Robinson and Researcher G. Jeffrey Taylor, both at the UHM Hawai'i Institute of Geophysics and Planetology, compiled water measurements
from lunar samples performed by colleagues from around the world, as well as their own.
Not exact matches
Our third expedition will bring back
samples of
lunar dust and rocks that everyone can own, providing scientists with a new source of
lunar materials for research, and making these treasures
from the Moon available to collectors and commercial purposes.
Researchers are using recent advances in imaging to reexamine
lunar samples from Apollo 11.
So says a fresh analysis of
lunar rock
samples from two American moonshots.
The next step will be to
sample the
lunar surface, finding ways to build with it or extract resources (especially water)
from it.
Wang and Jacobsen examined seven
lunar rock
samples from different
lunar missions and compared their potassium isotope ratios to those of eight terrestrial rocks representative of Earth's mantle.
The theft of the safe, which contained 101.5 grams of material, including
samples from every
lunar landing, was in fact stranger and more pedestrian...
Such
samples,
from an unexplored part of the
lunar surface, says Neal, «will have a huge impact on
lunar science... but will U.S. scientists be allowed to study these?»
Based on an extensive collection of
lunar and terrestrial
samples, a new study probing the elusive origins of the Moon — now typically thought to have formed
from a collision between a proto - Earth and a solid impactor — supports theories of a collision with extremely high energy.
And a mission to return a
sample from the moon's largest impact crater would have been some comfort to
lunar scientists still smarting
from Obama's decision to redirect NASA's crewed space exploration
from the moon to near - Earth asteroids.
All
lunar samples have come
from a region that's «not representative of the whole.
Brown University's Alberto Saal and colleagues measured the ratio of hydrogen to deuterium (hydrogen with an extra neutron) in
lunar rock
samples from the Apollo missions.
When water was first discovered in
lunar samples in 2008, it was very surprising because
from the time Apollo astronauts brought
lunar samples, scientists thought that the Moon contained virtually no water.
From spacecraft studies and analysis of samples from NASA's Apollo lunar missions, the researchers knew how often large solar storms oc
From spacecraft studies and analysis of
samples from NASA's Apollo lunar missions, the researchers knew how often large solar storms oc
from NASA's Apollo
lunar missions, the researchers knew how often large solar storms occur.
Also, if the solar wind were responsible for the amino acids, then
samples taken
from near the
lunar surface, which had the highest exposure to the solar wind, should have a greater abundance of amino acids than
samples taken
from deeper beneath the surface.
Just like contamination
from lunar module exhaust, material
from the solar wind could produce amino acids during
sample workup.
If contamination
from the exhaust produced the amino acids, then a
sample taken
from right under the Apollo 17
lunar module should have more amino acids than a
sample taken far away.
The development of ever more sensitive microscopy and chemical - analysis techniques will continue to produce new insights
from existing
samples into the foreseeable future — good news, considering that no nation appears to be close to returning humans to the
lunar surface.
Analysis of
lunar rock
samples thought to have been derived
from the original magma has given scientists a new estimate of the Moon's age.
Most interesting is that the about monthly variations correlate with the
lunar phases (peak on full moon) The Helsinki Background measurements 1935 The first background measurements in history;
sampling data in vertical profile every 50 - 100m up to 1,5 km; 364 ppm underthe clouds and above Haldane measurements at the Scottish coast 370 ppmCO2 in winds
from the sea; 355 ppm in air
from the land Wattenberg measurements in the southern Atlantic ocean 1925-1927 310
sampling stations along the latitudes of the southern Atlantic oceans and parts of the northern; measuring all oceanographic data and CO2 in air over the sea; high ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936
sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic
from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2
sampling on swedish island (Kattegatt) in summer
from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly average