Mostrando entradas con la etiqueta ESA’s GOCE satellite. Mostrar todas las entradas
Mostrando entradas con la etiqueta ESA’s GOCE satellite. Mostrar todas las entradas

domingo, 4 de diciembre de 2016

ESA : Electrifying spacecraft propulsion .- Electrificación de la propulsión de la nave espacial.............

http://www.esa.int/Our_Activities/Space_Engineering_Technology/Talking_technology/Electrifying_spacecraft_propulsión
Neil Wallace
A vuelo

Electrifying spacecraft propulsion

Neil Wallace, electric propulsion engineer
Electric propulsion has been around for a long time –1920s rocket pioneer Robert Goddard wrote about it. Perhaps it was an idea ahead of its time, because when I got into the space industry the thinking was that chemical thrusters were good enough, certainly for telecom missions. The platforms were small, working lifetimes were limited, power availability was constrained – and electronics didn’t last that long then either. All that started to change around the turn of the century, with a creeping up of mass, lifetime and power that made the various electric propulsion technologies more attractive.
From Ariane 5 rockets to small onboard thrusters, standard chemical thrusters work in the same way, squirting together chemicals that react in the form of heat, sending out exhaust to trigger an acceleration. These face a fundamental upper limit on performance however, set by the amount of energy in the chemical reaction that heats the ejected propellant, producing the thrust.
Electric propulsion pumps extra energy into the thrust reaction to reach much higher propellant velocities – up to an order of magnitude or so more – because their propellant is accelerated using electrical energy generated by the spacecraft solar arrays.
There are a wide range of different engine designs, starting with resistojets that simply use a heater on exhaust gases, to arcjets that pass a current through them, to Hall effect thrusters – a Russian speciality which has found commercial success – based on ionising propellant and then the highest-efficiency gridded ion thruster I’ve done a lot of work with, and has been applied to ESA’s GOCE and now BepiColombo missions.  
 
 
Gridded ion thrsters reach very high exhaust speeds – typically an order of magnitude greater than chemical thrusters – because ionised propellant is accelerated through a set of high-voltage grids using electrical energy, freely available from solar arrays.
Much less propellant is required, although the down side is that thrust levels are much lower and therefore the initial spacecraft acceleration is also low, around the the weight of a Euro coin to start off with – meaning the thrusters have to keep firing for long periods to be effective. However, in space there is nothing to slow a spacecraft down, so the craft’s velocity ends up increasing dramatically. Assuming the same propellant mass, our T6 thrusters can accelerate BepiColombo to a speed 15 times greater than an equivalent chemical thruster.
The difficulty has been developing them, of course. There’s a physics side to understand and then an engineering side as well, to optimise the materials, achieve stable gas discharges and so on. What was originally the UK’s Farnborough Royal Aircraft Establishment, now the QinetiQ company has been researching electric propulsion since the early 1960s. These high-temperature thrusters require utmost reliability through thousands of on/off cycles, amounting to tens of thousands of hours of testing. 
What's needed next is a shift in scale - it took four years to build these four Bepi Colombo flight models, the real challenge would be to speed up production
The initial result was the 10-cm diameter T5 thruster, which became a key enabling technology for ESA’s gravity-mapping GOCE mission. Because GOCE stayed in the lowest possible orbit for maximum gravitational sensitivity, it needed a continuously throttling thruster to overcome constantly-varying drag from the thin vestiges of atmosphere. GOCE’s drag compensation system operated continuously throughout its four-year lifetime, responding in tenths of a second – the mission only ending when its xenon fuel finally ran out. Then came the scaled-up 22-cm T6, four of which will propel BepiColombo into Mercury orbit after its 2018 launch. The mission would not be realisable in its current form without them.
What’s needed next is a shift in scale. It took four years to build these four BepiColombo flight models, the real challenge would be to speed up production so the technology could be routinely available for missions – including large scale mega-constellations to come. 
ESA
Guillermo Gonzalo Sánchez Achutegui
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lunes, 28 de mayo de 2012

The Earth:CryoSat goes to sea

Hi My Friends: A VUELO DE UN QUINDE EL BLOG., CryoSat was launched in 2010 to measure sea-ice thickness in the Arctic, but data from the Earth-observing satellite have also been exploited for other studies. High-resolution mapping of the topography of the ocean floor is now being added to the ice mission’s repertoire.
 An Earth-orbiting radar cannot see the ocean floor, but it can measure ocean-surface height variations induced by the topography of the ocean floor. The gravitational pull of the seafloor produces minor variations in ocean surface height. Seafloor mapping by ships is much more accurate than radar altimeter mapping, but to date only 10% of the seafloor has been charted this way. A complete mapping of the deep oceans using ships would take 200 ships navigating Earth, 24 hours a day, for an entire year at a cost of billions of dollars. Mapping using satellite radars can cover a larger area in a shorter amount of time. When interesting features are discovered in satellite measurements, they can later be surveyed in fine detail by ships.

Credits: Scripps Institution of Oceanography
 Gravity field over the Pacific Ocean’s Emperor Seamounts based on CryoSat, ERS and Geosat satellite altimeter measurements of ocean-surface height. At this scale, the gravity field of the ocean reflects seafloor topography, called bathymetry. The improved radar measurements from CryoSat will be used to improve bathymetry. The measurements will be used in the next generation of the seafloor maps in Google Earth.

Credits: Scripps Institution of Oceanography/NOAA

CryoSat was launched in 2010 to measure sea-ice thickness in the Arctic, but data from the Earth-observing satellite have also been exploited for other studies. High-resolution mapping of the topography of the ocean floor is now being added to the ice mission’s repertoire.
  The main objective of the polar-orbiting CryoSat is to measure the thickness of polar sea ice and monitor changes in the ice sheets that blanket Greenland and Antarctica.
But the satellite’s radar altimeter is not only able to detect tiny variations in the height of the ice but it can also measure sea level.
The topography of the ocean surface mimics the rises and dips of the ocean floor due to the gravitational pull. Areas of greater mass, such as underwater mountains, have a stronger pull, attracting more water and producing a minor increase in ocean-surface height.
Therefore, instruments that measure sea-surface height incidentally map the ocean floor in previously uncharted areas. 
There have been several recent global gravity missions, such as ESA’s GOCE satellite, that provide extraordinarily accurate measurements of gravity at the spatial resolution of hundreds of kilometres.
But CryoSat’s radar altimeter can sense the gravity field at the ocean surface, so that seafloor characteristics at scales of 5–10 km are revealed. This is the first altimeter in 15 years to map the global marine gravity field at such a high spatial resolution.
Recent studies at the Scripps Institution of Oceanography in San Diego, USA, found that the range precision of CryoSat is at least 1.4 times better than the US's Geosat or ESA's ERS-1.
They estimate that this improved range precision combined with three or more years of ocean mapping will result in global seafloor topography – bathymetry – that is 2–4 times more accurate than measurements currently available
“We know more about the surfaces of Venus and Mars than we do about the bathymetry of deep oceans,” said David Sandwell from the Scripps Institution of Oceanography in the US.
“This new mapping from CryoSat will revolutionise our understanding of ocean floor tectonics and reveal, perhaps, 10 000 previously uncharted undersea volcanoes.”
Most satellite radar altimeters such as the one on the joint CNES/NASA/Eumetsat/NOAA Jason-2 follow repeated ground-tracks every 10 days to monitor the changes in ocean topography associated with ocean currents and tides.
CryoSat’s 369-day repeat cycle provides a dense mapping of the global ocean surface at a track spacing of over 4 km. Three to four years of data from CryoSat can be averaged to reduce the ‘noise’ due to currents and tides and better chart the permanent topography related to marine gravity.
ESA
Guillermo Gonzalo Sánchez Achutegui
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