一个三维生化反应竞争模型的非线性振荡     

黄迅成  许晓宁 《广东海洋大学学报》2007,27(1):59-61

在微生物培养的过程中,有时会产生一些振荡现象,这种现象对应了有关数学模型中的极限环的存在性。本文中心流定理证明了一类两个微生物竞争一个具有再生功能营养物的生化模型的Hopf分支以及极限环的存在性,证明了在这一类的生化培养中非线性振荡现象同样存在。  相似文献   

Preliminary Observations in the Neighbourhood of Urumuchi; Sinkiang     

S.Ting 《地理学报(英文版)》1947,(2)

In May 1945, the author flew to Urumuchi vis the Kansu Corridor. There are evidently streamflood cournes on the no 'thern front the Chilienshan and great pediments have been formed. Former erosional surface on the Chilienshan were seen in two localities. They ars well preserved flat-topped benches sloping towards the north; and flanked by gullies, These lie at the altitude 3,200 meters above the sea.  相似文献   

国家信息化与数字地球     

承继成  李琦 《中国测绘》1999,(6):13-14

  相似文献   

如何打造高精度地质时间轴？          下载免费PDF全文

沈树忠  樊隽轩  王向东  张飞飞  史宇坤  张书涵 《地球科学》2022,47(10):3766-3769

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藏南冈底斯岩浆带研究进展与展望     

孟元库  袁昊岐  魏友卿  张书凯  刘金庆 《高校地质学报》2022,28(1):1-31

冈底斯岩浆岩带（以下简称冈底斯带）是新特提斯洋俯冲和印度—亚洲板块碰撞的产物,为典型的复合型大陆岩浆弧,是研究板块增生、大陆地壳生长再造和碰撞造山的天然实验室。大量研究揭示新特提斯洋主要经历了4个重要的演化时期：分别是早期俯冲（>152 Ma）、晚期俯冲（100~65 Ma）、主碰撞（55~40 Ma）和后碰撞伸展期（23 Ma至今）。前人对其开展了大量的工作,并取得了重要的认识和进展,然而关于新特提斯洋的形成和演化以及冈底斯带火成岩岩浆源区的属性、精细的成岩过程等方面仍然存在着激烈的争议。文章首先介绍了冈底斯带的研究历史和大地构造背景,对冈底斯带目前存在的主要科学问题和争议进行了初步梳理,从13个方面进行了论述和总结。初步的梳理给出的启示是：冈底斯带是一个典型的岩浆—构造—成矿—变形变质带,经历了长期、复杂和多阶段的演化过程,而不是简单地拼贴于古老拉萨地体之上的新生大陆岛弧体。主要认识包括：（1）冈底斯岛弧带是研究新特提斯洋俯冲最为理想的场所,记录了新特提斯洋演化的关键信息,是破解新特提斯洋板片初始俯冲时限和板片俯冲方式最佳的研究对象;（2）冈底斯带中不同时代的花岗岩基或岩株可能经历了一个多期次组装累积的过程,今后应运用晶粥体的模型去重新理解冈底斯带花岗质岩石的形成和动力学成岩过程;（3）冈底斯地区地幔的性质沿着走向表现出复杂性,具有地球化学上的不均一性;（4）冈底斯带的火成岩存在同位素上的倒转,这可能暗示冈底斯地区存在老的基底;（5）冈底斯岛弧带在构造上具有明显的掀斜性,表现出东段以下地壳组分为主,中西段以中上地壳组分为主,暗示了冈底斯带自新生代以来经历了一个不均衡的构造抬升和剥露过程; （6）冈底斯带的研究对象仍以火成岩为主,研究方法多限于传统的岩石学和放射性Sr-Nd-Hf同位素手段,而非传统的稳定性同位素（Mg-O-Li-B-Mo）的研究却鲜有报道,并且在研究内容上主要以岩石成因和地质年代学为主,而对火成岩侵位过程和成岩后的构造变形和抬升剥蚀等相关研究则相对薄弱;（7）目前,构造地质学手段在冈底斯带的研究中运用较少,常以岩浆演化来代替构造演化。最后,文章针对目前的研究现状,对冈底斯带未来的研究方向进行了展望。  相似文献   

Estimation of the impact of biomass burning based on regional transport of PM_2.5 in the Colombian Caribbean     

Jehison Bolaño-Truyol  Ismael L.Schneider  Heidis Cano Cuadro  Jorge D.Bolaño-Truyol  Marcos L.S.Oliveira 《地学前缘(英文版)》2022,(1)

Deterioration of air quality due to the increase in atmospheric emissions from biomass burning(BB)is one of the major environmental problems worldwide.In this study,we estimated the contributions of BB to PM_2.5 concentrations in the municipalities of Soledad and Malambo located in the Colombian Caribbean.The evaluation period ranged from February 24 to March 30,2018,a period with a high number of BB events recorded in the surroundings of the evaluated sites.The contribution of BB to the two sampling sites was estimated using the Hybrid Single-Particle Lagrangian Integrated Trajectory(HYSPLIT)dispersion model with forwarding trajectories from each of the burning points identified by satellite images(n=1089).The PM_2.5 emissions were determined using the fire radiative power(FRP),obtained by remote-sensing data,and corresponded to the radiant energy released per time unit by burning vegetation.The average PM_2.5 concentrations during the evaluation period were 19.91μg/m³ for Soledad and 22.44μg/m³ for Malambo.The average contribution of BB to these municipalities was 22.8%and 28.8%,respectively.The methodology used in this study allowed to estimate the contribution of this important source without knowledge of a previous tracer of BB,thereby increasing the use of the proposed procedure worldwide.This information would enable the implementation of effective mitigation,thereby diminishing the adverse impact of PM_2.5 on the health of the population.  相似文献   

Segmental closure of the Mongol-Okhotsk Ocean: Insight from detrital geochronology in the East Transbaikalia Basin     

Anastasia V.Arzhannikova  Elena I.Demonterova  Marc Jolivet  Ekaterina A.Mikheeva  Alexei V.Ivanov  Sergey G.Arzhannikov  Valentin B.Khubanov  Vadim S.Kamenetsky 《地学前缘(英文版)》2022,13(1):101254

The Late Paleozoic–Early Mesozoic Mongol-Okhotsk Ocean extended between the Siberian and Amur–North China continents.The timing and modalities of the oceanic closure are widely discussed.It is largely accepted that the ocean closed in a scissor-like manner from southwest to northeast(in modern coordinates),though the timing of this process remains uncertain.Recent studies have shown that both western(West Transbaikalia)and eastern(Dzhagda)parts of the ocean closed almost simultaneously at the Early–Middle Jurassic boundary.However,little information on the key central part of the oceanic suture zone is available.We performed U-Pb(LA-ICP-MS)dating of detrital zircon from wellcharacterized stratigraphic sections of the central part of the Mongol-Okhotsk suture zone.These include the initial marine and final continental sequences of the East Transbaikalia Basin,deposited on the northern Argun-Idemeg terrane basement.We provide new stratigraphic ages for the marine and continental deposits.This revised chronostratigraphy allows assigning an age of~165–155 Ma,to the collisionrelated flexure of the northern Argun-Idemeg terrane and the development of a peripheral foreland basin.This collisional process took place 5 to10 million years later than in the western and eastern parts of the ocean.We demonstrate that the northern Argun-Idemeg terrane was the last block to collide with the Siberian continent,challenging the widely supported scissor-like model of closure of the MongolOkhotsk Ocean.Different segments of the ocean closed independently,depending on the initial shape of the paleo continental margins.  相似文献   

基于现场试井数据和岩心驱替试验的采油初期渗透率演化规律     

KOZHEVNIKOV V.Evgenii  TURBAKOV S.Mikhail  RIABOKON P.Evgenii  GLADKIKH A.Evgeniy  POPLYGIN V.Vladimir  GUZEV A.Mikhail  戚承志 《岩土力学》2023,(3):834-842

油气开采过程中渗透率预测是一个非常重要的问题。由于油气储量衰竭导致渗透率降低,储层压力下降（有效压力增加）,导致油气生产时间增加。对有效压力导致渗透率降低的问题进行了大量研究,主要是通过各种方法建立渗透率模型,如岩心驱替试验和现场试井。前期研究结果表明,渗透率对有效压力具有幂律或指数依赖性,然而,预测渗透率的困难在于滞后现象,其原因尚不完全清楚。一些学者利用储层力学模型模拟渗透率以及解释滞后的原因,但该模型在油气生产初期有效压力波动较小时并不适用。在这项工作中,分析Perm地区北部一个油田的试井数据得出：生产初期的储层渗透率很大程度上取决于流体产出量。基于陆相储层的试井数据,得到一个描述采油初期渗透率变化的模型。为验证该模型,根据专门开发的程序对陆相储层样品进行岩心驱替试验。岩心驱替结果表明,从试井数据中获得的模型具有高收敛性。利用计算机断层扫描（computed tomography,简称CT）和扫描电镜（scanning electron microscope,简称SEM）研究岩心孔隙的属性和结构,发现天然胶体的迁移是生产初期低黏土岩石渗透率下降的主要原因。  相似文献   

甘肃北山古堡泉西铁矿床地质特征及成因分析     

司豪佳  陈百磊  刘甲成  马国龙  李文轩 《化工矿产地质》2023,(3):237-243

古堡泉西铁矿位于甘肃北山成矿带南缘,是该区新发现的中型铁矿床。该矿深部勘查取得了许多新的进展,但矿床成因研究较少。本文结合区内成矿地质背景,探讨了矿床地质特征及成因类型,初步建立了铁矿成矿模型。综合研究认为,古堡泉西铁矿床为岩浆热液型铁矿床,成矿方式以充填作用为主,交代作用次之;矿体赋存岩性为辉长岩,呈不规则的脉状及透镜状,矿石矿物主要为磁铁矿、黄铁矿、黄铜矿。  相似文献   

济南边界层风廓线雷达与L波段雷达大风探空测风对比     

王栋成  邱粲  董旭光  曹洁 《气象》2019,45(8):1169-1180

基于相同站点的济南边界层风廓线雷达(WPR)和L波段雷达大风探空测风(以下简称LW)资料,采用相关、拟合、廓线分析等方法,系统地对比两者大风(≥10.8 m·s~(-1))数据的各统计特征、相关性、时空变化规律的异同。结果表明:(1)两者u分量、v分量、风向、风速的相关系数分别为0.973、0.965、0.994、0.665,标准偏差分别为2.04 m·s~(-1)、2.88 m·s~(-1)、10.82°、2.53 m·s~(-1),大风数据相关性总体较高,且相关系数风向优于风速的、降水样本优于非降水的,表明WPR观测大风数据可信、降水期间WPR水平大风数据可以使用。(2)两者大风风向、风速基本一致,但在低层差异较高层的大,尤其是340 m及以下高度层更显著,降水、非降水、全部样本在2980、1900、2740 m以下WPR风向值均略小于LW,而在1300、2740、1660 m以下WPR风速值均略大于LW。(3)两者资料互补性总体较好,大风风向、风速、v分量差值随高度变化符合对数律递增或递减规律,但u分量需分段拟合;在进行回归方程求算和资料互补时,应考虑差异随高度等的变化。  相似文献