Research status and thoughts on the development of seismic sedimentology in China

The seismic sedimentology is a continuous development of seismic stratigraphy and sequence stratigraphy,and has been paid much attention in recent ten years,especially in its principle,continental and marine classic sedimentary sandbodies,carbonate and mixed deposits,prediction of seismic diagenetic facies,fine characterization of sandbodies,new geophysical methods and techniques,RGB fusion of seismic attributes,and 3D visualization carving geobodies,etc. The future development of seismic sedimentology should concentrate on seismic geomorphological model,new method of seismic lithology,seismic sedimentology for exploration and exploitation, geophysical inversion methods,and artificial intelligent technology,etc. The gradually improvement of theory and methods in seismic sedimentology as well as the extended application of seismic sedimentology in hydrocarbon exploration and exploitation will increase its economic efficiency.     

Fluvial sequence pattern and its response of geomorphy in depression phase of rift basin: A case study of the Lower Member of Neogene Minghuazhen Formation in Shaleitian Uplift area,Bohai Bay Basin

The sequence classification is a difficulty of sequence stratigraphic study on rivers that are distal to coast area during the depression phase of rift basin. Based on the integrated analysis of logging,cores and seismic data,the case study shows that the Lower Member of Neogene Minghuazhen Formation in the Shaleitian Uplift area in the western Bohai Sea region corresponds to one complete third-order sequence which can be divided into four fourth-order sequences(i.e. SQm1-SQm4). Sedimentary hiatus,wide and shallow incised valley and amalgamated channel sand bodies are the main recognition of sequence boundaries in fluvial sequence stratigraphy of the study area. Each fourth-order sequence comprises low and high accommodation systems tracts. According to seismic sedimentological and quantitative geomorphological analysis,low-sinuosity rivers including braided river and low-sinuosity meandering river are well developed in the low accommodation systems tract,whereas the medium- to high-sinuosity meandering rivers are well preserved in the high accommodation systems tract. The change in the new creation of accommodation and the sediment supply exert a significant control on the stacked pattern within different systems tracts.     

Characteristics and forming mechanism of laminae fine-grained sedimentary rock of the Paleogene Funing Formation in Gaoyou and Jinhu sags,Subei Basin

The deep-water fine-grained deposits can be not only the source rock,but also the reservoir of unconventional oil and gas. Combined with high-precision centimeter-scale core observation,thin section identification,X-ray diffraction whole rock analysis,trace element test and scanning electron microscopy(SEM)analysis,the laminae characteristics and the genesis mechanism of semi-deep to deep lake fine-grained sedimentary rocks in the Member 2 of the Funing Formation are investigated in the Gaoyou and Jinhu sags of the Subei Basin. The results show that the semi-deep and deep lake fine-grained sedimentary rocks of the Member 2 of the Funing Formation in the Gaoyou and Jinhu sags are complex in lithology,and the laminae with different colors are formed by the mixture and superposition of various material components. The horizontal bedding developed in the fine-grained sedimentary rocks can be further divided into thin-laminated and thick-laminated sedimentary structures,whose macroscopic,microscopic characteristics and the composition are different. The complex forming mechanism of laminae includes two aspects: Formation process and preservation process. The generation(or the input)and the precipitation of each component have seasonal significance during the formation of laminae,whereas the preservation of the laminae could be mainly related to the water depth in the study area.     

基于波导相位调制器的光谱色散平滑技术实验研究

利用波导相位调制器产生的正弦调频脉冲进行了光谱色散平滑技术实验研究.结果表明该铌酸锂波导相位调制器可以容易地将DFB振荡器产生的单纵模信号展宽到0.1—1.5 nm,远场分析表明焦斑扫动规律与理论计算一致,近场分析表明SSD对近场百微米尺度的调制有显著改善.本研究为高功率激光装置束匀滑方案的优化提供了参考.     

龙门口水库滨岸带硝化作用研究

以龙门口水库滨岸带湿地为研究对象,以农业径流中氮元素为主要的农业面源污染物,2012年7~9月通过设置植被类型和氮浓度不同的3个采样区进行对比试验,对滨岸带土壤中氮含量、硝化细菌数量及其硝化速率进行了研究。结果表明,表层土壤硝化速率和硝化细菌数量水平分布特征为有农田径流且有水草区有农田径流且无水草区无农田径流且无水草区,且均随着土壤深度的增加明显降低。从月份变化来看氨氧化细菌(Ammonia-Oxidizing Bacteria,AOB)的数量分布表现为7月8月9月,与氨氮含量变化趋势基本一致,硝化速率也呈现出夏季大于秋季的特点。对滨岸带土壤硝化作用有显著影响的因子为AOB的数量、氨氮、总氮、总磷含量、含水率和温度,从而进一步证实了氨氧化是硝化作用的限制性步骤。     

陇西六盘山黄土及最近1．8Ma B．P．以来的构造运动与气候变化

对陇西盆地六盘山西侧山麓剥蚀面上断岘剖面的古地磁、磁化率和粒度分析表明,该剖面具有1.8 M a B.P.以来完整的黄土-古土壤沉积序列。断岘剖面以下7级黄河阶地的发育形成以及在1.1和0.8 M a B.P.前后所指示的腾格里沙漠扩张变化,反映了第四纪早更新世以来青藏高原阶段性隆升对黄土高原西部环境变化影响,以及在青藏高原隆升过程中构造与气候的变化与耦合响应。     

近交对凡纳滨对虾(Litopenaeus vannamei)生长、存活及抗逆性的影响

通过设计交配组合,建立中度近交组GM(近交系数大于0.25,家系G1,G2,G3,G4)、轻度近交组GL(近交系数0.0625—0.25,家系Z1,Z2,Z3,Z4),非近交组GN(近交系数为0,家系F1,F2,F3,F4),比较共同环境养殖90d不同近交程度凡纳滨对虾(Litopenaeus vannamei)家系体质量(BW)、存活率(SR)、高氨氮耐受存活率(SRA)及低溶氧耐受存活率间(SRH)的差异性,计算近交家系相关性状的近交衰退系数,评价近交对凡纳滨对虾生长、存活和抗逆性的影响。结果显示:GN组BW为7.66±2.86g,显著高于GM组BW(P0.05);GL组SR、SRA、SRH间差异近交衰退系数为–6.41%、–13.63%、–11.84%;GM组的SR、SRA、SRH的近交衰退系数为5.30%、–4.73%、–4.77%;Z2的BW最大为8.59±3.85g,G3的BW高于GN组均值;G2家系SR为84.81%±10.37%,显著高于其它家系(P0.05);75%的近交家系表现出SR近交衰退,62.5%的近交家系表现出SRH近交衰退。结果表明:近交导致凡纳滨对虾生长、高氨氮耐受性及低溶氧耐受性的衰退普遍存在,应避免高度近交个体的产生,近交系数应控制在0.25以下;少数近交家系的生长、存活、高氨氮耐受性或低溶氧耐受性优于非近交家系,推测选择合理亲缘选配方案可加快凡纳滨对虾遗传改良进程。     

陇西六盘山黄土及最近1.8 Ma B.P.以来的构造运动气候变化

对陇西盆地六盘山西侧山麓剥蚀面上断岘剖面的古地磁、磁化率和粒度分析表明,该剖面具有1.8 Ma B.P.以来完整的黄土-古土壤沉积序列.断岘剖面以下7级黄河阶地的发育形成以及在1.1和0.8 Ma B.P.前后所指示的腾格里沙漠扩张变化,反映了第四纪早更新世以来青藏高原阶段性隆升对黄土高原西部环境变化影响,以及在青藏高原隆升过程中构造与气候的变化与耦合响应.     

烟威近海鱼类群落分类β多样性及其组分空间变化的驱动因素分析

β多样性是区域生物多样性研究的重要方向,根据2020年在烟威近海的底拖网调查数据,采用Mantel检验分析和冗余分析(RDA)等方法,对驱动烟威近海鱼类群落β多样性及其组分的环境因素和空间距离进行了研究。结果显示,烟威近海调查共出现鱼类33种,其中优势种有3种,鱼类群落的β多样性均值为0.711～0.737,整体处于较高水平;全部鱼类群落和弱扩散鱼类群落β多样主要以物种替换(周转)组分为主,强扩散鱼类群落β多样性由丰富度差异(嵌套)组分来解释;空间距离和环境因素共同驱动烟威近海鱼类群落β多样性,离岸距离OD是影响烟威近海鱼类群落β多样性的关键因素,地理距离GD是物种替换的决定性驱动因子,环境因子影响了弱扩散鱼类群落的丰富度差异。表明空间距离驱动烟威近海鱼类群落β多样性的作用强于环境过滤,扩散限制是其β多样性的关键影响因素,研究结果可为烟威近海生物多样性保护提供理论依据。     

具有2个公共小函数的整函数及其k阶导数的唯一性

利用加权分担的思想,证明整函数及其k阶导数具有2个公共小函数的1个唯一性定理,改进Frank G, 郑稼华,王书培和杨连中等人的有关结果.