心里去。 该收获的季节,枣乡的景色真诱人。 望着漫山遍野的红枣,我禁不住诗兴大发。红枣,这枣乡的相思豆,曾在我心中刻下深深的记忆,那一个个甜甜的故事又在我心灵的屏幕上历历再现。 … … 那年秋天,也是枣儿成熟的季节,我们登上石板路走向我们的枣园,你靠在一棵枣树上,双手轻轻地揉抚着你那又长又黑的发辫,不时给我一个含羞的微笑,一个温柔的眼神,那…     

萨拉乌苏河流域萨拉乌苏组砂丘砂沉积特征

The Salawusu Formation of Milanggouwan section in Salawusu River Valley includes 7 layers of paleo-mobile dune sands, and 4 layers of paleo-fixed and semi-fixed dune sands. Their structures have been observed and their grain size, surface textural features and several main chemical elements have been analyzed. The results showed that： 1） Some of the aeolian structural characteristics of these dune sands are similar to that of the recent dune sands. 2） They are also similar to the recent dune sands in grain size components, and parameters of Mz,σ, Sk and Kg, as well as in several main chemical components. 3） The scattergrams of Mz-σ and SiO2-Al2O3＋TOFE and the probability curves of grain size showed that these paleo-dune sands are different from paleosols and fluvio-lacustrine facies, but are consistency with recent dune sands. 4） Quartz sands have well roundness and surface textural features such as dish-shaped pits, crescent-shaped pits, pockmarked pits, upturned cleavage plates, siliceous precipitates and siliceous crevasses, indicating that they had been carried for a long time by the wind. As the 11 layers of paleo-dune sands possess the aeolian characteristics in structure, grain size, surface textural features and chemical elements, the origin of their formation should be attributed to eolation.     

冷泉活动区气泡羽状流数值模型研究

羽状流对天然气水合物的识别起到了间接指示作用,为研究冷泉活动区气泡羽状流产生的地震响应,需建立符合实际羽状流特征的模型。为此,参考实际羽状流赋存状态,结合含气泡水体特征,在已建立模型基础上,从羽状流气泡的垂直运移规律、分布特点及羽状流外观特征上对模型进行了改进,先后获得3个羽状流模型,最后的模型Ⅲ更接近实际羽状流赋存特征。通过与实际羽状流的对比,讨论分析了模型Ⅲ的合理性,并得出结论：所建模型体现了实际羽状流气泡的本质特征,并包含了更为复杂的气泡含量变化,可用于进一步深入研究羽状流地震响应特征,也为气泡羽状流的地震识别及天然气水合物的相关研究提供了较好的数值模型。     

故乡的颜色(组诗)

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基于NDVI时间序列数据的江西省水稻种植制度变化研究

利用Savitzky-Golay滤波对覆盖江西省范围的SPOT VGT NDVI时间序列数据进行平滑处理的基础上,结合坡度数据,通过非监督分类的方法提取了江西省2000、2005和2010年水稻种植范围,并根据NDVI的年内动态变化,从水稻种植范围、水稻生长季起始时间、水稻复种指数和NDVI最大振幅等分析了江西省水稻种植和生长情况,探讨2000~2010年江西省水稻生产的变化。     

云南乌东德水电站施期料场中元古代热液白云岩研究

云南禄劝乌东德水电站是我国第三座超千万千瓦级水电站,其建设所采用的混凝土人工骨料来源于坝址下游施期料场的中元古代落雪组灰岩.在骨料勘察和实际开采过程中,发现灰岩与白云岩在同一层位产出,其岩性变化界线切割岩层面,该类现象为工程地质研究中所罕见,引起了高度关注.以施期料场灰岩-白云岩过渡带和骨料开采残留的一处白云岩凸起岩块...     

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萨拉乌苏河流域萨拉乌苏组沙丘砂沉积特征

萨拉乌苏河流域米浪沟湾剖面萨拉乌苏组含7层古流动沙丘砂、4层古固定-半固定沙丘砂.对这些沙丘砂的沉积构造观察以及粒度、扫描电镜和常量化学元素分析结果表明：（1）这些沙丘砂具有与现代沙丘砂相似的风成沉积构造特征;（2）粒度及其参数——Mz、σ、Sk和Kg,以及主要化学组分SiO2、Al2O3和TOFE也与现代沙丘砂相近;（3）Mz-σ、SiO2-Al2O3＋TOFE散点图和概率累积曲线显示这些沙丘砂与萨拉乌苏组中的河湖相、古土壤差别明显,而与现代沙丘砂一致;（4）石英砂颗粒具有良好的磨圆以及碟形坑、新月形坑、麻坑、上翻解理薄片、硅质沉淀和硅质裂纹等表面结构特征,反映其曾受持久的风力搬运作用.沉积构造、粒度、石英砂颗粒表面结构和化学元素等多个方面具备了与现代沙丘砂类似的风成特征,证明这些沙丘砂的成因是风成的.     

Spectral features of geomagnetic low point displacement and its mechanism

In this paper,Changli station in Hebei Province was taken as an example,in which the minute data of geomagnetic Z component was used to analyze the spectral values of its main frequencies during normal time,geomagnetic storm time and low point displacement time interval respectively. After fitting of ten high spectral values to loga-rithmic functions,it is found that,by using same length of data,the spectral values at geomagnetic storm time in-crease apparently compared with those at normal time,especially at the high frequency segment. While low point displacement occurred,the spectral values at high frequency are approximate to those at normal time,but at period above 4 hours they are mostly lower than those at normal time. Comparison of accumulating of some FFT results at low point displacement and normal time shows that,spectral values at periods of 8.5 and 13.7 hours increase at low point displacement time relative to those at normal time. Compared with the images of Ne observed at DE-METER satellite,it is illustrated that the occurrence of geomagnetic low point displacement is well corresponding with the increase of Ne in ionosphere. Finally it was discussed about those spectral features and the occurrence mechanism of geomagnetic low point displacement.     

基于张衡一号卫星波动观测的人工甚低频台站信号特征统计分析

地基人工甚低频(10~30 kHz)台站信号可以穿透电离层, 甚至泄露进地球磁层, 从而导致内辐射带高能电子的沉降.研究人工甚低频台站信号的特征对于研究辐射带电子的损失具有重要的科学意义.基于张衡一号卫星2019—2022年的电场观测数据, 本文对全球10个人工甚低频台站在电离层中的信号特征进行了研究, 统计分析了电离层中人工甚低频台站信号的昼夜差异、季变规律、对地磁活动水平的依赖性, 及其在地磁共轭区的分布特征.结果表明, 人工甚低频台站信号会传播至台站上空电离层及其共轭区, 信号辐射范围及强度与台站的发射功率呈正相关.电离层电子密度对甚低频信号的传播具有重要影响, 在夜侧和当地冬季, 电离层电子密度相对较小时, 泄露进入内磁层的人工甚低频台站信号较强, 而信号强度受地磁活动影响很弱.在台站上空, 信号增强区域以穿刺点为中心呈现近圆形分布, 并存在明显的波模干涉效应, 在共轭半球, 信号增强区域中心相对共轭穿刺点会发生极向漂移(L＜2的台站)或赤道向漂移(L＞2的台站), 但所有台站的电波能量都被限制在1/2赤道电子回旋频率磁壳以内的区域.这些统计观测特征表明, 发射台站位于较低L值(L＜1.4)的人工甚低频台站信号在内磁层中主要以非导管模式传播到共轭半球, 而发射台站位于较高L值(L＞2.6)的人工甚低频台站信号主要以导管模式传播.