基于无人机遥感的古银叶树群落健康快速诊断

采用无人机低空遥感与地面调查相结合的方法对邻海陆地、远海陆地和盐生沼泽生境的古银叶树群落健康进行评价，利用冠层高度、林窗特征、光合有效辐射截面比、归一化植被指数（NDVI）、氮素反射指数（NRI）、黄色波段指数（YI）以及森林健康指数（FHI）等遥感指标指征古银叶树群落的健康状况。空-地结合的调查结果表明：1）盐生沼泽生境的古树由于树龄高，其树洞大且数量多，生境内生物多样性最低，邻海陆地生境的生物多样性最高。2）盐生沼泽生境的冠层高度最低；林窗面积最大，数量最少，形状复杂度最低；光合有效辐射截面比最小。以上指标在邻海陆地和远海陆地间差异不明显。NDVI、NRI、YI以及FHI的数值均表现出盐生沼泽小于远海陆地和邻海陆地的趋势，而在远海陆地和邻海陆地间的差异较小。3）无人机遥感的评价结果与地面调查结果契合度较高，客观地反映了不同生境古银叶树的健康状态。基于无人机遥感的评价体系在针对具体植物群落修改完善后，可以作为一种快速、无损和定量化的古树群落健康诊断方法。     

东海季节性低氧海区柱状沉积物中氧化还原敏感元素对沉积环境变化的响应

氧化还原敏感元素(Redox Sensitive Elements，RSE)如V、Cr、Mo、U等，通常在氧化条件下呈溶解态，在还原沉积环境中除Fe、Mn外，RSE被还原成低价态转移至沉积物中富集积累，因此可以利用氧化还原敏感元素在沉积物中的富集情况反演沉积环境的氧化还原状况。本文通过研究东海内陆架季节性低氧海区Zb7沉积柱中氧化还原敏感元素V、Cr、Ni、Cu、Zn、Mo、U的垂直分布、富集特征和比值，探究沉积环境氧化还原状况；发现RSE/Al和富集系数自1978年以来呈增加的趋势，但自2009年开始有所降低，整体RSE富集系数均小于3，未见明显富集。RSE比值V/Cr<2、Ni/Co<5、U/Th<0.75、0.25<(Cu+Mo)/Zn<0.55，以及Mo_EF/U_EF比值主要分布在0.08～0.3倍海水Mo/U值之间，均指示氧化的沉积环境。RSE/Al与Fe/Al、Mn/Al具有显著的相关性，表明RSE在剔除陆源碎屑输入后，主要通过与Fe、Mn氧化物结合进入沉积物，也指示氧化的沉积环境。研究结果与该区域溶解氧历史数据反映的季节性低氧结果不一致，可能与RSE在夏季季节性低氧时，沉积物中的富集信号在秋冬季溶氧水平恢复后缺失有关。尽管RSE不能有效指示东海季节性低氧环境，但Zb7沉积柱RSE在1978年后富集程度的增加以及2011年后的降低，在一定程度上反映了该区域自1978年后季节性低氧程度加重，2009年后又有所缓解的变化趋势。     

中国化石能源补贴区域分布及改革影响效应研究

从区域分布视角出发,采用价差法估算了中国2006~2015年化石能源补贴量。结果表明：能源补贴呈现东、中、西部地区依次递减的格局,分别为2.72万亿元、1.80万亿元和1.53万亿元;能源补贴存在较强的空间相关性,且呈现显著的“俱乐部”现象;取消能源补贴对于中国实现“十一五”期间节能减排目标具有重要意义,具体来说,可使全国能源强度下降幅度由19.10%提升为22.36%;取消能源补贴的东部地区节能减排效应最为明显,中部地区敏感程度相对较弱;同时,取消能源补贴会导致居民生活成本不同幅度上涨,其中中部地区居民面临最大的影响,尤其是农村居民受到的冲击更为显著;化石能源补贴改革进程中,政府需要加大对中部地区尤其是农村居民扶持力度,以抵消可能进一步拉大贫富差距的风险。     

Statistical Characteristics of Sunspot Umbra Oscillations in the Ca Bandtwo

A group of successive evolutionary images of a sunspot were observed on 4th March 2014 at the Ca II H (396.85 nm) line by the telescope on board of the Hinode satellite. The calculated oscillation period of the sample point in the umbra is 149.75 s by using the Jurkevich (JK) method. A proper averaged value of the intensity profile is selected as the steady background radiation, then the distribution of the extreme values of oscillations in the umbra is analyzed by a statistical method. The results show that the valley values follow a normal distribution, while the peak values satisfy a partial normal distribution. The distribution of these extreme values indicates that the 3 min oscillation of the umbra may be caused by the propagation of a traveling wave with a period of about 5 min in the umbra. The variation of light intensity caused by the traveling wave may be proportional to the square of the displacement of the traveling wave, resulting in a 3 min period of the light intensity, which is one half of the period of traveling wave.     

2016年南极中山站固定冰冰厚观测分析

极区海冰是全球气候系统的重要组成部分，南极的固定冰普遍存在于其沿海地区，中山站周边固定冰一般在11月中下旬达到最厚。海冰厚度是海冰的重要参数之一，2016年在南极中山站附近3个站点(S1、S2、S3站点)共布放了4套温度链浮标，包括1套SIMBA (Snow and Ice Mass Balance Array)温度链浮标和3套太原理工大学温度链浮标(TY温度链浮标)，SIMBA温度链浮标每天观测4次，TY温度链浮标每小时观测1次。利用浮标观测的温度剖面以及海冰和海水间不同介质温度差异计算得到海冰厚度。在S3站点，同时布放了SIMBA温度链浮标和TY温度链浮标。温度链浮标计算冰厚和人工钻孔观测冰厚比较结果显示，S1站点TY温度链浮标计算的海冰厚度平均误差和均方根误差分别为3.3 cm和14.7 cm，S2站点和S3站点分别为6.6 cm、6.9 cm以及4.0 cm、4.8 cm。S3站点的SIMBA温度链浮标计算冰厚和人工观测冰厚的平均误差和均方根误差为8.2 cm和9.7 cm。因而S3站点TY温度链浮标计算的海冰厚度更接近人工观测的结果。进一步对Stefan定律海冰生长模型进行对比，模型计算得到的海冰生长率为0.1～0.8 cm/d，生长率快于TY温度链浮标的结果，且受积雪影响明显。相比于卫星遥感反演冰厚的误差和观测时段的限制以及有限的人工观测，2种温度链浮标未来对于中山站附近海冰的长期监测均有重要的应用价值。     

Structural analysis and anti-complement activity of polysaccharides extracted from Grateloupia livida (Harv.) Yamada

Polysaccharides were extracted from Grateloupia livida(Harv.) Yamada using hot water(extracted product denoted WGW) and then degraded in dilute sulfuric acid(degraded product denoted WGWD). The degraded mixture was then separated into four fractions through anion exchange chromatography on 2-diethylaminoethanol(DEAE)-Bio-Gel Agarose FF gel. Electrospray ionization collision-induced dissociation tandem mass spectrometry(ESI-CID-MS/MS) was performed to elucidate the structural features of all fractions. In combination with nuclear magnetic resonance spectroscopy(NMR)and infrared spectroscopy(IR) data, the major polysaccharide structures were concluded to be μ-carrageenan and κ-carrageenan. μ-Carrageenan usually has a backbone of alternating 1,3-linked β-D-galactopyranose residues sulfated at C-4 and 1,4-linked a-D-galactopyranose residues sulfated at C-6, while κ-carrageenan consists of alternating 1,3-linked β-D-galactopyranose residues sulfated at C-4 and 1,4-linked a-D-3,6-anhydrogalactopyranose residues. Trace v-carrageenan, composed of 1,3-linked β-D-galactopyranose residues sulfated at C-4 and 1,4-linked a-D-galactopyranose residues sulfated at C-2 and C-6, was also detected. Furthermore, the polysaccharide had a backbone comprising 1,3-linked β-D-galactopyranose and1,4-linked α-L-galactopyranose sulfated at C-6, which is the agarose precursor. The hydroxy groups in the galactopyranose were partially substituted by methyl and pyruvic acid acetal(PA) groups. The anticomplementary activities of WGW and its derivatives against classical pathways were measured. The native polysaccharides in WGW had higher activities, while the derivatives had much weaker activities. This indicated that the molecular weight and sulfate content were important factors affecting the anti-complement activity.     

塔里木盆地南部中生代碰撞相关构造及其在古特提斯研究中的意义

地震资料解释和野外地质调查,在塔里木盆地南部发现中生代碰撞相关构造.同碰撞构造发育于西昆仑山前、阿尔金山前和麦盖提斜坡,为晚三叠世冲断构造.既有晚三叠世新形成的冲断构造,也有先存构造的复活(如车尔臣断裂).碰撞后构造见于西昆仑和阿尔金山前,是一些规模不大的侏罗纪—白垩纪正断层及其控制下形成堑—垒构造.晚三叠世构造应力场...     

The effect of three-dimensional variational data assimilation of QuikSCAT data on the numerical simulation of typhoon track and intensity

In this paper, the three-dimensional variational data assimilation scheme (3DVAR) in the mesoscalemod el version 5 (MM5) of the US Pennsylvania State University/National Center for Atmospheric Research is used to study the effect of assimilating the sea-wind data from QuikSCAT on the prediction of typhoon track and intensity. The case of Typhoon Dujuan (2003) is first tested and the results show appreciable improvements. Twelve other cases in 2003 are then evaluated. The assimilation of the QuikSCAT data produces significant impacts on the structure of Dujuan in terms of the horizontal and vertical winds, sealevel pressure and temperature at the initial time. With the assimilation, the 24-h (48-h) track prediction of 11 (10) out of the 12 typhoons is improved. The 24-h (48-h) prediction of typhoon intensity is also improved in 10 (9) of the 12 cases. These experiments therefore demonstrate that assimilation of the QuikSCAT sea-wind data can increase the accuracy of typhoon track and intensity predictions through modification of the initial fields associated with the typhoon.     

Chemical characteristics of haze during summer and winter in Guangzhou

Airborne particles were collected with a 10-stage MOUDI and a PM₁₀ sampler in Guangzhou, China, during both haze and normal days in the summer of 2002 and 2003, and winter 2002. The characteristics of PAHs, organic carbon, elemental carbon and water-soluble inorganic ions were studied under four periods (summer normal, summer haze, winter normal and winter haze). In this study, secondary pollutants (OC, SO₄²⁻, NO₃⁻ and NH₄⁺) were the major chemical components and appeared to show a remarkably rapid increase from normal to haze days. The particle mass size distributions were bimodal and dominated by fine particles in haze days. A significantly higher OC/EC ratio was found in haze days (3.2–4.7) compared to normal days (1.8–2.8), indicating secondary organic aerosol formation might be significant during haze days. Correlation analysis between visibility and chemical species showed that the major scattering species were TC (total carbon) and sulfate in normal days and nitrate and TC in haze days, respectively. Simultaneously, correlation analysis between visibility and meteorological factors demonstrated that visibility increased with both temperature and wind speed, while it decreased with relative humidity. Furthermore, the relatively higher value of IcdP/(BghiP + IcdP) and the low value of Cmax, CPI, and BghiP/BeP in winter haze could be due to the growth of motor vehicle usage and energy consumption in winter.