Local-scale patterns of genetic variation in coexisting floating-leaved Nymphoides peltata and submerged Myriophyllum spicatum in Donghu Lake

Journal of Oceanology and Limnology - Coexisting floating-leaved and submerged plants experience similar environmental changes but may evolve different patterns of genetic variation. To compare...     

A Novel Approach for Evaluating Nonstationary Response of Dynamic Systems to Stochastic Excitation

The transient state of a dynamic system, such as offshore structures, to random excitation is always nonstationary. Many studies have contributed to evaluating response covariances at the transient state of a linear multi-degree-of-freedom(MDOF) system to random excitations, but a closed-form solution was not available unless the excitation was assumed to be a physically unrealizable white noise process. This study derives explicit, closed-form solutions for the response covariances at the transient state by using a pole-residue(PR) approach operated in the Laplace domain when the excitations are assumed to be stationary random processes described by physically realizable spectral density functions. By using the PR method, we can analytically solve the triple integral in evaluating the nonstationary response covariance. As this approach uses the poles and residues of system transfer functions, rather than the conventional mode superposition technique, the method is applicable to MDOF systems with non-classical damping models. Particular application of the proposed method is demonstrated for multi-story shear buildings to stochastic ground acceleration characterized by the Kanai–Tajimi spectral density function model, and a numerical example is provided to illustrate the detailed steps. No numerical integrations are required for computing the response covariances as the exact closed-form solution has been derived. The correctness of the proposed method is numerically verified by Monte Carlo simulations.     

莱州湾早全新世高黏粒软土工程地质特征及岩相古地理

依据工程地质调查、土工试验、~(14)C测年及古生物鉴定,从莱州湾滨海地区的早全新世高黏粒软土中识别出3种古地理沉积环境。分析发现,软土黏粒含量高、呈暗色调,属埋藏型。颗粒级配、压缩模量等物理力学指标差异则指示了同期异相沉积软土的工程地质特征。采取Q型聚类分析,将莱州湾早全新世高黏粒软土划分为下三角洲相沉积软土、潮平相沉积软土、湖沼相沉积软土。通过统计分析,掌握了滨海区软土工程地质特性,为合理选取土工试验参数提供沉积学依据,为合理利用天然地基提供参考。     

A two-step ionospheric modeling algorithm considering the impact of GLONASS pseudo-range inter-channel biases

The Global Navigation Satellite System presents a plausible and cost-effective way of computing the total electron content (TEC). But TEC estimated value could be seriously affected by the differential code biases (DCB) of frequency-dependent satellites and receivers. Unlike GPS and other satellite systems, GLONASS adopts a frequency-division multiplexing access mode to distinguish different satellites. This strategy leads to different wavelengths and inter-frequency biases (IFBs) for both pseudo-range and carrier phase observations, whose impacts are rarely considered in ionospheric modeling. We obtained observations from four groups of co-stations to analyze the characteristics of the GLONASS receiver P1P2 pseudo-range IFB with a double-difference method. The results showed that the GLONASS P1P2 pseudo-range IFB remained stable for a period of time and could catch up to several meters, which cannot be absorbed by the receiver DCB during ionospheric modeling. Given the characteristics of the GLONASS P1P2 pseudo-range IFB, we proposed a two-step ionosphere modeling method with the priori IFB information. The experimental analysis showed that the new algorithm can effectively eliminate the adverse effects on ionospheric model and hardware delay parameters estimation in different space environments. During high solar activity period, compared to the traditional GPS + GLONASS modeling algorithm, the absolute average deviation of TEC decreased from 2.17 to 2.07 TECu (TEC unit); simultaneously, the average RMS of GPS satellite DCB decreased from 0.225 to 0.219 ns, and the average deviation of GLONASS satellite DCB decreased from 0.253 to 0.113 ns with a great improvement in over 55%.     

基于游客认同的文化遗产景区安全标识系统研究——以青城山-都江堰景区为例

文化遗产景区安全标识系统作为传播信息和规范观赏行为的有效方式,已成为影响游客旅游体验和衡量景区服务水准的重要因素。借助实地考察与随机抽样问卷调查,以青城山-都江堰世界文化遗产景区为例,综合利用文献分析和数理统计验证,拟定11项安全标识测量指标以调查游客对景区安全标识系统的认同感,研究结果表明:游客普遍认同遗产景区安全标识系统的重要性,但多是从利己角度的直观考虑;游客对青城山-都江堰文化遗产景区安全标识系统认同度低,安全标识系统各构成要素急需改进,尤其是安全标识的设计和功能;游客对文化遗产景区安全标识系统的认同度并不完全受人口统计特征影响;游客对文化遗产景区安全标识系统的认同度受游客出游频率和旅游形式影响。建议文化遗产景区从完善安全标识布局和基本功能、强调景观感设计、规范安全标识系统文字和色彩、改进标识的视觉尺寸和开展定期检查维护方面实施优化。     

基于遥感和InVEST模型的白龙江流域景观生物多样性时空格局研究

以甘肃白龙江流域为例,结合遥感、GIS技术和InVEST模型,从景观地理学角度选取区域生境质量、植物净初级生产力和景观状态指数为评价指标,构建区域景观尺度上生物多样性空间格局综合评估方法,并在栅格像元尺度上开展白龙江流域景观生物多样性时空变化特征分析。结果表明：白龙江流域景观生物多样性空间格局差异显著,其生物多样性高值区主要集中在自然保护区和林业管护区,低值区主要分布在舟曲-武都-文县的白龙江两岸及其以北区域、宕昌县岷江沿岸、高寒稀疏植被区和高山积雪-裸岩区。1990~2010年,流域景观生物多样性较为丰富,整体呈现不断增长的趋势,个别局部区域减弱,其增长区主要体现在生态工程实施区和林业管护区,减少区多分布在人类活动频繁的城乡农耕区和灾害多发区。     

沙坡头生态水文学研究进展及水量平衡自动模拟监测系统

在中国科学院野外站网络重点科技基础设施建设项目的支持下,沙坡头沙漠研究试验站建成了以36台大型称重式蒸渗仪为主体的中国北方不同气候带沙区水量平衡自动模拟监测系统——Lysimeter群。概述了沙坡头生态水文学研究进展。介绍了Lysimeter群建设的科学目标、构建思路、建设内容和预期研究方向。Lysimeter群由大型称重式蒸渗仪、各类探头、移动大棚和降水模拟器等组成,具有集成性和唯一性。该平台可全自动模拟控制降水和地下水位,量化植物水分来源;自动监测蒸散发、植物蒸腾、土壤水渗漏、土壤水分、温度和电导率等。该平台的建成将提升在不同尺度上认知中国沙区生态和水文过程、植被重建的生态水文学和环境胁迫生理生态学机理等相关领域的研究能力,回答不同沙区土壤水分植被承载力和人工植被稳定性维持的生态水文阈值等国家在防沙治沙实践中所面临的核心科学问题。     

基于GWR模型的中国区域旅行社业效率空间分异及动力机制分析

基于DEA模型对中国31个省域的旅行社业效率空间分异特征进行了分析,首次运用GWR模型探索交通、资本、人才、信息化和经济动力对区域旅行社业效率影响的空间差异。结果表明：旅行社业效率在空间上具有正相关性和集聚特征,空间格局从“川”字型向“山”字型转变。各动力因子的系数均存在空间非平稳性。资本和人才动力的回归系数在空间分布上从南向北依次递减;经济动力的分布趋势为从北向南依次递减;交通动力对中西部地区旅行社效率提升的促进作用显著于东部地区;信息化动力则在东部地区表现出较强的促进作用。     

中国3A级以上旅游景区空间集聚特征研究

基于中国3 228个3A级以上旅游景区数据分析其空间集聚特征。结果表明,中国3A级以上旅游景区具有典型的“类型极化、区域分化、板块集聚”的分布特征,胡焕庸线两侧景区密度悬殊;中东部地区为凝聚-随机分布,西部地区为凝聚分布,不同区域发育主题和特色不同;5A级景区集聚在经济发达地区,4A级景区沿黄河、长江集中分布,3A级景区多处于东部滨海沿线;历史知名度、自然地理环境、人口经济规模、交通区位条件、审批标准、效仿发展等因素影响较大,循环累积效应显著。据此提出“区域平衡、跨区协调、分类优化”的发展建议。     

基于北极黄河站观测的日侧极光研究新进展

回顾了基于中国黄河站全天空极光观测对日侧弥散极光与喉区极光研究的最新进展。首先,利用黄河站极光观测,对日侧弥散极光展开系统性分类与统计研究,对这一重要空间物理现象取得新认识,指出日侧弥散极光对研究日侧外磁层冷等离子体的分布、形成及磁鞘粒子进入磁层都具有重要启示作用;同时发现并定义了一种新型分立极光结构——喉区极光,并推断其可能对应磁层顶的局地变形。喉区极光是指发生在电离层对流喉区附近、从极光卵赤道侧向低纬方向延伸出来的分立极光结构。全天空极光观测表明喉区极光走向大致与电离层对流方向一致。之后,观测验证了喉区极光对应磁层顶局地内陷式变形的推测;统计发现喉区极光是一种非常高发的现象,对应的磁层顶变形尺度可达2—3 Re,并指出这种变形最可能由磁鞘高速流冲击磁层顶产生;发现在喉区极光产生过程中还可能触发磁重联;证实伴随喉区极光的产生,磁鞘粒子会进入磁层并诱发产生一种新型弥散极光。通过喉区极光研究,可以将已有的磁鞘瞬态过程研究和触发式磁重联研究有机地结合在一起,对太阳风-磁层耦合过程形成一种新的认识,即:在磁鞘中局地产生(而不是存在于太阳风中)的瞬态过程可以在日下点附近频繁地导致磁层顶局地变形、触发重联、引发系列地球空间效应,可能对太阳风-磁层耦合具有不可忽略的重要性。以此为基础,讨论了日侧极光研究引出的新课题。