Lake–mire ecosystem transformation and its possible forcing mechanisms in volcanic landform regions: a case study in the Gushantun peatland of northeast China     

Mingming Zhang  Zhaojun Bu  Shasha Liu  Jie Chen  Yaxin Cui  Xu Chen 《地球表面变化过程与地形》2020,45(13):3141-3154

Large numbers of peatlands were developed in volcanic landform regions, which would provide valuable long-term records of lake–mire ecosystem shifts and act as significant carbon pool in regional carbon cycle. To investigate lake–mire ecosystem transformations and driving mechanisms in volcanic landform regions, the developmental history of Gushantun peatland in northeast China was reconstructed in this study. Results indicate that Gushantun peatland initiated in the deepest portions of the basin, and subsequently experienced expansions outward. Peat initiated from approximately 12 ka cal. bp to present. The developmental patterns of Gushantun peatland can be divided into four stages: the stable stage 1 (12–10 ka cal. bp ), maximum stage (10–7 ka cal. bp ), stable stage 2 (7–4 ka cal. bp ) and stable stage 3 (4–0 ka cal. bp ). The possible forcing mechanisms for the development of Gushantun peatland were different during different periods. From 12 ka cal. bp to 10 ka cal. bp , autogenic process was probably the major controlling factor for the expansion of this peatland. From 10 to 7 ka cal. bp , flat basin morphology was the major influence factor for fast expansion. However, the development of Gushantun peatland was probably controlled by the dual effects of high moisture and autogenic process during the period of 7 to 4 ka cal. bp . From 4 ka cal. bp to present, steep basin morphology was the major influence factor, while moisture might be the secondary factor for development of Gushantun peatland. These features indicate that lake–mire ecosystem transforms in volcanic landform regions of Changbai Mountains were probably triggered by the complex effects of autogenic process, hydroclimate and underlying basin morphology. © 2020 John Wiley & Sons, Ltd.  相似文献   

Study on forecast scenarios for simulation of future urban growth in Shenyang City based on SLEUTH model     

Xiaoqing Wu  Yuanman Hu  Hongshi He  Fengming Xi  Rencang Bu 《地球空间信息科学学报》2010,13(1):32-39

The SLEUTH urban growth model was used to simulate future urban growth patterns and to explore potential environ-mental impacts of urban development under different conditions of development in Shenyang City, China. The SLEUTH model was calibrated with historical data (1988-2004) extracted from a time series of TM satellite images, and the future growth was pro-jected out to 2030 assuming three different policy scenarios: (1) current trends scenario (Scenario CT), (2) regional policy and ur-ban planning sce...  相似文献   

The 273.15-K-Isothermal Evaporation Experiment of Lithium Brine from the Zhabei Salt Lake, Tibet, and its Geochemical Significance     

Feng Gao  Mianping Zheng  Pengsheng Song  Lingzhong Bu  Yunsheng Wang 《Aquatic Geochemistry》2012,18(4):343-356

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海底蚀变玄武岩中次生组分去除实验研究     

卜文瑞  李力  朱爱美  张辉  张俊  崔菁菁 《地球科学进展》2012,27(10):1167-1172

选择有大量次生方解石沉淀的海底蚀变玄武岩为研究对象,研磨、均一化后将粉末样品分为49份,其中48份分别以0.25,0.5,1.0,1.5,2.0,2.5 mol/L 6种浓度的足量HCl溶解0.5,1,2,4,8,16,32,64 h,选取溶解残渣测定其主要氧化物和特征微量元素含量,研究确定HCl溶解法去除海底玄武岩中次生组分的浓度—时间组合。结果表明,1.0 mol/L-0.5 h,1.0 mol/L-1 h,1.0 mol/L-2 h,1.0 mol/L-4 h,1.5 mol/L-0.5 h,1.5 mol/L-1 h,2.0 mol/L-0.5 h,2.0 mol/L-1 h和2.5 mol/L-0.5 h等9种HCl浓度—时间组合是可供去除海底蚀变玄武岩中次生碳酸盐的理想方案。  相似文献   

影响低渗透油藏注水开发效果的因素及改善措施          下载免费PDF全文

李志鹏  林承焰  董波  卜丽侠  崔玲 《地学前缘》2012,19(2):171-175

在单砂体划分和内部结构研究的基础上,运用地质因素与生产相结合的手段,研究了影响低渗油藏注水开发效果的因素,发现影响低渗油藏开发效果的地质因素主要有3个:(1)孔隙结构特征。一般孔隙结构越复杂,孔径越小,开发效果越差。(2)砂体内部构型。砂体建筑结构越复杂,开发效果越差。(3)夹层频率的影响。适量的夹层提高厚油层的开发效果,而过量的夹层,则降低开发效果。除地质因素以外,还分析了渗流特点、贾敏效应以及压敏效应等开发因素对低渗透油藏开发效果的影响。启动压力梯度越大,开发效果越差;贾敏效应降低开发效果;压敏效应越严重,开发效果越差。针对以上影响因素提出了5种改善低渗透油藏开发效果的措施:以小层为单位按单砂体合注合采、水平井开发、适当放大生产压差、尽量减小井距以及早期注水。  相似文献   

散粒体斜坡堆积特性与崩坍形式研究     

李川  傅荣华  魏丽娜  何娜  卜祥航  汪留洋 《地质灾害与环境保护》2012,23(3):68-72

通过圆盘沙堆以及斜坡堆积物理模拟试验,解释其崩滑的动力学机制.发现溜砂坡堆积的过程是一个典型的自组织临界过程,整个坡体是一个广延耗散动力学系统.从颗粒级配的角度探究其对散粒体边坡稳定性的影响.  相似文献   

鲁西隆起晚中生代盆地重矿物组合分析及其构造响应          下载免费PDF全文

卜香萍  石永红  李忠 《地质科学》2012,(4):1116-1129

本文以鲁西隆起区盆地及周边盆地砂岩中碎屑重矿物为研究对象,通过重矿物的稳定性分析,以及通过不同源区重矿物组合的差异,探讨了鲁西隆起及周边地区晚中生代以来的物源及构造演化过程。研究结果显示,鲁西盆地中生代早期早中侏罗纪时期主要源区为鲁西隆起,中晚侏罗纪时期主要物源为胶东地区和鲁西隆起,而早白垩世时期主要物源为胶东地区,其次才是鲁西隆起。晚白垩世沂沭断裂带盆地物源主要是鲁西隆起和胶东地区,鲁西隆起贡献量大于胶东地区。重矿物的稳定性也折射出源区构造演化历史。早-中侏罗世至中-晚侏罗世,鲁西盆地重矿物物源由鲁西隆起向胶东地区的显著转变,暗示着苏鲁造山带自三叠纪形成之后,经折返抬升,至晚侏罗世之前已经到达地表。重矿物的含量变化显示,早白垩世中期和晚白垩世中期鲁西盆地内沉积了大量的鲁西变质岩矿物组合,并且不稳定重矿物含量急剧增加,我们推测鲁西在早白垩世晚期、晚白垩世中期存在两次构造抬升。  相似文献   

Evaluation of phosphorus bioavailability in sediments of the shallow lakes in the middle and lower reaches of the Yangtze River region,China   总被引：3，自引：0，他引：3  

Shengrui Wang  Xiangcan Jin  Qingyun Bu  Haiqing Liao  Fengchang Wu 《Environmental Earth Sciences》2010,60(7):1491-1498

Phosphorus (P) fractions and their bioavailability in the sediments from the middle and lower reaches of the Yangtze River region were investigated using different chemical extraction methods. The results show that the contents of bioavailable P in the sediments extracted by different extraction procedures varied greatly. But their rank order was similar. Potentially releasable P (PRP) was the largest, followed by algal available P (AAP), NaHCO₃ extractable P (Olsen-P), water soluble P (WSP), and readily desorbable P. PRP contributed approximately 60% to total P (TP) in most sediments, AAP 20%, Olsen-P 15%, WSP 2%, and readily desorbable P (RDP) 0.5%. For the heavily polluted sediments, their bioavailable P extracted from TP mainly originated from inorganic P (IP), IP mainly originated from NaOH–P, the bioavailable P concentrations can be evaluated by measuring the concentrations of TP, NaOH–P, and IP. For the slightly polluted sediments, the bioavailable P can only be evaluated by different chemical extractable methods.  相似文献   

Kinematics of Interacting ICMEs and Related Forbush Decrease: Case Study     

D. Maričić  B. Vršnak  M. Dumbović  T. Žic  D. Roša  D. Hržina  S. Lulić  I. Romštajn  I. Bušić  K. Salamon  M. Temmer  T. Rollett  A. Veronig  N. Bostanjyan  A. Chilingarian  B. Mailyan  K. Arakelyan  A. Hovhannisyan  N. Mujić 《Solar physics》2014,289(1):351-368

We study heliospheric propagation and some space weather aspects of three Earth-directed interplanetary coronal mass ejections (ICMEs), successively launched from the active region AR 11158 in the period 13?–?15 February 2011. From the analysis of the ICME kinematics, morphological evolution, and in situ observations, we infer that the three ICMEs interacted on their way to Earth, arriving together at 1 AU as a single interplanetary disturbance. Detailed analysis of the in situ data reveals complex internal structure of the disturbance, where signatures of the three initially independent ICMEs could be recognized. The analysis also reveals compression and heating of the middle ICME, as well as ongoing magnetic reconnection between the leading and the middle ICME. We present evidence showing that the propagation of these two, initially slower ICMEs, was boosted by the fastest, third ICME. Finally, we employ the ground-based cosmic ray observations, to show that this complex disturbance produced a single cosmic ray event, i.e., a simple Forbush decrease (FD). The results presented provide a better understanding of the ICME interactions and reveal effects that should be taken into account in forecasting of the arrival of such compound structures.  相似文献   

杭州市伏、秋旱灾害风险区划     

陈鑫  缪启龙  俞布  沈伟风  宋健 《气象与减灾研究》2013,(3):57-62

根据杭州市1959-2010年降水资料、自然环境以及社会经济要素,综合致灾因子、孕灾环境、承灾环境及防灾减灾能力,构建区域干旱灾害风险评价模型。通过ArcGIS空间分析技术结合模糊综合评价法,编制以100 m＆#215;100 m栅格为基本评价单元的杭州市伏、秋旱灾害风险区划图。区划结果表明,淳安西北部、建德中南部、桐庐中部、富阳南部、临安东部以及余杭、主城区,伏旱、秋旱灾害风险均较高。  相似文献