苏北滨海盐碱土壤性质演化及其对脱盐规律的启示

结合野外观测和室内分析,研究了江苏如东县滨海地区围垦土地土壤性质演化规律,及其演化过程中不同粒径组分含量变化对脱盐规律的影响。结果表明,江苏如东滨海地区围垦土地随着围垦年限的增加,土壤质地逐渐变细,盐度逐渐降低。土壤质地变化趋势与盐度变化趋势具有较好一致性。砂粒含量与盐度随着围垦年限的增长而同时降低,粉粒含量随着围垦年限的增长而增加。黏粒含量与盐度变化关系较复杂,在围垦年限短的高盐度区域表现为黏粒含量随围垦年限增加而升高,与盐度变化呈相反趋势。而随着围垦年限增加到土壤盐度处于较低水平时,黏粒含量对盐分淋洗的阻碍作用较强,黏粒含量较高区域往往盐度较高。     

走滑运动—三角洲的耦合控藏——以俄罗斯北萨哈林盆地为例

基于对俄罗斯北萨哈林盆地构造演化及地层充填特征的基础地质特征分析和油气分布规律的总结,对盆地油气分布特征的主控因素进行了探讨。研究认为:盆地的油气分布在平面上具有油气田呈S—N向成带分布,从北向南具有"油减少、气增多"的特点;在纵向上,油气发现的层位具有"北上南下"的特点;在规模上,油气储量分布具有"陆小海大"的特点。油气成藏条件综合评价分析认为,油气分布主要受走滑断裂和三角洲发育的控制,具体表现为:走滑运动与不同时期的三角洲控制着烃源岩的展布,使得油气分布呈北产油南产气的特征;走滑运动和3期三角洲的迁移使得油气发现层位呈"北上南下"的特点;走滑断裂带控制了圈闭规模和保存条件,使得油气田规模呈"陆小海大"的特点。结合以上分析指出,北萨哈林盆地东部海域勘探程度低,含油气系统证实具有多期三角洲和多类型圈闭发育,是北萨哈林盆地具有较大勘探潜力的区域。     

壮医经筋挑刺法治疗神经根型颈椎病30例临床观察

目的：观察壮医经筋挑刺法治疗神经根型颈椎病的临床疗效。方法：将60例神经根型颈椎病患者随机分为2组,每组各30例。治疗组采用壮医经筋挑刺法治疗,对照组采用常规针刺治疗。观察比较2组综合疗效、VAS评分、NPQ评分及SF-36生活质量量表评分。结果：总有效率治疗组为96.7%,对照组为73.3%,2组比较,差异有统计学意义（P<0.05）;2组VAS、NPQ及SF-36生活质量量表评分治疗前后组内比较及治疗后组间比较,差异均有统计学意义（P<0.05）。结论：壮医经筋挑刺法治疗神经根型颈椎病能有效减轻症状,改善生活质量,疗效显著。     

方斑东风螺早期发育阶段形态的观察

方斑东风螺样品采自福建省南部诏安海域.其卵囊无色透明,叶片状,每个卵囊内有受精卵500～1 600个,卵径为280～308μm.方斑东风螺胚胎发育在卵囊内进行,第一次和第二次卵裂分别为经裂,分裂中有极叶出现.随后其卵裂以螺旋式不等裂方式进行,在胚胎的动物极形成帽状胚盘.其囊胚期胚体开始缓慢转动.在水温为29.0～29.5℃的条件下,产卵后60～63 h其成为早期面盘幼虫.此期以面盘、足、壳的出现为标志.中期面盘幼虫阶段包括囊内的面盘幼虫至出囊后且卵黄尚未消失的浮游幼虫初期阶段.出囊后的幼虫浮游1～2 d后,卵黄囊完全消失成为后期面盘幼虫,心脏搏动频率加快,足变大并伸长.在水温为27.5～28.5℃的条件下,经10～12 d的浮游,后期面盘幼虫转为底栖生活,随后面盘退化、萎缩并完成变态,营爬行生活,贝壳上出现棕褐色斑纹,成为稚螺.     

顶点成分分析算法在端元数目估计中的应用研究

确定端元数目是混合像元分解中端元提取的前提,目前端元数目主要还是通过图像处理人员目视判读来获取。 在研究顶点成分分析算法的原理和端元光谱之间在大多数情况下相互独立的基础上,提出一种基于顶点成分分析算法的端元数目估计方法。 通过在不同端元数目、对噪声的稳健性、图像大小不同时的实验表明,该方法能够比较正确、有效地估计图像中的端元数目,文中方法与其他端元数目估计算法及相关系数阈值的自动化确定问题还需要进一步研究。     

Spar平台垂荡-纵摇耦合运动失稳机理

研究参数激励和强迫激励共同作用下Spar平台垂荡-纵摇耦合运动的失稳机理.考虑静稳性和排水体积的变化,推导平台的垂荡回复力和纵摇回复力矩表达式,建立规则波浪中平台垂荡-纵摇耦合的运动方程.以经典Spar平台为例,分析平台垂荡-纵摇耦合运动发生马休类型不稳定运动的条件以及平台运动失稳的形式,给出波高和波浪周期平面上平台因大幅运动失稳的参数域.结果表明,当波高相对较小时,波浪的临界周期接近于垂荡固有周期,平台失稳的形式为马休失稳;当波高相对较大时,波浪的临界周期远离垂荡固有周期,平台由于大幅摇摆运动而失稳.     

兰西局加快信息化建设

本报讯 兰西县国土资源局不断加强信息化建设,有力地推进了部门工作,提高了工作质效,降低了行政工作成本。 一是加大资金投入力度,微机配置层次高。二是搭建了电子政务信息平台。三是业务往来网络化。     

A new economic assessment index for the impact of climate change on grain yield

The impact of climate change on agriculture has received wide attention by the scientific community. This paper studies how to assess the grain yield impact of climate change, according to the climate change over a long time period in the future as predicted by a climate system model. The application of the concept of a traditional ＂yield impact of meteorological factor （YIMF）＂ or ＂yield impact of weather factor＂ to the grain yield assessment of a decadal or even a longer timescale would be suffocated at the outset because the YIMF is for studying the phenomenon on an interannual timescale, and it is difficult to distinguish between the trend caused by climate change and the one resulting from changes in non-climatic factors. Therefore, the concept of the yield impact of climatic change （YICC）, which is defined as the difference in the per unit area yields （PUAY） of a grain crop under a changing and an envisaged invariant climate conditions, is presented in this paper to assess the impact of global climate change on grain yields. The climatic factor has been introduced into the renowned economic Cobb-Douglas model, yielding a quantitative assessment method of YICC using real data. The method has been tested using the historical data of Northeast China, and the results show that it has an encouraging application outlook.     

A numerical study on the winter monsoon and cold surge over East Asia

By using the improved regional climate model （RegCM_NCC）, a numerical study has been undertaken for the East Asia region over a period of 5 years （1998-2002） in an effort to evaluate the model＇s ability to reproduce the winter monsoon conditions that were observed. The results showed that the model can successfully simulate the basic characteristics of the winter monsoon circulations, including the location and intensity of the cold-surface, high-pressure system, as well as the wind patterns and the intensity of the winter monsoon. The simulated occurrence frequency and regions of the cold surge were consistent with the observations. The simulated rainfall distribution over China was consistent with the observations collected in South China. The features of the simulated moisture transport were also in good agreement with the observations that were derived from the NCEP reanalysis data, indicating that moisture transport coming from the Bay of Bengal trough plays a crucial role in supplying moisture needed for precipitation in South China. In addition, the moisture transport coming from the near-equatorial west-Pacific was also important. These two branches of moisture transport converged in South China, as a prerequisite for occurrence of the precipitation that was observed there. Heat budgets have shown that the development of a heat sink over the East Asian continent was remarkable and its thermal contrast relative to the neighboring seas was the important forcing factor for the winter monsoon activity. The simulation also indicated that the significant differences in circulation patterns and rainfalls during the winters of 1997/98 and 1998/99 were affected by cold and warm ENSO events, respectively. The above analysis demonstrated the model＇s ability to simulate the East Asian winter monsoon.     

滇西北地区现今构造应力状态及其与地震的关系

基于搜集到的2000—2018年滇西北地区MS≥3.0地震的震源机制解,运用线性叠加反演法进行应力场反演,分析了滇西北地区现今的构造应力状态,进一步探讨了应力张量方差的时空分布与地震活动的关系。结果显示：(1)滇西北地区地震的震源机制解类型复杂,主要以走滑型（46%）为主,正断型（27%）次之;(2)研究区的构造应力场具有整体的一致性和局部的非均匀性,呈现为NNW向挤压和ENE向拉张的走滑型应力结构,说明研究区受到来自NNW向的水平挤压作用,对该地区上地壳运动和断裂活动起主导作用;(3)滇西北地区的应力张量方差大都小于0.2,除北部一些地区外,应力场基本处于均匀状态。根据应力张量方差随时间的变化和后续地震可知,中强地震大都发生在应力张量方差值低于0.2的情形,且主要发生在应力张量方差减小即震源机制解趋于一致的过程中。空间上这些地震基本都发生在应力张量方差的低值分布区及其边缘,这一结果有助于判定发震地点和了解区域应力集中增强过程。