16种地震科学期刊载文被引统计分析

依据《中国学术期刊文献评价统计分析系统》（V 1.0）,统计分析了2003~2007年16种地震科学期刊的总被引频次、影响因子、被引半衰期、即年指标、Web即年下载率等被引指标和较高频次被引论文。同时对期刊的现状进行了初步讨论,并提出了一些建议,以期为办刊提供一定的参考。     

宁波市不同粒径颗粒物中无机离子污染特征研究

细颗粒物(PM_2.5)对气候、空气质量和人体健康具有显著影响,水溶性无机离子是PM_2.5主要成分。在2018-01-24至2018-02-20期间,宁波地区经历了一系列低温和PM_2.5浓度较高的天气过程,利用在线离子色谱(MARGA)和颗粒物化学组分监测仪(ACSM)监测宁波气溶胶的无机离子,研究了PM_2.5和亚微米细颗粒物(PM_1.0)中硫酸根(SO₄^2-)、硝酸根(NO₃^-)和铵根(NH₄⁺)(三者统称为SNA)的变化特征。结果表明,SNA的质量浓度均与PM_2.5有明显正相关;随PM_2.5质量浓度的增加,SO₄^2-当量浓度(摩尔浓度×所带电荷数)百分比呈现减少趋势,而NO₃^-百分比呈现增加趋势;NH₄     

ZJB(BP)-30A型变频调速高压注浆泵的研制

介绍ZJB（BP）－30A型变频调速高压注浆泵的设计思路、研制过程以及其主要技术参数和性能特点。     

Quantifying the response of forest carbon balance to future climate change in Northeastern China: Model validation and prediction

In this study, we report on the validation of process-based forest growth and carbon and nitrogen model of TRIPLEX against observed data, and the use of the model to investigate the potential impacts and interaction of climate change and increasing atmospheric CO₂ on forest net primary productivity (NPP) and carbon budgets in northeast of China. The model validation results show that the simulated tree total volume, NPP, total biomass and soil carbon are consistent with observed data across the Northeast of China, demonstrating that the improved TRIPLEX model is able to simulate forest growth and carbon dynamics of the boreal and temperate forest ecosystems at regional scale. The climate change would increase forest NPP and biomass carbon but decrease overall soil carbon under all three climate change scenarios. The combined effects of climate change and CO₂ fertilization on the increase of NPP were estimated to be 10–12% for 2030s and 28–37% in 2090s. The simulated effects of CO₂ fertilization significantly offset the soil carbon loss due to climate change alone. Overall, future climate change and increasing atmospheric CO₂ would have a significant impact on the forest ecosystems of Northeastern China.     

华北地区重力势能差水平构造应力分布特征

采用Crust 1.0 地壳模型、SIO V24.1重力场模型和SIO V18.1地形模型计算华北地区的重力势能,并进行动力地形改正以消除岩石圈下地幔运动产生的径向作用力对重力势能的影响。利用有限元方法求解重力势能与水平构造应力之间的平衡方程,得到华北地区的水平构造应力分布。结果表明,华北地区水平构造应力空间分布不均匀,高重力势能区表现为引张状态,低势能区为压缩状态;阴山-燕山断块中北部为高势能区,张应力以N-S方向分布;华北平原断块西南部卫辉周围、东北部葫芦岛和秦皇岛一带以及河淮平原断块西北部郑州附近为低势能区,最大主应力方向为NWW-SEE。     

南苏鲁超高压变质带东海ZK703钻孔榴辉岩的变质作用

东海ＺＫ７０３钻孔位于苏鲁超高压变质带南部,钻孔深５５８ｍ穿过的岩性主要为榴辉岩,黑云斜长片麻岩和石榴橄榄岩,及少量多硅白云母石英片岩,石榴石多硅白云母英片岩,蓝晶石石英岩和硬玉石英岩,钻孔揭示榴辉岩呈层状产出,具中等倾角,稳定延利到钻孔深度以下。超高压矿物或其后成合晶假象在这些岩石中的保存,以及岩石之间的接触关系表明,这是一个整体经历了超高压变质作用的表壳岩和基性一超基性岩组合,据原生次要矿物,     

CG-LTDR地表覆盖数据对BCC_AVIM 1.0陆面温度模拟的影响研究

本文将CG-LTDR数据集中的地表覆盖数据产品应用于北京气候中心陆面模式（BCC_AVIM 1.0）中,并通过数值模拟分析不同覆盖类型的数据（冰川、湿地、湖泊、植被PFT）更新对模拟结果的影响。结果表明,新数据对不同地表类型的基本分布特征都有合理描述,但与模式中原有数据的差异明显,表现为冰川比例在格陵兰岛西部地区增加,湿地在大部分地区都减少,湖泊在北美和欧亚大陆中高纬地区的比例减少,但青藏高原及周边地区小幅增加,植被PFT的差异最明显。与采用模式原地表覆盖数据的控制试验相比,新数据引入所致的改变,主要局限于地表覆盖数据改变的区域。冰川数据更新使高纬冰川积雪区和青藏高原的温度降低,湿地数据提高了欧洲和北美主要水区的地面温度,湖泊数据有效降低了亚洲地区的温度,更新植被PFT的影响最广泛,使得南美、南非、东北亚、北美和澳洲大部分地区的温度升高,而中国华南江南地区以及南亚地区的温度降低,但在一些地区的模拟效果降低。数据全部更新引起的温度改变最明显,但并不是所有类型的简单叠加,尤其在地表复杂区域。不同的覆盖类型数据更新,可在一定程度上减少模式对于地表温度的模拟偏差（如格陵兰岛西部和青藏高原地区、欧洲内陆湖区的温度偏高）,因此需适当选用更新的数据。     

水文水深数据修正的普里兹湾数字水深模型

在第一版国际南大洋地图集(the International Bathymetric Chart of the Southern Ocean Version 1.0,IBCSO V1)的基础上,利用现场水文观测中的水深数据重构了普里兹湾及其周围海域的海底地形,建立了更准确的高分辨率数字水深模型。从多套现场水文观测数据中提取了水深观测结果,去除重复剖线后,比较了水文观测中的水深数据与IBCSO V1在500 m×500 m网格上的差异。在保留IBCSO V1中原始多波束、单波束回声测深数据和其他水深观测数据的前提下,使用插值技术修正了无观测数据海域地形。基于大量的海豹观测数据在较大程度上订正了IBCSO V1海床深度。与IBCSO V1海床深度相比,从戴维斯站以东至82°E的南极大陆沿岸、埃默里冰架前缘西部以及西冰架前缘附近区域的海床深度被低估的可能性最大。优化的南极普里兹湾海域水深数字地图改进了对普里兹湾海底地形结构特征的认识。更加准确的地形数据有利于理解海底地形对普里兹湾海洋环流的影响和建立更加可靠的数值模型。     

Crustal thickness in southeast Tibet based on the SWChinaCVM-1.0 model

Extensive geophysical research has been carried out in southeast Tibet due to the complex geological structure and high seismicity. The study of the Moho interface can provide useful information for the geophysical research. SWChinaCVM-1.0 is the first version of a regional community velocity model for the Sichuan-Yunnan region and aims to provide a reference for seismological research in the region. Based on this model, a high-precision community Moho interface model can be obtained using common conversion point (CCP) stacking, to further expand the applicability of SWChinaCVM-1.0. Before CCP stacking, it is necessary to check the fit of the practical and theoretical travel times of the Ps phase and its multiples under the constraints of the model. Using this method, referred to as Hκ0 stacking, we determined the Moho interface. However, the multiples were poorly fitted with the theoretical travel times at many stations, and the crustal thickness obtained was inconsistent with previous findings. Therefore, we speculate that the SWChinaCVM-1.0 model has some limitations that render it incompatible with the CCP stacking method. To further verify this hypothesis, we performed H-κ stacking using the vP-vS model, vP model, vS model, and the regional average velocity vP0 and compared the results with those of Hκ0 stacking. The results of the comparison indicate that the SWChinaCVM-1.0 model requires improvements. In addition, by analyzing the SWChinaCVM-1.0 inversion process, we found that the vS model was more reliable than the vP model. Finally, we adopted the crustal thickness obtained using H-κ stacking based on the vS model as the initial version of a community Moho interface model for the Sichuan-Yunnan region (SWChinaCVM-MOHO-1.0).     

A Comparison about Metamorphism among the Oldest-Rock Units from Orogenic Belts of Dabie, Eastern Qinling and Eastern Kunlun of Central Mountain Ranges, China

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