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2007年07月31日太空资讯

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Japanese And Nasa Satellites Unveil New Type Of Active Galaxy

An international team of astronomers using NASA’s Swift satellite and the Japanese/U.S. Suzaku X-ray observatory has discovered a new class of active galactic nuclei (AGN). By now, you’d think that astronomers would have found all the different classes of AGN – extraordinarily energetic cores of galaxies powered by accreting supermassive black holes. AGN such as quasars, blazars, and Seyfert galaxies are among the most luminous objects in our Universe, often pouring out the energy of billions of stars from a region no larger than our solar system.

But by using Swift and Suzaku, the team has discovered that a relatively common class of AGN has escaped detection…until now. These objects are so heavily shrouded in gas and dust that virtually no light gets out.

"This is an important discovery because it will help us better understand why some supermassive black holes shine and others don’t," says astronomer and team member Jack Tueller of NASA’s Goddard Space Flight Center in Greenbelt, Md.

Evidence for this new type of AGN began surfacing over the past two years. Using Swift’s Burst Alert Telescope (BAT), a team led by Tueller has found several hundred relatively nearby AGNs that were previously missed because their visible and ultraviolet light was smothered by gas and dust. The BAT was able to detect high-energy X-rays from these heavily blanketed AGNs because, unlike visible light, high-energy X-rays can punch through thick gas and dust.

To follow up on this discovery, Yoshihiro Ueda of Kyoto University, Japan, Tueller, and a team of Japanese and American astronomers targeted two of these AGNs with Suzaku. They were hoping to determine whether these heavily obscured AGNs are basically the same type of objects as other AGN, or whether they are fundamentally different. The AGNs reside in the galaxies ESO 005-G004 and ESO 297-G018, which are about 80 million and 350 million light-years from Earth, respectively.

Suzaku covers a broader range of X-ray energies than BAT, so astronomers expected Suzaku to see X-rays across a wide swath of the X-ray spectum. But despite Suzaku’s high sensitivity, it detected very few low- or medium-energy X-rays from these two AGN, which explains why previous X-ray AGN surveys missed them.

According to popular models, AGNs are surrounded by a donut-shaped ring of material, which partially obscures our view of the black hole. Our viewing angle with respect to the donut determines what type of object we see. But team member Richard Mushotzky, also at NASA Goddard, thinks these newly discovered AGN are completely surrounded by a shell of obscuring material. "We can see visible light from other types of AGN because there is scattered light," says Mushotzky. "But in these two galaxies, all the light coming from the nucleus is totally blocked."

Another possibility is that these AGN have little gas in their vicinity. In other AGN, the gas scatters light at other wavelengths, which makes the AGN visible even if they are shrouded in obscuring material.

"Our results imply that there must be a large number of yet unrecognized obscured AGNs in the local universe," says Ueda.

In fact, these objects might comprise about 20 percent of point sources comprising the X-ray background, a glow of X-ray radiation that pervades our Universe. NASA’s Chandra X-ray Observatory has found that this background is actually produced by huge numbers of AGNs, but Chandra was unable to identify the nature of all the sources.

By missing this new class, previous AGN surveys were heavily biased, and thus gave an incomplete picture of how supermassive black holes and their host galaxies have evolved over cosmic history. "We think these black holes have played a crucial role in controlling the formation of galaxies, and they control the flow of matter into clusters," says Tueller. "You can’t understand the universe without understanding giant black holes and what they’re doing. To complete our understanding we must have an unbiased sample."

Planetary Society Set To Launch First Library Of Mars

The Planetary Society’s silica-glass DVD is ready to launch to Mars on board Phoenix, NASA’s newest Scout mission led by Principal Investigator Peter Smith at the University of Arizona. Attached to the deck of the Phoenix lander, the DVD includes Visions of Mars, a collection of 19th and 20th century stories, essays and art inspired by the Red Planet, as well as the names of over a quarter million inhabitants of Earth. The disk will appear in some of the calibration images that Phoenix sends back from the Martian surface.

"Since The Planetary Society’s disk should last for centuries on Mars, we hope astronauts at some future date will enjoy the visionary works we have sent in this first Martian library," said Louis Friedman, Executive Director of The Planetary Society, who conceived the idea for Visions of Mars. "These tales and images have inspired generations about the wonder of space, including many men and women who are now researchers and engineers in the space program."

This first library on Mars contains materials that represent 20 nations and cultures. Visions of Mars includes works by The Planetary Society’s co-founder Carl Sagan, Isaac Asimov, Ray Bradbury, Kim Stanley Robinson, Arthur C. Clarke, Percival Lowell and many more.

Phoenix will be the first lander to explore the Martian arctic, landing near 70 degrees north latitude. Designed to search for and study water ice, the spacecraft is a fixed lander with a suite of advanced instruments and a robotic arm that can dig up to half a meter into the soil. The Phoenix team hopes to uncover clues in the icy soil of the Martian arctic about the history of near surface ice and the planet’s potential for habitability. Tune into a Planetary Radio interview about Phoenix with Peter Smith.

The first possible launch date for Phoenix is August 3, 2007, with a landing slated for 2008.

This will be The Planetary Society’s second attempt to send Visions of Mars to its namesake planet. It was originally created by the Society to launch aboard Russia’s Mars 96 spacecraft, which failed shortly after launch. The library has been updated and risen from the ashes for its Phoenix flight. It should be able to last at least 500 years on Mars, so there will be plenty of time for a future generation to discover and enjoy the works included on the DVD.

The Phoenix Mission is led by Principal Investigator Peter H. Smith of the University of Arizona, with project management at NASA’s Jet Propulsion Laboratory and a development partnership with Lockheed Martin Space systems. International contributions for Phoenix are provided by the Canadian Space Agency, the University of Neuchatel (Switzerland), the University of Copenhagen, and the Max Planck Institute in Germany.

 

 

Fossil Hunting On Mars

To date, only NASA has succeeded in sending a rover to explore our neighboring planet Mars. That is about to change. In 2011, the European Space Agency will send ExoMars to the Red Planet in search of signs that Mars is, or was, a living world. Astrobiology Field Research Editor Henry Bortman recently interviewed the ExoMars project scientist, Jorge Vago. In this, the second part of a two-part interview, Vago explains why ExoMars will focus on looking for fossil evidence of ancient life and why such evidence may be easier to find on Mars than it is on Earth.

Astrobiology Magazine: It’s my understanding that the instruments on ExoMars will be looking for biomolecules typical of terrestrial life. You don’t plan to look for indicators or patterns that could be caused by biology with a different chemical basis than that of terrestrial life. Is it true that ExoMars will focus on looking for Earth-like life, and if so, why?

Jorge Vago: Well, there are two answers to that. One is that, in reality, what we’re looking for is organic molecules, carbon-based. And that is of course based on what we know about life on Earth. The other thing we do know for sure is that there has been a very large exchange of meteoritic material between the two planets. So we can be pretty sure that Mars was in some way seeded with organic matter that came from Earth in the early period of the planet. Would this give rise to life on Mars as we know it or not? – well, I don’t know.

On the other hand, we know that carbon is a very able atom when it comes to producing complex molecules, under the thermodynamic conditions that we know to prevail on Earth and on other terrestrial planets, including Mars. We have no evidence that point to more exotic chemistry being active on Mars. And when you have to design a mission, you have to be practical. So we go for the things we know. If we don’t find any organics – we should at least be able to find the organics that we know are delivered to Mars daily by cometary and meteoritic dust – if we don’t find that, even in the subsurface, then at that point we will have moved the bar for trying to find life on Mars much, much higher. The next mission that will try this will have to probably go much, much deeper.

AM: Finding fossil life is also tricky. There’s a lot of debate about the oldest fossils on Earth, in which there are supposedly traces of life. There are questions about what you can really see, how easy it is to distinguish ancient fossils from the effects of purely chemical processes, what are reliable biomarkers. If it’s that hard to find ancient life on Earth, how are you going to do it on Mars?

JV: Well, actually, it might be easier to find reliable biomarkers for very ancient life on Mars than on Earth. Because on Earth you have had all these plate-tectonics and reformation processes and volcanism that have made it extremely hard for us to find old rocks, older than 3.5 billion years, where you can say, Yeah, I’m looking at a rock that is more or less in the same state it was in when it was formed 3.5 billion years ago. This is simply not possible on our planet. Now Mars seems to have gone into a dormant stage very early in its history, so it is likely – and this will depend, of course, on our landing site – that we can access a place that is very, very old, where the rocks will be more or less in the same state that they were in when they were deposited there, 3.5 or even 4 billion years ago. What are we going to find there? Nobody knows. But chances are that whatever organics might be encased in those rocks will be in a much better state than you would hope to find in Earth rocks of a similar age.

AM: You’re developing the capability to look both for extant life and for fossil life. How do you find a landing site that provides you with both opportunities?

JV: That would be very, very hard. My guess is that we will target some formation that we can definitely say is related to the past presence of water on old Mars. A site that may be of more interest for present life, is one where the Odyssey gamma-ray spectrometer indicates there may be water ice within one meter from the surface. Off course, water ice doesn’t mean there’s life there. It’s really, really cold, but it’s interesting. If anybody were to find some sort of heat in the next couple of years associated with the presence of water ice, then that would be interesting for a possible site for present life. I would say that from the point of view of the objectives of the mission, if we want to maximize the chances of finding something, the priority will be on targeting fossil life, or past life. And if we can get to a site that also has the potential for present life, that would be a bonus.

AM: Do you think Mars is, or ever was, a living world? What do you expect ExoMars to find?

JV: What I would like to answer with this mission is the question of where are the organics that we know should be there from the meteoritic delivery, and I think we have the instrumentation to do that. Hopefully these oxidants do not extend so deep into the subsurface that we are unable to find anything.

Now, regarding the possible emergence of life on Mars, I think if it happened, it happened very early, more or less at the same time when it did on Earth, and it will be very, very hard to prove with a single mission that there was life on Mars. But maybe we can at least plant a seed with this mission, and find a few strong indications that there could have been life there. To establish for sure that there was life on Mars may require more than one mission. But we can get started, and that would be a good thing.

Endeavour Marches Toward Launch

Space Shuttle Endeavour is ready to fly, NASA managers concluded July 26 after wrapping up the two-day flight readiness review at Kennedy Space Center in Florida. Launch of Endeavour on the STS-118 mission is officially set for August 7. "On behalf of all the people that work on Endeavour, both here and really across the country, it’s a great, great feeling to have Endeavour back on the pad," said Shuttle Launch Director Mike Leinbach. "We’re looking forward to a great launch."

Launch preparations continue at Launch Pad 39A. Hypergolic propellant has been loaded into the solid rocket booster hydraulic power units, as well as Endeavour’s orbital maneuvering system, forward reaction control system and auxiliary power units.

The suits to be worn on the mission’s spacewalks have been stowed, and flight crew equipment and supplies are being loaded into the crew cabin. Payload closeouts include camera tests on the shuttle’s robotic arm and orbiter boom sensor system.

The 22nd flight to the International Space Station, STS-118 will be the first flight for Endeavour since 2002, and the first mission for Mission Specialist Barbara Morgan, the teacher-turned-astronaut whose association with NASA began more than 20 years ago.

 

 

2007年07月30日太空资讯

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NASA翼身合一飞机首次试飞成功

NASA翼身合一飞机首次试飞成功(图)

NASA试验新型飞机

  北京时间7月29日消息,据国外媒体报道,美国宇航局表示,尚处于试验阶段的“翼身合一”飞机第一次试飞成功,这种飞机的外形就像一个飞行翼,它的问世有望催生一种燃料消耗更低、噪音更小、容量更大的新型飞机的诞生。

  美国宇航局德莱顿飞行研究中心表示,这是一种遥控的喷气式飞机,重500磅,有3个 发动机,翼展21英尺。它在7月20日进行了试飞,爬升到海拔7500英尺的高空,飞行了大约半小时后成功降落。地面站的飞行员控制X-48B“翼身合一”飞机的飞行。美国宇航局和波音公司表示,它们正在将这次飞行资料与风洞试验资料进行比较。波音公司幻影工程部与美国宇航局和俄亥俄州赖特-帕特森空军基地的空军研究实验室合作,设计出这种飞机和它的复制品,由英格兰贝德福德的克兰菲尔德航空航天有限公司制造,现在飞机的尺寸只有未来完整版的飞机的8.5%。

  美国宇航局和波音公司表示,X-48B很像一个飞行翼,但是飞机的机翼与宽大、扁平且无尾的机身融合在一起。与传统飞机的圆柱形机身相比,这个设计提高了飞机的抬升力,减少了空气阻力,降低了飞行时的燃料消耗。发动机安装在飞机的后面,因此飞行时机体的内部会更加安静,到达地面的噪音也更少。测试开始时,这架飞机以很慢的速度飞行,以便研究人员获得有关它的设计稳定性和飞行控制特征的资料,尤其是在起飞和降落期间。另一架用作风洞测试的X-48B还能当作飞行测试的候补飞机。

科学家证实早期宇宙是黑洞摇篮

据美国《科学》杂志在线报道,天文学家利用钱德拉X射线天文望远镜发现了一些特大质量的黑洞,在7月24日公布的这幅由艺术家绘制的图画(如上图)中,一个黑洞正在加速运转的过程中吞噬周围的物质。与今天的黑洞相比,110亿年前的黑洞体积要大20倍。这可能是由于它们当时的“伙食”很好——这些怪物在早期星系团中出现的频率要比今天高6倍,因为后者中包含大量的气体,从而为黑洞的生长提供了更多的物质基础。

8月可赏三大天象

 新华社南京7月29日电 江苏、天津两地天文学会通报,8月公众可赏英仙座流星雨、海王星冲日和月全食等三大天象。

  英仙座流星雨将在8月13日晚间从天空划过,届时公众用肉眼就能观测。根据预报,今年该流星雨将发生两次极大值,分别是北京时间8月13日13时至15时30分和当天晚上23时,第二次极大值的出现最适合我国公众观测。按农历计算,当日是七月初一,整晚观测流星雨都不会有月光的干扰,观测条件相当不错。

  英仙座流星雨刚落幕,海王星便登场。8月14日海王星冲日,此后的20多天,海王星离地球的距离最近,天文爱好者可借助望远镜一睹这颗神秘星球。冲日期间,太阳落山后,海王星从东方地平线升起,直到第二天太阳升起后才从西方落下,因此整夜都能观测。在望远镜中,海王星是一个有着深蓝色视圆面的天体。

  8月28日将发生月全食,虽然我国各地公众都无法看到本次月食的全过程,但如果天气晴好,很多地区还是可以看到“带食月出”的景象。月全食发生的具体时间为28日16时52分—20时24分。

凤凰号8月3日升空前往寻找火星生命证据

凤凰号8月3日升空前往寻找火星生命证据(图)

凤凰号火星探测器
 
 

凤凰号8月3日升空前往寻找火星生命证据(图)

凤凰号火星探测器

  北京时间7月30消息,据《星期日泰晤士报》报道,8月3日,美国宇航局将向火星发射“凤凰”号探测器,决心为“外星球是否真的存在生命?”这一地球人都关注的问题,给出一个确定的答案。

  发射:即将上演

  美国东部时间8月3日早上5点35分(北京时间8月3日17时35分),美国宇航局的“凤凰”号探测器将在位于佛罗里达的卡纳维拉尔角发射升空,开始穿越太阳系的长达4.23亿英里(约6.8亿公里)的太空之旅。飞行10个月之后,“凤凰”号的发现有望最终回答科学界的一个最大疑问——过去或现在的 火星是否存在生命。

  在“德耳塔2”号 火箭的推动下,这艘造价4.2亿美元的飞船将首先冲出地球大气层,而后利用太阳的地心引力弹向火星。在此之后,“凤凰”号将在火星从未被勘测过的名为“Vastitas Borealis”——位于火星远北的北极大平原——的地区登陆。2008年5月,成功入主火星的“凤凰”号将利用机器检测设备,对火星的土壤和大气进行检测,寻找火星过去或现在生命存在的迹象,以及是否存在水;这也是美国宇航员一心想要解开的谜题。

  任务:困难重重

  在火星上演更多的发现已成为太空探索的一个最受人瞩目的课题。但自上世纪60年代以来的37项火星任务中,只有6次成功将数据从火星表面传回地球。如此高的失败率甚至让美国宇航局的一些人产生荒诞的推测——存在一个所谓的“巨型银河食尸鬼”,正是这个可怕的家伙吞噬了火星探测器。当然了,这种说法更多的只是一种自嘲。但有一点必须提醒人们,其它有关“火星诅咒”的说法只能阻止我们对这颗红色星球进行合理探索的脚步。

  事实上,向火星发射探测器本身就是一件相当复杂的事情:每26个月才能上演一次发射,也就是当地球轨道和火星轨道最为接近的时候。除此之外,飞抵火星的太空之旅也存在诸多技术难题。在登陆之前,科学家不得不将探测器在大气极为稀薄的火星上登陆所面临的挑战计算在内。这颗红色星球的地表一直遭到太阳风和尘暴的破坏,而且温度始终处于零度以下。

  执行火星任务将面临怎样的难度和挑战,只需问一问曾参与英国“小猎犬2”号任务的研究员科林·皮林格教授就知道了。2003年,试图将“小猎犬2”号送上火星的行动最终以失败告终。

  挑战:绝非一个

  “凤凰”号任务首席研究员、亚利桑那州大学月球与行星实验室的彼得·史密斯表示:“进入、降落和登陆是火星任务中最为危险的阶段。虽然只有短短的7分钟时间,但在小心翼翼安排的一系列步骤中,必须采取数百次行动才能实现安全登陆。”

  这些行动包括打开一个降落伞,将降落的速度从最初的每小时1.275万英里(约2万公里)降至每小时5英里(约8公里);在忍受数千度的高温之后抛弃隔热板;激活雷达;获取有关大气状况的读数并谨慎使用12个推进器以在更大程度上实现减速。

  如果所有这些均能顺利完成,并且“凤凰”号登陆车的3条机械腿得以最终接触火星表面,真正的工作便可以开始了。直径不到5英尺的“凤凰”号装有两组十角形的 太阳能电池板,展开后能够将太阳辐射转换成电能,为“凤凰”号的车载设备提供电力。

  在使用一台超高频发射机与地球进行无线电定期通信时,一组和可反复充电的锂离子电池将为“凤凰”号提供备用电力。两颗正绕着火星轨道运行的卫星——“火星奥德赛”和“火星侦察”——将接受“凤凰”号发出的信号。“凤凰”号的“寿命”预计为90个火星日,相当于92个地球日。

  时机:恰到好处

  寻找生命存在的证据并不是一件轻松的事情。有机分子的标记带有很大的欺骗性,同时也会被太空碎片或是在不经意下从地球“进口”的物质搞得“一塌糊涂”。为了避免这种事情的发生,“凤凰”号至关重要的组件均被封在一个所谓的“生物障碍包”里,并在无菌的条件下加热。史密斯说:“我们用了特别长的时间保持干净的地表,但地球本身就是一个脏兮兮的星球,到处是细菌和有机物质。”

  尽管存在这些问题,科学家还是急于重返火星。2002年,“火星奥德赛”号任务在火星极地地下发现了水冰,从而震惊了整个科学界。“凤凰”号任务标志着美国宇航局“寻水”政策进入另一个阶段,他们希望在地表4英寸之内发现冰。这也就是为什么要选在火星极地大平原这个特殊的地点登陆。极地平原的高度相当于格陵兰岛,至今还没有任何探测器在此登陆。此外,“凤凰”号驾临的时候正值火星春天,因此不会出现霜冻,而它的太阳能电池板也能获得更长的日照时间。

  前景:十分乐观

  太阳能电池板将为“凤凰”号高精尖的检测设备的电池充电,其中便包括7英尺8英寸长由铝和钛制成的机械手臂。如果一切都能按计划进行,这个机械手臂将钻进火星土壤层20英寸,寻找地表以下从未被动过的样本。任何发现的水冰都将被放置小烤炉内加热,检测构成生命的氢和碳基化学物质。

  其它针对有机化合物的检测是由上世纪70年代发射的两个“海盗”号探测器完成的。但它们没有任何发现,原因很简单:“海盗”号寻找有机化学物质微小痕迹的能力实在无法与它们的“后辈”相比。

  对于火星是否存在生命这个疑问,“凤凰”号将给出一个确定的答案。史密斯对此十分乐观的。他说:“如果火星合作的话,我们将发现有关水作用下修改的矿物与土壤化学成分的清晰标记。”

2007年07月29日天文新闻

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科学家称目前所有太阳黑子几乎消失

美科学家称几乎所有的太阳黑子都消失了

太阳和太阳风层探测器拍摄的太阳照片

       据俄罗斯有关媒体7月26日报道,美国宇宙空间研究中心的科学家称,太阳和太阳风层探测器最近发回的一批图片显示,太阳活动目前正处于最低潮。但科学家认为,这可能是太阳活动走出低谷前的“平静”。

于1995年入轨的太阳和太阳风层探测器由美国宇航局和欧洲航天局共同掌管。宇航局说,这颗卫星传回的最新图片显示,太阳表面目前称得上“一尘不染”,几乎看不见太阳黑子和耀斑,这是太阳活动处于最低潮的特征。科学家们正在密切关注太阳活动,等待与新一轮太阳活动周期有关的首批太阳黑子的出现。

据美国家海洋和大气管理局太空环境中心预测,下一个太阳活动周期将从2008年3月开始,到2011年岁末或者2012年到达顶峰。通常,一个太阳活动周期为11年,即从活动最低潮增强到最高潮,再缓慢回到最低潮的周期。在最低潮期间,太阳黑子和耀斑活动减少,有时好几天都看不到太阳表面有什么动静。

当太阳黑子重新开始出现时,表明太阳进入了新一轮活动周期。当其活跃程度到达最高潮时,太阳表面会持续显现太阳黑子,太阳耀斑频繁爆发。这期间,太阳会将大量带电粒子抛射到太空中,有可能对卫星和地面电网的运转、无线电通信等造成一定影响。

据来自负责跟踪观察太空的天气并预测其变化的科罗拉多州博尔德空间环境中心的消息称,当太阳活动周期达到高峰时,会影响到地球上一系列重要活动,如石油钻探、汽车导航和航空航天等。

专家们还预言,下一个周期的太阳黑子活动会比较强,将有140个黑子于2011年10月达到活动高峰。而另一半专家预言太阳黑子的活动较弱,认为会有90个黑子于2012年8月达到活动高峰。

科罗拉多大学大气和宇宙物理实验室主任丹尼尔-贝克指出,随着太阳活动周期的起伏,太阳辐射的变化可能会影响到太空里总价值2000亿美元以上的卫星。贝克称,其它问题还有:飞越极点的航班会失去联络信号、全球定位系统可能会受到太阳活动的干扰等。

土卫八胡桃外形之谜破解

土卫八的胡桃外形之谜被解开

土卫八

 

据国外媒体报道,美国宇航局下属的喷气推进实验室的科学家表示,卡西尼飞船观测到了围绕土星运行的土卫八,这颗冰卫星——伊阿珀托斯的形状像胡桃,中间部分突出。这是太阳系中已知的唯一一颗形状仍然和数亿年前一样的星球。这是因为在土卫八还年幼的时候,其外壳就被冻结了,形成了一个坚固的壳,迫使它保持年轻的外形。卡西尼飞船项目科学家朱利·卡斯蒂略说,“土卫八旋转快速,在其早年就已‘冻结’,留下的形体带有持久不变的曲线”。

如今,土卫八的直径比极地间距离宽33公里。通常,只有当卫星快速旋转时,才会发生这种失真现象,像快速旋转的滑冰运动员。研究人员解释说,这可能是短期的放射性元素,如铝-26和铁-60提供了足够的热量,保证年幼的土卫八里面温暖且湿软,容易压扁。此发现发表在最新出版的《伊卡洛斯》杂志上。

研究人员制作一个土卫八的模型,以解释其现有的“突出”形状。他们还测算了它的年龄,大约45.64亿年,与地球年龄(46亿年)相当。土卫八是土星卫星系统中的一颗外围卫星,距离土星356万多公里,每绕土星一周需79.33个地球日。在太阳系所有天体中,它是亮度变化幅度最大的一个。据观测,土卫八的自转周期等于其公转周期。

虽然有了这一惊人发现,但土卫八的谜并没有完全解开,它有巨大的山脉沿着赤道奔跑,它是如何形成的还是一个谜,卡斯蒂略说。

旨在探索神秘的土星及其卫星的卡西尼飞船具有可见光和红外观测能力,已传回许多关于土星及其卫星的珍贵图像资料。

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