Wednesday, December 17, 2008

Two new dinosaurs found in ancient Saharan river system

Dinosaur hunters have discovered two new species while searching an ancient river in the Sahara desert।

Thursday, October 16, 2008

Dunes and Dust in Arabia Terra

The battered region of Arabia Terra is among the oldest terrain on Mars. A dense patchwork of craters from countless impacts testifies to the landscape's ancient age, dating back billions of years.

In eastern Arabia lies an anonymous crater, 120 kilometers (75 miles) across. The floor of this crater contains a large exposure of rocky material, a field of dark sand dunes, and numerous patches of finer-grain material, probably dust. The shape of the dunes hints that prevailing winds have come from different directions over the years.

This false-color image, made from frames taken by the Thermal Emission Imaging System (THEMIS) aboard NASA's Mars Odyssey orbiter, shows the center of the crater's floor. The image combines a daytime view at visible wavelengths with a nighttime view at infrared (heat-sensing) wavelengths, thus giving scientists clues to the physical nature of the surface.

Fine-grain materials, such as dust and the smallest sand particles, heat up quickly by day and cool off equally quickly at night. However, coarser materials - bigger sand particles, gravel, and rocks - respond more slowly to the same daily cycle.

This means that when THEMIS views these late in the martian night, they appear warmer than the pools and patches of dust. In the image here, areas that are cold at night appear in blue tints, while the warmer areas show in yellows, oranges, and reds.

Location: 26.7N, 63.0E Released: 2006/02/07 Instrument: VIS Image Size: 37.7x34.2 km, 23.4x21.3mi, 2092x1907 pixels Resolution: 18m (59ft.)

Wednesday, October 08, 2008

Earth Science Literacy Initiative (ESLI)

PROJECT DESCRIPTION

The Earth Science Literacy Initiative (ESLI), funded by the National Science Foundation, aims to gather and codify the underlying understandings of Earth sciences into a succinct document that would have broad-reaching applications in both public and private arenas. It will establish the “Big Ideas” and supporting concepts that all Americans should know about Earth sciences. The resulting Earth Science Literacy framework will also become part of the foundation, along with similar documents from the Oceans, Atmospheres and Climate communities, of a larger geoscience Earth Systems Literacy effort.

The primary outcome of the Earth Science Literacy Initiative will be a community-based document that clearly and succinctly states the underlying principles and ideas of Earth science across a wide variety of research fields that are funded through the NSF-EAR program, including Geobiology and Low-Temperature Geochemistry, Geomorphology and Land-Use Dynamics, Geophysics, Hydrologic Sciences, Petrology and Geochemistry, Sedimentary Geology and Paleobiology, and Tectonics.

The Earth Science Literacy framework document of Big Ideas and supporting concepts will be a community effort representing the current state-of-the-art research in Earth sciences. It will be written, evaluated, shaped and revised by the top scientists working in Earth science. Because of its validity, authority and succinct format, the ESL framework will be influential in a wide variety of scientific, educational and political settings. Future governmental legislation will be guided by it, and future national and state educational standards will be based upon it.

Draft Document

Wednesday, September 24, 2008

Two Planets Suffer Violent Collision

Two Planets Suffer Violent Collision

ScienceDaily (Sep. 24, 2008) — Two terrestrial planets orbiting a mature sun-like star some 300 light-years from Earth recently suffered a violent collision, astronomers at UCLA, Tennessee State University and the California Institute of Technology will report in a December issue of the Astrophysical Journal।

"It's as if Earth and Venus collided with each other," said Benjamin Zuckerman, UCLA professor of physics and astronomy and a co-author on the paper. "Astronomers have never seen anything like this before. Apparently, major catastrophic collisions can take place in a fully mature planetary system."

"If any life was present on either planet, the massive collision would have wiped out everything in a matter of minutes — the ultimate extinction event," said co-author Gregory Henry, an astronomer at Tennessee State University (TSU). "A massive disk of infrared-emitting dust circling the star provides silent testimony to this sad fate."

Zuckerman, Henry and Michael Muno, an astronomer at Caltech at the time of the research, were studying a star known as BD+20 307, which is surrounded by a shocking 1 million times more dust than is orbiting our sun. The star is located in the constellation Aries. The astronomers gathered X-ray data using the orbiting Chandra X-ray Observatory and brightness data from one of TSU's automated telescopes in southern Arizona, hoping to measure the age of the star.

"We expected to find that BD+20 307 was relatively young, a few hundred million years old at most, with the massive dust ring signaling the final stages in the formation of the star's planetary system," Muno said.

Those expectations were shown to be premature, however, when Carnegie Institution of Washington astronomer Alycia Weinberger announced in the May 20, 2008, issue of the Astrophysical Journal that BD+20 307 is actually a close binary star — two stars orbiting around their common center of mass.

"That discovery radically revised the interpretation of the data and transformed the star into a unique and intriguing system," said TSU astronomer Francis Fekel who, along with TSU's Michael Williamson, was asked to provide additional spectroscopic data from another TSU automated telescope in Arizona to assist in comprehending this exceptional binary system.

The new spectroscopic data confirmed that BD+20 307 is composed of two stars, both very similar in mass, temperature and size to our own sun. They orbit about their common center of mass every 3.42 days.

"The patterns of element abundances in the stars show that they are much older than a few hundred million years, as originally thought," Fekel said. "Instead, the binary system appears to have an age of several billion years, comparable to our solar system."

"The planetary collision in BD+20 307 was not observed directly but rather was inferred from the extraordinary quantity of dust particles that orbit the binary pair at about the same distance as Earth and Venus are from our sun," Henry said. "If this dust does indeed point to the presence of terrestrial planets, then this represents the first known example of planets of any mass in orbit around a close binary star."

Zuckerman and colleagues first reported in the journal Nature in July 2005 that BD+20 307, then still thought to be a single star, was surrounded by more warm orbiting dust than any other sun-like star known to astronomers. The dust is orbiting the binary system very closely, where Earth-like planets are most likely to be and where dust typically cannot survive long. Small dust particles get pushed away by stellar radiation, while larger pieces get reduced to dust in collisions within the disk and are then whisked away. Thus, the dust-forming collision near BD+20 307 must have taken place rather recently, probably within the past few hundred thousand years and perhaps much more recently, the astronomers said.

"This poses two very interesting questions," Fekel said. "How do planetary orbits become destabilized in such an old, mature system, and could such a collision happen in our own solar system?"

"The stability of planetary orbits in our own solar system has been considered for nearly two decades by astronomer Jacques Laskar in France and, more recently, by Konstantin Batygin and Greg Laughlin in the U.S.A.," Henry noted. "Their computer models predict planetary motions into the distant future and they find a small probability for collisions of Mercury with Earth or Venus sometime in the next billion years or more. The small probability of this happening may be related to the rarity of very dusty planetary systems like BD+20 307."

"There is no question, however," Zuckerman said, "that major collisions have occurred in our solar system's past. Many astronomers believe our moon was formed from the grazing collision of two planetary embryos — the young Earth and a body about the size of Mars — a crash that created tremendous debris, some of which condensed to form the moon and some of which went into orbit around the young sun. By contrast with the massive crash in the BD+20 307 system, the collision of an asteroid with Earth 65 million years ago, the most favored explanation for the final demise of the dinosaurs, was a mere pipsqueak."

In their 1932 novel "When Worlds Collide," science fiction writers Philip Wylie and Edwin Balmer envisioned the destruction of Earth by a collision with a planet of a passing star. The 1951 classic movie based on the novel began a long line of adventure stories of space rocks apocalyptically plowing into Earth.

"But," Zuckerman noted, "there is no evidence near BD+20 307 of any such passing star."

This research is federally funded by the National Science Foundation and NASA and also by Tennessee State University and the state of Tennessee, through its Centers of Excellence program.

Thursday, August 21, 2008

Speed

Traveling Faster Than the Speed of Light: Two Baylor Physicists Have a New Idea That Could Make It Happen

Aug. 11, 2008

by Matt Pene

Two Baylor University scientists have come up with a new method to cause a spaceship to effectively travel faster than the speed of light, without breaking the laws of physics.

Dr. Gerald Cleaver, associate professor of physics at Baylor, and Richard Obousy, a Baylor graduate student, theorize that by manipulating the extra spatial dimensions of string theory around a spaceship with an extremely large amount of energy, it would create a "bubble" that could cause the ship to travel faster than the speed of light. To create this bubble, the Baylor physicists believe manipulating the 10th spatial dimension would alter the dark energy in three large spatial dimensions: height, width and length. Cleaver said positive dark energy is currently responsible for speeding up the expansion rate of our universe as time moves on, just like it did after the Big Bang, when the universe expanded much faster than the speed of light for a very brief time.

"Think of it like a surfer riding a wave," said Cleaver, who co-authored the paper with Obousy about the new method. "The ship would be pushed by the spatial bubble and the bubble would be traveling faster than the speed of light."

The method is based on the Alcubierre drive, which proposes expanding the fabric of space behind a ship and shrinking space-time in front of the ship. The ship would not actually move, rather the ship would sit in a bubble between the expanding and shrinking space-time dimensions. Since space would move around the ship, the theory does not violate Einstein's Theory of Relativity, which states that it would take an infinite amount of energy to accelerate a massive object to the speed of light.

String theory suggests the universe is made up of multiple dimensions. Height, width and length are three dimensions, and time is the fourth dimension. String theorists use to believe that there were a total of 10 dimensions, with six other dimensions that we can not yet identify because of their incredibly small size. A new theory, called M-theory, takes string theory one step farther and states that the "strings" that all things are made of actually vibrate in an additional spatial dimensional, which is called the 10th dimension. It is by changing the size of this 10th spatial dimension that Baylor researchers believe could alter the strength of the dark energy in such a manner to propel a ship faster than the speed of light.

The Baylor physicists estimate that the amount of energy needed to influence the extra dimension is equivalent to the entire mass of Jupiter being converted into pure energy for a ship measuring roughly 10 meters by 10 meters by 10 meters.

"That is an enormous amount of energy," Cleaver said. "We are still a very long ways off before we could create something to harness that type of energy."

The paper appears in the Journal of the British Interplanetary Society.

The full paper can be viewed here.

For more information, contact Dr. Cleaver at (254) 710-2283.

Black holes

Black holes 'dodge middle ground'

For black holes, there appears to be very little room for mediocrity, astronomers have found.

A study suggests they come in either small or large sizes, but medium-sized ones are very rare or non-existent.

A team of astronomers has examined one of the best hiding places for a middleweight black hole, and found that it cannot possibly host one.

Details of the research are to be published in the latest issue of the Astrophysical Journal.


If a medium black hole existed in a cluster, it would either swallow little black holes or kick them out of the cluster
Daniel Stern, JPL
Black holes are incredibly dense points of matter, whose gravity prevents even light from escaping.

The least massive black holes known are about 10 times the mass of our Sun and form when colossal stars explode as supernovas.

The heftiest black holes are billions of times the mass of the Sun and lie deep in the bellies of almost all galaxies.

That leaves black holes of intermediate mass, which were thought to be buried at the cores of globular clusters.

Full of stars

Globular clusters are dense collections of millions of stars, which reside within galaxies containing hundreds of billions of stars.

Theorists argue that these clusters should have a scaled-down version of a galactic black hole. Such objects would be about 1,000 to 10,000 times the mass of the Sun - medium-sized as far as black holes are concerned.

Now, a team of astronomers led by Stephen Zepf of Michigan State University, East Lansing, has carried out a detailed examination of a globular cluster called RZ2109.

The researchers' work led them to the conclusion that it could not possess a medium-sized black hole.

"Some theories say that small black holes in globular clusters should sink down to the centre and form a medium-sized one, but our discovery suggests this isn't true," said co-author Daniel Stern of Nasa's Jet Propulsion Laboratory in Pasadena, California.

In a previous study, Dr Zepf and his colleagues looked for evidence of a black hole in RZ2109, located 50 million light-years away in a nearby galaxy.

Elusive quarry

Using the European Space Agency's (Esa) XMM-Newton telescope, they discovered the telltale X-ray signature of an active, or "feeding", black hole. But, at that point, they still didn't know its size.

Stephen Zepf and Daniel Stern then teamed up with other researchers to obtain a chemical fingerprint, called a spectrum, of the globular cluster, using the WM Keck Observatory on Mauna Kea in Hawaii.

The spectrum revealed that the black hole is petite, with roughly 10 times the mass of the Sun.

According to theory, a cluster with a small black hole cannot have a medium one, too.

"If a medium black hole existed in a cluster, it would either swallow little black holes or kick them out of the cluster," said Dr Stern. In other words, the small black hole in RZ2109 rules out the possibility of a medium one being there, too.

The study does not quite represent the end of the road for medium-sized black holes.

Zepf said it was possible such objects were hiding in the outskirts of galaxies like our Milky Way, either in surrounding "dwarf galaxies" or in the remnants of dwarf galaxies being swallowed by a bigger one.

If so, he said, the black holes would be faint and difficult to find.

Story from BBC NEWS:
http://news.bbc.co.uk/go/pr/fr/-/1/hi/sci/tech/7573364.stm

Published: 2008/08/20 22:30:54 GMT

Thursday, February 28, 2008

Quakes Under Pacific Ocean Floor Reveal Unexpected Circulation System

Research upsets long-held view of volcanism-driven hydrothermal vents

Scientists have discovered a new way in which ocean water circulates through deep-sea vents. Credit and Larger Version
January 11, 2008
Zigzagging some 60,000 kilometers across the ocean floor, Earth's system of mid-ocean ridges plays a pivotal role in many workings of the planet: plate-tectonic movements, heat flow from the interior, and the chemistry of rock, water and air।

Now, a team of seismologists working in 2,500 meters of water on the East Pacific Rise, some 565 miles southwest of Acapulco, Mexico, has made the first images of one of these systems--and it doesn't look the way most scientists had assumed. The results of the National Science Foundation (NSF)-supported research appear in this week's issue of the journal Nature.
It was not until the late 1970s that scientists discovered the existence of vast plumbing systems under the oceans called hydrothermal vents. The systems pull in cold water, superheat it, then spit it back out from seafloor vents--a process that brings up not only hot water, but dissolved substances from rocks below. Unique life-forms feed off the vents' stew, and valuable minerals, including gold, may pile up.
The hypothetical image of a hydrothermal-vent system shows water forced down by overlying pressure through large faults along ridge flanks. The water is heated by shallow volcanism, then rises toward the ridges' middles, where vents (often called "black smokers" for the cloud of chemicals they exude) tend to cluster.
"The new images show a very different arrangement," said Rodey Batiza, marine geosciences section head in NSF's Division of Ocean Sciences.
The research team's calculations suggest that water moves a lot faster than previously thought--perhaps a billion gallons per year--through these systems. The water appears to descend instead through a buried 200-meter-wide chimney atop the ridge studied on the East Pacific Rise, run below the ridge along its axis through a tunnel just above a magma chamber, then bubble back up through a series of vents further along the ridge.
"If you look at images of hydrothermal vents, you come up with cartoons that don't at all match what we see," said lead Nature paper author Maya Tolstoy, a marine geologist at Lamont-Doherty Earth Observatory in Palisades, N.Y.
The images were created using seismometers planted around the ridge to record tiny, shallow earthquakes--in this study, 7,000 of them over seven months in 2003 and 2004.
The shallow quakes cluster neatly, outlining the cold water's apparent entrance. It dives straight down about 700 meters, then fans out into a horizontal band about 200 meters wide, before bottoming out at about 1.5 kilometers just above the magma. Heated water rises back up through a dozen vents about 2 kilometers north along the ridge.
The researchers interpret the quakes as being the result of cold water passing through hot rocks and picking up their heat--a process that shrinks the rocks and cracks them, creating small quakes.
Seawater, forced down into the resulting space, eventually gets heated by the magma, then rises back to the seafloor--much the same process seen in a pot of boiling water. Tolstoy and co-authors believe the water travels not through large faults--the model previously favored by some scientists--but through systems of tiny cracks.
Their chart of the water's route is reinforced by biologists' observations from submersible dives that the area around the downflow chimney is more or less lifeless, while the surging vents are covered with bacterial mats, mussels, tubeworms and other creatures that thrive off the heat and chemicals.
It is a mystery where vent organisms originally came from--some evolutionary biologists believe that life on Earth began with them--and how they make their way from one isolated vent system to another.
These findings could add to an understanding of seafloor currents along which they may move, and of the nutrient flows that feed them, said Tolstoy. The work also has large-scale implications for how heat and chemicals are cycled to the seafloor and overlying waters, she said.
Scientists are still retrieving and analyzing data on the vents and their circulation. In 2006, an ocean-bottom volcanic eruption buried many of their instruments; most of the instruments were lost, but the "survivors" provided new information about how undersea eruptions work.
-- Cheryl Dybas, NSF (703) 292-7734 cdybas@nsf.gov
Kevin Krajick, LDEO (212) 854-9729 kkrajick@ei.columbia.edu