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This thesis establishes constrained motion model and sensor model of a mobile robot to represent mobility and perceptivity, respectively, and defines the k step reachable region to describe the states that the robot may reach. We show that the calculation of the k step reachable region can be reduced from that of 2k reachable regions with the fixed motion styles to k + 1 such regions, and provide an algorithm for its calculation.

首先建立了移动机器人约束运动模型和传感器模型用于描述机器人的移动和感知,给出了可达定义,即机器人在有限步内可能到达的域,在此基础上证明了在k步不同运动模式下多达2k个可达的计算可以降为k+1个可达的计算,并提出了k步可达由k+1个扇形组成的计算算法。

Although both of FDRMADS7 and FDRMADS8 wereexpressed in the root, they have different expression pattern.The transcripts of FDRMADS7 weredetected throughout the root,especially the expression in the root meristem was the highest.However,the expression of FDRMADS8 was mainly localized in elongation and mature rigion.No apparent expression signal was detected in the root cap, root meristem and pericycle cells.

虽然FDRMADS7和FDRMADS8都在根中表达,但它们在根中的表达模式也不相同:FDRMADS7在根中到处表达,尤以生长点处表达量最高;而FDRMADS8在伸长和根毛的皮层中有大量表达,在根冠,根尖分生和根毛的中柱鞘细胞中却无明显表达,暗示它们在根中行使的功能也不相同。

Base on above studies, some conclusions were obtained as follows:(1) ore-forming background of the studied ferromanganese crusts are mainly controlled by intensity of Antarctic Bottom Waters and variations of material source;(2) it is confirmed that the ferromanganese crusts are mainly hydrogenetic and their composition are affected by volcanic and continental material simultaneously; there are no obvious phosphatization reconstruction and element reaction occurred in them, so they have important paleoceanological significance;(3) from researches on element occurrence modes in the new-type ferromanganese crusts and the lying sediments, it is proposed that there is no great biological affection on the crusts formation and their composition mainly came from the adsorptive action of the ferromanganese oxides in them;(4) two major types of ore-controlling factors are identified through compilation of ore-controlling factors, which are geological and oceanic factors;(5) considering the long-term variation trends of the crusts composition, combing the U-series and 10Be isotope dating results, it is proposed that the ore-forming processes of ferromanganese crusts in the studied areas can be divided into three major stages (5.6~2.8 Ma, 2.8~2.7 Ma and since 2.7 Ma), and then the activities of AABW since the Late Miocene, changes of input flux coming from volcanic and continental material are confirmed.

通过研究,得出如下结论:(1)研究铁锰结壳的成矿背景主要受控于南极底流强弱及物源供给的变化;(2)证实铁锰结壳主要为水成成因,同时其物质组成也受一定程度的火山和陆源物质的影响;结壳自形成以来没有遭受到明显的磷酸盐化等成岩后期改造和元素再迁移,具有重要的古海洋学意义;(3)通过新型铁锰结壳及下伏沉积物元素赋存状态的研究,认为生物作用对研究结壳的形成并没有很大的直接影响,其物质成分主要来自于结壳中铁锰氧化物的吸附作用;(4)在控矿要素的研究中,归纳出了地质与海洋两大类结壳控矿要素;(5)根据结壳成分长周期变化趋势,结合铀系和10Be测年结果,将研究结壳的形成过程划分为三个主要阶段(5.6~2.8 Ma,2.8~2.7 Ma和2.7 Ma以来),并确定了晚中新世以来研究南极底流的活动情况、火山和大陆来源物质输入量的变化。

Furthermore,in order to obtain the best energy saving,Sushi Jet has three independent heat chambers of temperature control ,each of which can be set whether to work or not in the production run according to the operational method of screen printing and identity of ink .Testing data shows that it only needs to open two sets of heat chambers when drying water- based binder under 120 ℃,and the average energy consumption costs is only 10 yuan / hour. In the plastisol ink drying process,the cost of the average energy consumption is less than 25 yuan / hour with opening three groups.

另外,Sushi Jet型燃气炉具备三组独立控温的烘可根据印花工艺、油墨原料特性减少开启烘,从而达到最佳节能效果,经检验数据表明在烘干水性普通胶浆时,仅需开启两组烘。120℃下平均能耗成本,仅为10元/小时,热固油墨的烘干过程,在开启三组烘,160℃下的平均能耗成本低于25元/小时。

Results Of 61 cases, 4 cases (7%) in center 3 mm zone of cornea had mean thickness:(0.439±0.071) mm and polar distance:(3.108±0.904) nun; 8 cases (13%) in 3~5 mm zone had T:(0.328±0.088) mm and p:(3.108±0.904) mm; 28 cases (46%) in 5~7 mm zone had T:(0.320±0.093) mm and p:(3.233±0.381) mm; 21 cases (34%) in 7~9 mm zone had T:(0.340±0.128) mm and p:(3.756±0.539) mm; 61 cases (100%) in 0~9 mm zone had T:(0.336±0.112) mm and p:(3.108±0.904) mm.

结果 61例角膜最薄点平均厚度为(0.336±0.112)mm且平均极距为(3.108±0.904)mm;其中最薄点分布,角膜中央3mm4例(7%)T为(0.439±0.071)mm且p为(3.108±0.904)mm;角膜3~5mm8例(13%)T为(0.328±0.088)mm且p为(3.108±0.904)mm;角膜5~7mm28例(46%)T为(0.320±0.093)mm且p为(3.233±0.381)mm;角膜7~9mm21例(34%)T为(0.340±0.128)mm且p为(3.756±0.539)mm。

We selected 15 representative floras from different climatic zones from north to south, and did DCA ordination between the Reserve flora and them. It showed that both spermatophyte flora and pteridophyte flora of the Reserve were more close to some southern floras, which located in much lower latitudes.

将之与我国不同气候带15代表性地点的植物系进行DCA排序,发现其种子植物系与蕨类植物系组成都与更低纬度的一些系更相近,表现出强烈的热带残遗性和亲缘性。

Through many years' development and construction, the infrastructure of QFTZ has already reached the domestic first-class level, such as power supply, telecommunication, water purveyance, water draining, sewage draining, heat supply and vapor supply; the complete infrastructure and commercial environment has formed; QFTZ is the first which has passed both ISO9001 and ISO14001. Being the first "Non-charge Zone","Garden-like Invest Model Zone" and the pilot area of "the Integration of the Port and the Zone", QFTZ has become the forerunner of opening up to the outside world, the experimental area of system innovation, the demonstration area of scientific and technical innovation, the radiation driving area of flow economy of Shandong.

经过多年的开发建设,青岛保税基础开发已基本完成,域功能培育取得明显突破,供电、通讯、供排水、供热、供汽等基础硬件设施均已达到国内一流水平,形成了完备的基础设施和商务环境,率先通过ISO9001质量管理体系和ISO14001环境管理体系双认证,建成了山东省第一个投资"无费"和花园式投资示范,"港联动"试点域之一,成为山东省对外开放的先行、体制创新的实验、科技创新的示范、流量经济的辐射带动

Monitoring scope was divided to 3 zones including radioactive source, operating and denuded, all monitoring results were recorded and archived.

将监测范围划分放射源、操作和清洁共3个,监测结果记录存档。

Lastly, sand and reef area were compared. Since reef areas has more suitable natural substratum than sand areas.

另外由较大的空间尺度来看,礁与砂为两个天然底质不同的域,在这两个域分别放置面积相同的附苗板时,由於礁的天然底质数量较多,根据附苗强化效应,幼生在附苗板上的附苗密度应在砂较高。

The intensification phenomenon at 1-meter scale was not found. The larval density in water column might be highly heterogeneous even in very small scale. On the other hand, we consistently found higher settlement density in sand areas than in reef areas. This phenomenon may well have been caused by the intensification

本研究结果在1公尺的空间尺度下并没有发现附苗强化现象,但是礁的附苗密度却如预期低於砂,推测可能是1公尺空间尺度内幼生数量过於不均匀,相差5倍的附苗板面积不足以造成幼生附苗密度的变异,而礁与砂则由於面积相差相当大因此可以发现附苗强化现象。

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