Outline of a small unmanned aerial vehicle (Ant-Plane) designed for Antarctic research

As part of the Ant-Plane project for summertime scientific research and logistics in the coastal region of Antarctica, we developed six types of small autonomous UAVs (unmanned aerial vehicles, similar to drones; we term these vehicles ‘Ant-Planes’) based on four types of airframe. In test flights, Ant-Plane 2 cruised within 20 m accuracy along a straight course during calm weather at Sakurajima Volcano, Kyushu, Japan. During a period of strong winds (22 m/s) at Mt. Chokai, Akita Prefecture, Japan, Ant-Plane 2 maintained its course during a straight flight but deviated when turning leeward. An onboard 3-axis magneto-resistant magnetometer (400 g) recorded variations in the magnetic field to an accuracy of 10 nT during periods of calm wind, but strong magnetic noise was observed during high winds, especially head winds. Ant-Plane 4-1 achieved a continuous flight of 500 km, with a maximum flight altitude of 5690 m. The Ant-Plane can be used for various types of Antarctic research as a basic platform for airborne surveys, but further development of the techniques employed in takeoff and landing are required, as well as ready adjustment of the engine and the development of small onboard instruments with greater reliability.     

城镇化区域无人机低空航路网迭代构建的理论体系与技术路径

由于低空环境复杂,当前以无人机为应用主体的低空空域资源开发安全性和利用效率较低。而随着无人机数量的迅猛发展和商业化应用的快速扩张,旺盛的飞行需求与有限的飞行空间在低空的矛盾日益突出,如何安全、高效地管理无人机低空活动成为突出问题。目前各国都在探索解决途径,其中无人机低空航路是一种由中国科学院率先提出并得到业界和中国民用航空局认可的无人机低空交通和低空资源高效利用的综合解决方案。然而,这一概念还处在探索阶段,如何构建还不太明晰,尤其是对于地表环境复杂和高动态变化的城镇化区域,如何快速获取高精度的地理信息以满足无人机安全、高效飞行也是一大难题。鉴于遥感技术在航路的敏感信息提取与深化处理方面呈现出良好的应用前景,本文提出一种基于遥感和地理信息技术的城镇化区域低空公共航路网的高效迭代构建方法,并从理论支撑和已有研究基础论证了该方法的可行性。该研究技术路径主要包括基于地面路网生成具有多高度层的I级航路网,以充分利用地面交通设施;利用航路正约束地理要素生成II级航路网,如沿路的城市绿地和水域;规避负约束地理要素构建III级航路网,主要包括建筑物、通信盲区和电力线（杆）等;最后,通过仿真飞行和实际飞行测试分别生成IV、V级航路网,通过实际量测对比分析来检验无人机飞行的环境地图,保证飞行的安全性。以上方法基于遥感、地理信息、航空、交通等交叉学科解决无人机低空运行难题,为构建无人机低空航路网提供了一种新思路。更进一步讲,本文在低空领域运用地理学方法构建无人机航路网,是继无人机遥感应用之后无人机在地理学应用的又一大突破,同时也拓展了地理学的研究范畴,必将推动地理科学发展。     

Use of camera traps to determine dispersal of tigers in semi-arid landscape,western India

Dispersal is a life history trait that plays a key role in population dynamics. We used camera traps to estimate the distance male and female tigers (Panthera tigris) dispersed from Ranthambhore Tiger Reserve (RTR) in semi-arid habitats of western India from 2003 to 2010. We deployed camera traps whenever tiger tracks were found in places adjacent to protected areas where tigers had not been recently reported. We identified tigers by matching strip patterns by using their photographs with the database of camera-trapped tigers of RTR at the Wildlife Institute of India, Dehradun. We determined the aerial distance (straight line) between the last location of photo-capture in the natal area (in RTR) and the location of the most recent photo-capture. One female and three male tigers that dispersed from RTR were identified from photographs. The longest distance dispersed by a tiger was 148.4 km, and the average dispersed distance was 124.2 ± 23.7 km (n = 3) for male tigers and 78.4 km for the female tiger. The minimum age of the male tigers when they dispersed was 24 months. These data are important for making conservation and management decisions for restoration of potential connectivity between landscapes.     

地理信息技术应用下的无人机云端管理系统发展

日益增长的无人机飞行需求与有限的低空空域之间的矛盾愈发激烈,世界各国都在推进无人机管控政策和技术手段研究,即便在最自由的美国G类非管制空域,管理当局也在制定更为严格的无人机管控措施。无人机云端管理系统作为一种新型的数字化监管手段,其系统建设框架和技术路线得到了国内外学者和监管部门的广泛关注与研究。地理信息技术作为云端管理系统的应用技术之一,具体体现在以下几方面:利用全球导航卫星系统(GNSS)实现无人机精准空间定位;通过遥感技术(RS)获取影响无人机飞行安全的地理约束要素信息;基于地理信息系统(GIS)对低空地理空间数据进行组织管理以及构建低空虚拟地理环境等。论文结合团队在无人机低空应用上的研究进展,指出地理信息技术可以在云端管理和航路规划方面为无人机运行管理提供解决方案。     

Quantitative Analysis of Scale of Aeromagnetic Data Raises Questions About Geologic-Map Scale

A recently published study has shown that small-scale geologic map data can reproduce mineral assessments made with considerably larger scale data. This result contradicts conventional wisdom about the importance of scale in mineral exploration, at least for regional studies. In order to formally investigate aspects of scale, a weights-of-evidence analysis using known gold occurrences and deposits in the Central Lapland Greenstone Belt of Finland as training sites provided a test of the predictive power of the aeromagnetic data. These orogenic-mesothermal-type gold occurrences and deposits have strong lithologic and structural controls associated with long (up to several kilometers), narrow (up to hundreds of meters) hydrothermal alteration zones with associated magnetic lows. The aeromagnetic data were processed using conventional geophysical methods of successive upward continuation simulating terrane clearance or ‘flight height’ from the original 30 m to an artificial 2000 m. The analyses show, as expected, that the predictive power of aeromagnetic data, as measured by the weights-of-evidence contrast, decreases with increasing flight height. Interestingly, the Moran autocorrelation of aeromagnetic data representing differing flight height, that is spatial scales, decreases with decreasing resolution of source data. The Moran autocorrelation coefficient scems to be another measure of the quality of the aeromagnetic data for predicting exploration targets.     

基于多类型无人机数据的红树林遥感分类对比

使用固定翼无人机、消费级旋翼无人机和专业级旋翼无人机获取广东珠海淇澳岛红树林保护区多类型无人机遥感影像,使用基于面向对象分类的K-最近邻与随机森林分类器对研究区影像进行红树林树种精细分类和对比分析,并探讨了不同类型无人机平台在红树林资源调查应用中的优缺点。结果表明：1）固定翼无人机、消费级旋翼无人机和专业级旋翼无人机数据使用K-最近邻法的分类精度分别为：73.8%、72.8%和79.7%;使用随机森林法的分类精度分别为：81.1%、84.8%和89.3%。3种平台类型的无人机数据均适用于红树林精细分类研究,对于无人机红树林遥感数据,随机森林的分类方法优于K-最近邻方法。2）以拍摄面积与用时之比估算采集效率,固定翼无人机、消费级旋翼无人机和专业级旋翼无人机分别为0.036、0.013和0.003 km2/min。固定翼无人机的采集效率具有明显优势。3）固定翼无人机适合大范围红树林数据采集,要求较高;消费级旋翼无人机适于获取小范围精细数据,成本低且易学易用;专业级旋翼无人机适合搭载质量稍大的如成像光谱仪、LiDAR等专业传感器获取多源数据。最后给出了无人机在红树林遥感研究中的注意事项和建议。     

Paleo‐fluid expulsion and contouritic drift formation on the Chatham Rise,New Zealand

The Chatham Rise is located offshore of New Zealand's South Island. Vast areas of the Chatham Rise are covered in circular to elliptical seafloor depressions that appear to be forming through a bathymetrically controlled mechanism, as seafloor depressions 2–5 km in diameter are found in water depths of 800–1100 m. High‐resolution P‐Cable 3D seismic data were acquired in 2013 across one of these depressions. The seafloor depression is interpreted as a mounded contourite. Our data reveal several smaller buried depressions (<20–650 m diameter) beneath the mounded contourite that we interpret as paleo‐pockmarks. These pockmarks are underlain by a complex polygonal fault system that deforms the strata and an unusual conical feature results. We interpret the conical feature as a sediment remobilization structure based on the presence of stratified reflections within the feature, RMS amplitude values and lack of velocity anomaly that would indicate a nonsedimentary origin. The sediment remobilization structure, polygonal faults and paleo‐depressions are the indicators of the past subsurface fluid flow. We hypothesize that the pockmarks provided the necessary topographic roughness for the formation of the mounded contourites thus linking fluid expulsion and the deposition of contouritic drifts.     

无人机低空飞行障碍物环境风险评估方法研究——以京津新城为例

无人机应用日益广泛,但随着城市环境建设的不断推进,无人机在城市中安全运行的问题也日益突出,因此无人机低空障碍物环境风险评估成为无人机领域研究的关键问题之一。论文按照不同类型无人机及运行高度将低空空域划分为微型、轻型和小型无人机风险评估区域,在充分考虑无人机自身形状大小、运动约束以及障碍物约束等条件的基础上,提出一种近似点扩张算法,基于障碍物原始边界生成扩张边界,并将其作为低空飞行环境中高风险与低风险之间的风险过渡区。以京津新城为例,分别提取不同风险评估区内的障碍物要素,并基于风险评估技术生成面向微型、轻型和小型无人机多高度层的低空飞行障碍物环境风险地图,按其对无人机威胁程度分为高风险区、高风险过渡区、中风险区和低风险区。实验结果表明:研究区内微型、轻型、小型无人机风险评估区内的风险过渡区分别占10.9%、7.3%、9.0%,该方法可以在考虑无人机与障碍物相互影响的基础上,计算飞行区域内无人机潜在碰撞风险区域,实现对低空障碍物环境风险的科学有效评估,为不同机型的无人机在飞行区域内的可航行性提供科学参考。     

Array analysis using circular-wave-front geometry:an application to locate the nearby seismo-volcanic source

The zero-lag cross-correlation technique, used for array analysis in the hypothesis of plane waves, has been modified to allow the wave front to be circular. Synthetic tests have been performed to check the capability of the method, which returns the input test data when the source–array distances are not greater than two or three times the array aperture. For this distance range the method furnishes an estimate of the apparent velocity and the epicentral coordinates of the source. For more distant sources the method becomes equivalent to that based on the planar-wave approximation, which gives an estimate of the backazimuth to the source and the apparent velocity. The method has been applied to seismic data recorded at the active volcano located at Deception Island, Antarctica. 35 volcanic long-period events occurring in a small swarm were selected. Results show that the epicentres are close to the array (between 0.4 and 2 km) and aligned in a SW direction, in agreement with one of the main directions of the fracture system of Deception volcano.     

西南极利文斯顿岛火山岩多种成因过程的地球化学证据

利文斯顿岛火山岩是南极南设得兰岩浆弧的一部分。对岩石的Ｓｒ、Ｎｄ、Ｐｂ同位素组成以及８７Ｓｒ／８６Ｓｒ与１／Ｓｒ、Ｒｂ、Ｋ和ＳｉＯ２关系的研究表明,利文斯顿岛火山岩具有不同的源区特征。百耳斯半岛和史莱夫角的火山岩、西多斯角的粗玄岩和第三纪的英云闪长岩显示出同成因的特点,和依诺特角第四纪橄榄玄武岩一样,它们均具有原生地幔的同位素组分,源区岩浆可能直接来自上地幔。汉那角和中利文斯顿岛火山岩岩浆则受到地壳成分的混染。不相容元素对Ｌａ／Ｓｍ－Ｌａ和Ｃｅ／Ｙｂ－Ｃｅ的研究进一步显示出,上述不同产地的岩石分别为不同源岩浆不同程度部分熔融的产物。结合岩相学和岩石化学特征的研究,提出百耳斯半岛和史莱夫角的火山岩以及西多斯角的粗玄岩是上地幔发生部分熔融所生成的玄武岩岩浆从深部岩浆囊沿构造薄弱带直接喷出形成的。古生代基底岩系的存在对中利文斯顿岛和汉那角火山岩的成因过程有重要的影响,即来自深部岩浆囊的原始岩浆在上地壳中的浅部岩浆囊受到了壳源物质混染。更新世－现代火山岩的源区岩浆直接自上地幔部分熔融生成,火山作用与晚新生代时该区的拉张构造有关。     

Tectonic geomorphology of the San Andreas Fault zone from high resolution topography: An example from the Cholame segment

High resolution topographic data along fault zones are important aids in the delineation of recently active breaks. A 15 km-long portion of the south-central San Andreas Fault (SAF) along the southern Cholame segment contains well preserved tectonic landforms such as benches, troughs, scarps, and aligned ridges that indicate recurring earthquake slip. Recently acquired LiDAR topographic data along the entire southern SAF (“B4” project) have shot densities of 3–4 m^− 2. Computed from the LiDAR returns, Digital Elevation Models (DEMs) of 0.25 to 0.5 m resolution using local binning with inverse distance weighting and 0.8 m or larger search radii depict the tectonic landforms at paleoseismic sites well enough to assess them confidently. Mapping of recently active breaks using a LiDAR-only based approach compares well with aerial photographic and field based methods. The fault zone varies in width from meters to nearly 1 km and is comprised of numerous en echelon meter to kilometer-length overlapping sub parallel fault surfaces bounding differentially moving blocks that elongate parallel to the SAF. The semantic variations of what constitutes “active” and the importance of secondary traces influence the breadth and complexity of the resulting fault trace maps.     

无人机遥感组网冗余容错的研究

针对无人机在遥感遥测领域组网过程中存在的随机故障,进而导致无人机在任务执行过程中任一约束的及时响应缺失,将会影响任务总体结果或导致整个任务部分及完全失败的问题,论文提出无人机遥感组网冗余容错方法。该方法采用领航—跟随的无人机编队飞行模式,多台组网无人机稳定可靠完成指定的飞行任务,验证了冗余容错方法,解决了无人机遥感组网冗余容错技术中的有和无的问题。     

西南极利文斯顿岛火山岩地质

本文综合近年研究中新获得的资料和证据，对利文斯顿岛火山岩的地质特征和火山作用特点作了综合性的介绍。百耳斯建造是该岛最老的火山岩地层，由晚侏罗世至早白垩世生成的玄武岩、玄武安山岩质熔岩和火山碎屑岩、集块岩以及泥岩、页岩等组成，分布在岛西部的百耳斯半岛。中白垩世的鲍勒斯山组主要出露在岛的中部，是由安山岩质熔岩和火山碎屑岩夹层组成的一套蚀变火山岩系。汉那角剖面的火山碎屑岩和熔岩及史莱夫角的橄榄玄武岩均具有中白垩世的年龄。晚白垩世火山活动的产物以粗玄岩为代表，集中出露在西多斯角一带。伴随着火山活动，始新世英云闪长岩侵入白垩系火山岩地层。更新世至现代则有依诺特角组橄榄玄武岩在岛的东北部产出。上述火山活动随时间演进而自北西向南东不断迁移的特点，与整个南设得兰群岛火山作用的发展趋势相符。岩石化学和地球化学资料表明，百耳斯半岛熔岩、史莱夫角的橄榄玄武岩和西多斯角的粗玄岩等白垩纪火山岩基本属于钙碱性岩系并且具有低钾低镁的特点。早第三纪的英云闪长岩继承了橄榄玄武岩和粗玄岩的成分特点，同是南设得兰群岛岩浆弧中生代－新生代火山作用的产物，在钙碱性岩系岩浆演化的晚期生成。而鲍勒斯山组的熔岩和汉那角的熔岩表现出岩相学和岩石化学性质上的     

Evidence of urban-induced precipitation variability in arid climate regimes

The study employs a 108-year precipitation historical data record, global climate observing network observations and satellite data to identify possible anomalies in rainfall in and around two major arid urban areas, Phoenix, Arizona and Riyadh, Saudi Arabia. The analysis reveals that during the monsoon season, locations in northeastern suburbs and exurbs of the Phoenix metropolitan area have experienced statistically significant increases in mean precipitation of 12–14% from a pre-urban (1895–1949) to post-urban (1950–2003) period. Further analysis of satellite-based rainfall rates suggests the existence of the anomaly region (AR) over a 7-year period. The anomaly cannot simply be attributed to maximum topographic relief and is hypothesized to be related to urban-topographic interactions and possibly irrigation moisture. Temperature records suggest that Riyadh has experienced an adjustment in mean temperature in response to the growth of urban surfaces (e.g. the so-called urban heat island effect). While ground-based precipitation records also indicate an upward trend in mean and total precipitation in and around Riyadh in the last 10–15 years, it is difficult to attribute the increase to urbanization because other less urbanized stations in Saudi Arabia also show a similar increase. Recent satellite-based precipitation estimates indicate an AR 50–100 km north of Riyadh, but this study is not robust enough to conclusively link it to urbanization although certain climate-regime attributes suggests that it might be.     

Diatom response to mid-Holocene climate change in Lago di Massaciuccoli (Tuscany,Italy)

A sedimentary sequence from the Mediterranean coastal basin of Lago di Massaciuccoli (Tuscany, Italy) was analyzed for diatoms, covering two periods over the past ca. 7,000 years. The site was selected because it is situated in a sensitive position at the limit between Mediterranean and Central European climates and biomes. Our focus is on the impact of accelerated human activity during the recent past (water uptake in the catchment, sand extraction, wastewater discharge) and on a phase of evident change between 6,600 and 5,400 cal. BP. The diatom record suggests fresh-water conditions and rather high lake levels until ca. 6,000 years ago. The subsequent shift towards brackish conditions peaked at around 5,500 cal. BP. We relate this shift to a pervasive change towards a drier climate that has been observed elsewhere in the Mediterranean and Northern African regions, and stands in contrast to the shift towards a cooler and more humid climate in the nearby Alps (200–350 km distant) and in central Europe. Pollen and charcoal records from a previous study on the same sedimentary sequence were used to gain additional insights about the causes of the changes in the diatom assemblages and apply numerical methods to search for common trends and correlations.     

Local physiographic controls on the responses of Arctic lakes to climate warming in Sirmilik National Park,Nunavut, Canada

Twenty high Arctic lakes and ponds were sampled for water chemistry and modern diatom assemblages in two distinct physiographic sectors of Sirmilik National Park, Nunavut, Canada. Sites on southwestern Bylot Island were warmer, more alkaline, less dilute, and had higher concentrations of nutrients, DOC and Chl-a (mesotrophic to oligo-mesotrophic), whereas sites on Qorbignaluk Headland on northern Baffin Island were deeper, very dilute, mostly oligotrophic and had lower pH. Diatom assemblages differed markedly between these two regions as a consequence of limnological differences between them. Paleolimnological records, spanning > 200 years and dated by ²¹⁰Pb activity, were produced from each region to compare biological responses to recent warming inferred from glaciological studies on Bylot Island and regional syntheses for the Arctic. Diatom assemblages began to change around AD 1900 at both sites. At Qorbignaluk Headland, marked shifts in diatom community composition occurred during the twentieth century, with large increases in the abundance of planktonic diatoms. At Bylot Island, diatom community changes began around the same time, and involved modest decreases in planktonic diatoms and increases in inferred specific conductance, likely because of a decrease in the areal extent of the small lake as a response to warming. The study confirms that responses of freshwater ecosystems to climate warming vary depending on local physiographic factors.     

南极拜尔斯半岛企鹅粪土沉积物元素地球化学特征

拜尔斯半岛位于南极利文斯顿岛最西部,是南设得兰群岛中最大的无冰区。对采自拜尔斯半岛的一根长55 cm的企鹅粪土沉积柱P1进行了元素和同位素地球化学分析。通过对沉积物C/N、有机质来源和δ15N的分析,发现P1沉积剖面中有机质主要来源于企鹅粪。利用富集系数、相关性分析、主成分分析等统计分析方法,识别出该沉积剖面中P、F、Cu、Hg、As、S六种元素具有共同的来源,与企鹅粪的输入密切相关,并且这些元素与TOC和δ15N显著正相关,说明沉积剖面中这些元素含量主要受控于企鹅粪的输入程度。通过与长城站区阿德雷岛、东南极戴维斯站加德纳岛企鹅粪土沉积物的标型元素特征比较,发现上述三个地区的标型元素组合大体上一致,反映了整个南极地区企鹅粪土沉积物生物标型元素组合的共性。研究结果为进一步恢复该地区的企鹅种群数量演化,及其对气候变化的响应提供了可能。     

Tectonic and oceanographic process interactions archived in Late Cretaceous to Present deep‐marine stratigraphy on the Exmouth Plateau,offshore NW Australia

Deep‐marine deposits provide a valuable archive of process interactions between sediment gravity flows, pelagic sedimentation and thermohaline bottom‐currents. Stratigraphic successions can also record plate‐scale tectonic processes (e.g. continental breakup and shortening) that impact long‐term ocean circulation patterns, including changes in climate and biodiversity. One such setting is the Exmouth Plateau, offshore NW Australia, which has been a relatively stable, fine‐grained carbonate‐dominated continental margin from the Late Cretaceous to Present. We combine extensive 2D (~40,000 km) and 3D (3,627 km²) seismic reflection data with lithologic and biostratigraphic information from wells to reconstruct the tectonic and oceanographic evolution of this margin. We identified three large‐scale seismic units (SUs): (a) SU‐1 (Late Cretaceous)—500 m‐thick, and characterised by NE‐SW‐trending, slope‐normal elongate depocentres (c. 200 km long and 70 km wide), with erosional surfaces at their bases and tops, which are interpreted as the result of contour‐parallel bottom‐currents, coeval with the onset of opening of the Southern Ocean; (b) SU‐2 (Palaeocene—Late Miocene)—800 m‐thick and characterised by: (a) very large (amplitude, c. 40 m and wavelength, c. 3 km), SW‐migrating, NW‐SE‐trending sediment waves, (b) large (4 km‐wide, 100 m‐deep), NE‐trending scours that flank the sediment waves and (c) NW‐trending, 4 km‐wide and 80 m‐deep turbidite channel, infilled by NE‐dipping reflectors, which together may reflect an intensification of NE‐flowing bottom currents during a relative sea‐level fall following the establishment of circumpolar‐ocean current around Antarctica; and (c) SU‐3 (Late Miocene—Present)—1,000 m‐thick and is dominated by large (up to 100 km³) mass‐transport complexes (MTCs) derived from the continental margin (to the east) and the Exmouth Plateau Arch (to the west), and accumulated mainly in the adjacent Kangaroo Syncline. This change in depositional style may be linked to tectonically‐induced seabed tilting and folding caused by collision and subduction along the northern margin of the Australian plate. Hence, the stratigraphic record of the Exmouth Plateau provides a rich archive of plate‐scale regional geological events occurring along the distant southern (2,000 km away) and northern (1,500 km away) margins of the Australian plate.     

西南极利文斯顿岛中部中生代－新生代火山岩岩石化学研究

出露在利文斯顿岛中部的白垩纪火山岩为玄武岩－玄武安山岩－安山岩－英安岩组合，基本属于钙碱性系列，但具有低钾拉斑玄武岩的某些特点。岩石富集Ｒｂ、Ｔｈ、Ｂａ，轻度亏损Ｚｒ、Ｔｉ、Ｈｆ、Ｎｂ，较强亏损Ｃｒ和Ｎｉ，而且随着岩浆从基性向酸性成分的演化，富集（或亏损）程度加大。岩石的轻稀土元素中度富集，岩石的（Ｃｅ／Ｙｂ）ＣＮ比值较低。白垩纪火山岩形成在一个造山环境，是南设得兰岩浆弧的一部分。然而，在利文斯顿岛不同地区出露的岩石其化学性质有所区别，因此认为它们可能源于不同的岩浆体系。在晚古生代至早中生代，利文斯顿岛中部处于一个独特的浊积扇的构造环境。主要产在利文斯顿岛中部和汉那角的鲍勒斯山组火山岩与其它地点的中生代火山岩相比，无论岩相学特征还是岩石化学性质均有所不同。因此认为它们的产生同时受到太平洋板块的俯冲作用和该地构造位置所控制。史莱夫角的橄榄玄武岩成分中碱高硅低，并且通常表现出高铝的特点，这些性质与百耳斯半岛的玄武岩极为相似。区域上火山活动不断发展，活动中心逐渐向北东迁移，导致粗玄岩岩颈和岩席生成，最后是英云闪长岩的侵入。更新世至现代的依诺特角组橄榄玄武岩以化学成分中的低硅高碱含量区别于中生代火山岩。岩石的高Ｍ值     

南极欺骗岛土壤细菌群落结构和多样性分析

采用基于16S r DNA克隆文库的非培养方法和传统培养方法相结合的手段,对南极欺骗岛土壤细菌群落结构及多样性进行了初步分析。对来自16S r DNA克隆文库的118个阳性克隆进行测序和序列比对,结果显示细菌来自放线菌门(Actinobacteria)、变形杆菌门(Proteobacteria)和拟杆菌门(Bacteroidetes)3大门的39个操作分离单元(OTU),其中优势菌群为放线菌门和变形杆菌门,分别占65.25%和28.81%。放线菌门的主要优势属为鱼孢菌属(Sporichthya)、类诺卡式氏菌属(Nocardioides)、束缚菌属(Conexibacter)、Gaiella和节杆菌属(Arthrobacter)。变形杆菌门的主要优势属为鞘氨醇单胞菌属(Sphingomonas)、硫杆菌属(Thiobacillus)、寡养单胞菌属(Stenotrophomonas)和热单胞菌属(Thermomonas)。采用6种培养基对细菌进行培养和分离,共得到57株菌,来自放线菌门、变形杆菌门、拟杆菌门和厚壁菌门4大门的13个OTU,其中优势菌群为放线菌门和变形杆菌门,分别占57.89%和31.58%。优势属是放线菌门的节杆菌属(Arthrobacter)、雷夫松氏菌属(Leifsonia)和变形杆菌门的假单胞菌属(Pseudomonas)。本论文为研究欺骗岛土壤细菌多样性以及有益菌种资源的开发和利用奠定了基础。