mars exploration: an overview of indian and international
TRANSCRIPT
Taurian Innovative Journal/Volume 1/ Issue 1
Corresponding Author: Nayama Valsa Scariah 66
Mars exploration: An overview of Indian and
International Mars Missions
NayamaValsa Scariah1, Dr. Mili Ghosh2, Dr.A.P.Krishna3
Birla Institute of Technology, Mesra, Ranchi
Abstract- Mars is the fourth planet from the sun. It is
also known as red planet because of its iron oxide
content. There are lots of missions have been launched to
mars for better understanding of our neighboring planet.
There are lots of unmanned spacecraft including
orbiters, landers and rovers have been launched into
mars since early 1960. Sputnik was the first satellite
launched in 1957 by Soviet Union. After seven failure
missions to Mars, Mariner 4 was the first satellite which
reached the Martian orbiter successfully. The Viking 1
was the first lander reached on Mars on 1975. India
successfully launched a spacecraft, Mangalyan (Mars
Orbiter Mission) on 5th November, 2013, with five
payloads to Mars. India was the first nation to
successfully reach Mars on its first attempt. It was really
a proud moment for all the Indians. India is the fourth
planet to reach Mars after United States, Europe and
Soviet Union. India may put a lander on Mars in 2021 or
2022. MOM(Mars Orbiter Mission) has five payloads
such as LAP(Lyman Alpha photometer), MSM(Methane
Sensor for Mars), MENCA(Mars Exospheric Neutral
Composition Analyser), TIS(Thermal Infrared Imaging
Spectrometer), MCC(Mars Color Camera). LAP is used
to measure the relative abundance of deuterium and
hydrogen in the upper atmosphere. Deuterium/hydrogen
ratio will allow an estimation of the amount of water loss
to the atmosphere. MENCA is used for analyzing the
neutral composition of particles. MSM is used to
measure methane in the Martian atmosphere. MCC
gives images and information about the surface features
and composition of the Martian surface. Temperature
and emissivity can be measured by using TIS data.
There are lots of studies have been carried out in Mars
such as mineral exploration, morphological analysis,
climatic variation, assessment of environmental
conditions ever been favorable for microbial conditions
etc. The curiosity rover, which was launched on 2011 by
NASA gave more salient information regarding the
evidence of water in Mars.
1. Introduction
Mars is also known as red planet, because of the
reddish iron oxide prevalent on its surface gives it a
reddish appearance. It is the fourth planet from sun.
The term sol is used to define duration of solar day on
Mars. A mean Martian solar day or sol is 24 hours 39
minutes and 34.244 seconds. Many space missions to
Mars have been planned and launched for Mars
exploration (Table:1) but most of them failed without
completing the task specially in early attempts
whereas some NASA missions were very
successful(such as the twin Mars Exploration Rovers,
MER-A Spirit and MER-B Opportunity).There are lots
of unmanned spacecraft including orbiters, landers
and rovers which have been launched since early 1960
for the better understanding of our neighboring planet.
Marsnik 1 (USSR) launched Oct. 10, 1960, was the
first satellite on an intended Mars flyby. After seven
failure missions to Mars, Mariner 4 was the first
satellite which reached the Martian orbiter successfully
on July 14, 1965, and sent 21 photos back to Earth.The
Viking 1 was the first lander reached on Mars on 1975.
India successfully launched a spacecraft, Mangalyan
(Mars Orbiter Mission) on 5th November 2013, with
five payloads to Mars. India was the first nation to
successfully reach Mars on its first attempt. It was
really a proud moment for all the Indians. India is the
fourth country to reach Mars after United States,
Europe and Soviet Union. India may put a lander on
Mars in 2021 or 2022. There are lots of studies have
been carried out in Mars such as mineral exploration,
morphological analysis, climatic variation, assessment
of environmental conditions ever been favorable for
microbial conditions etc. The curiosity rover, launched
in 2011 by NASA, gave more salient information
regarding the evidence of water in Mars.
Taurian Innovative Journal/Volume 1/ Issue 1
Corresponding Author: Nayama Valsa Scariah 67
Spacecraft Agency Launched on
Mission Type
Outcome Remark
Marsnik1 USSR 1960 Mars flyby Launch
failure
Failed to orbit
Marsnik2 USSR 1960 Mars flyby Launch failure
Failed to orbit
Sputnik22 USSR 1962 Mars flyby Launch
failure
Booster stage ("Block
L") disintegrated in LEO
Mars1 USSR 1962 Mars flyby Spacecraft failure
Communications lost before flyby
Sputnik 24 USSR 1962 Lander Launch
failure
Never left LEO
Mariner 3 NASA 1964 Mars flyby Launch failure
Payload fairing failed to seperate
Mariner 4 NASA 1964 Mars flyby Successful Closest approach at
01:00:57 UTC on 15 July 1965
Zond 2 USSR 1953 Mars flyby Spacecraft
failure
Communications lost
before flyby
Mariner 6 NASA 1969 Mars flyby Successful
Mars M-69
No:521
USSR 1969 Orbiter Launch
failure
Failed to orbit
Mariner 7 NASA 1969 Mars flyby Successful
Mars M-69
No:522
USSR 1969 Orbiter Launch
failure
Failed to orbit
Mariner 8 NASA 1971 Orbiter Launch
failure
Failed to orbit
Kosmos 419 USSR 1971 Orbiter Launch
failure
Never left LEO;
booster stage burn
timer set incorrectly
Mars 2 USSR 1971 Orbiter Mostly
successful
Entered orbit on 27
November 1971,
operated for 362 orbits. Mapping
operations
unsuccessful due to
dust storms on the surface
Mars 2 Lander USSR 1971 Lander Spacecraft
failure
Deployed from Mars
2, failed to land during attempt on 27
Taurian Innovative Journal/Volume 1/ Issue 1
Corresponding Author: Nayama Valsa Scariah 68
November 1971
Mars 3 USSR 1971 Orbiter Mostly
successful
Entered orbit on 2
December 1971,
operated for 20 orbits. Mapping operations
unsuccessful due to
dust storms on the surface
Mars 3 Lander USSR 1971 Lander Partial
failure
Deployed from Mars
3; landed at 13:52
UTC on 2 December 1971; contact lost
14.5 seconds after
transmission start
Prop-M Rover USSR 1971 Rover Spacecraft failure
Failed to deploy
Mariner 9 NASA 1971 Orbiter Successful Entered orbit on 14
November 1971, deactivated 516 days
after entering orbit
Mars 4 USSR 1973 Orbiter Spacecraft
failure
Failed to perform
orbital insertion burn
Mars 5 USSR 1973 Orbiter Partial
failure
Failed after 9 days in
Mars orbit; returned
180 frames
Mars 6 USSR 1973 Lander
Flyby
Spacecraft
failure
Contact lost upon
landing, atmospheric
data mostly unreadable. Flyby bus
collected data
Mars 7 USSR 1973 Lander
Flyby
Spacecraft
failure
Separated from coast
stage prematurely, failed to enter Martian
atmosphere
Viking 1
Orbiter
NASA 1975 Orbiter Successful Operated for 1385
orbits
Viking 1 Lander
NASA 1975 Lander Successful Deployed from Viking 1 orbiter,
operated for 2245 sols
Viking 2
Orbiter
NASA 1975 Orbiter Successful Operated for 700
orbits
Viking 2
Lander
NASA 1975 Lander Successfu Deployed
from Viking 2 orbiter, operated for 1281 sols
Taurian Innovative Journal/Volume 1/ Issue 1
Corresponding Author: Nayama Valsa Scariah 69
Phobos 1 USSR 1988 Orbiter
Phobos
Lander
Spacecraft
Failure
Communications lost
before reaching Mars;
failed to enter orbit
Phobos 2 USSR 1988 Orbiter
Phobos
Lander
Partial failure
Orbital observations successful,
communications lost
before landing
Mars Observer NASA 1992 Orbiter Spacecraft failure
Lost communications before orbital
insertion.
Mars Global Suveyor
NASA 1996 Orbiter Successful Operated for seven years
Mars 96 Rosaviak-
osmos
1996 Orbiter
Penetrators
Launch
failure
Never left LEO
Mars pathfinder NASA 1996 Lander Successful Landed at 19.13°N 33.22°W on 4 July
1997
Sojourner NASA 1996 Rover Successful Operated for 84 days
Nazomi ISAS 1998 Orbiter Spacecraft
failure
Ran out of fuel before
reaching mars
Mars climate
Orbiter
NASA 1998 Orbiter Spacecraft
failure
Approached Mars too
closely during orbit insertion attempt due
to unit conversion
error and burned up in the atmosphere
Mars Polar
Lander
NASA 1999 Lander Spacecraft
failure
Failed to land
Deep Space 2 NASA 1999 Penetrator Spacecraft failure
Deployed from MPL, no data returned
Mars Odyssey NASA 2001 Orbiter Operational Expected to remain
operational until 2025
Mars express ESA 2003 Orbiter Operational Enough fuel to remain operational until 2026
Beagle 2 ESA 2003 Lander Lander
failure
Deployed from Mars
Express. Successful
landing, but two solar panels failed to
deploy, obstructing its
Taurian Innovative Journal/Volume 1/ Issue 1
Corresponding Author: Nayama Valsa Scariah 70
communications
Spirit NASA 2003 Rover Successful Landed on January 4,
2004.
Operated for 2208 sols
Opportunity NASA 2003 Rover Operational Landed on January 4,
2004. Operated for
2208 sols
Rosetta ESA 2004 Gravity
assist
Successful
Mars
reconnaissance Orbiter
NASA 2005 Orbiter Operational Entered orbit on
March 10, 2006
Phoenix NASA 2007 Lander Successful Landed on May 25,
2008. End of mission
November 2, 2008
Dawn NASA 2007 Gravity
assist
Successful
Fabos-Grunt Roskosm
os
2011 Orbiter
Phobos
sample
Spacecraft
failure
Yinghuo-1 CNSA 2011 Orbiter Failure
Curiosity NASA 2011 Rover Operational
Mars Orbiter
Mission
ISRO 2013 Orbiter Operational
MAVEN NASA 2013 Orbiter Operational
ExoMars Trace
Gas Orbiter
ESA
Roskosm
os
2016 Orbiter Operational
Schiaparelli EDM lander
ESA 2016 Lander Partial failure
InSight NASA 2018 Lander En route
2. Spacecraft classification
Spacecrafts are the machine or vehicle designed to
fly in outer space. There are different types of
spacecrafts are available such as flyby spacecraft,
orbiter spacecraft, Atmospheric spacecraft, Lander
spacecraft, Rover spacecraft, Penetrator spacecraft,
Observatory spacecraft and communication
spacecraft. The Mars flyby is a movement of
spacecraft passing in the vicinity of the planet Mars,
but not entering the orbit or landing on it.
A spacecraft designed to travel to a distant planet
and enter into orbit is known as orbiter spacecraft
(Figure 1.). Atmospheric spacecraft are designed for
a relatively short mission to collect data about the
atmosphere of a planet or satellite. Lander spacecraft
(Figure2.) are designed to reach the surface of a
planet and survive long enough to telemeter data
back to Earth. Surface penetrators have been
designed for entering the surface of a body, such as a
comet, measuring, and telemetering the properties of
the penetrated surface. Rover moves (Figure 3.)
Taurian Innovative Journal/Volume 1/ Issue 1
Corresponding Author: Nayama Valsa Scariah 71
across the surface of a planet. An observatory
spacecraft does not travel to a destination to explore
it. Instead, it occupies an Earth orbit or a solar orbit
from where it can observe distant targets free of the
obscuring and blurring effects of Earth's atmosphere.
Figure 1. Mars Orbiter Mission Spacecraft
Figure 2. Viking Lander
Figure 3.Curiosity rover moving in Gale crater, Mars
3. Indian Mars Exploration
The Mars Orbiter Mission (MOM) also called
Mangalyan mission launched on November 5th
2013 by PSLV C-25 got inserted into Martian
orbit on September 24, 2014 in its first attempt.
Mars Orbiter Mission spacecraft orbiting Mars in
a highly elliptical orbit characterized by nearest
point to Mars (periapsis) at around 300km and
farthest point (apoapsis) at 7000km. It has five
payloads such as LAP (Lyman Alpha
photometer), MSM(Methane Sensor for Mars),
MENCA(Mars Exospheric Neutral Composition
Analyser), TIS(Thermal Infrared Imaging
Spectrometer), MCC(Mars Color Camera). LAP is
used to measure the relative abundance of
deuterium and hydrogen in the upper atmosphere.
Deuterium/hydrogen ratio will allow an estimation
of the amount of water loss to the atmosphere.
MENCA is used for analyzing the neutral
composition of particles. MSM is used to measure
methane in the Martian atmosphere. MCC gives
images and information about the surface features
and composition of the Martian surface.
Temperature and emissivity can be measured by
using TIS data.
Taurian Innovative Journal/Volume 1/ Issue 1
Corresponding Author: Nayama Valsa Scariah 72
4. Mars color camera (MCC)
Mars Color Camera operates in the visible range of
0.4 to 0.7μm with varying resolution of 20m to 4km.
MCC payload provides data in true colors of Mars
(Fig:4) covering red, green and blue in Bayer
pattern. The main science objectives of MCC are
studying morphology of land forms, wind streaks,
and study related to dust storm and dust devils in
different seasons.
5. Thermal Infrared Imaging Spectrometer
(TIS)
TIS is used to observe thermal emission from
Martian surface. It operates in the thermal region of
7-13μm. The main target of the TIS payloads are to
determine surface temperature and thermal inertia of
Martian surface and used to analyze dynamic
climatic variation over different seasons.
6. Methane Sensor for Mars (MSM)
MSM used to determine the amount of columnar
methane (CH4) in the Martian atmosphere at several
parts per billion (ppb) levels. The possible finding
of Methane in Martian atmosphere will provide
clues about the presence of life on Mars.
7.2 Lyman Alpha Photometer
Lap used to determine Deuterium to Hydrogen(D/H)
abundance ratio of Martian exosphere. Comparison of
past and present D/H ratio helps to determine the
hydrogen content in the atmosphere which gives the
evidence of presence water in Martian atmosphere.
7.3 Mars exospheric Neutral composition Analyzer
(MENCA)
MENCA is used for the in situ study of the composition
of the Martian neutral exosphere.
Figure 4. MCC image of Gale crater, Mars
7. Major findings through different Mars Missions
7.1 Evidence of Life on Mars
The serious hunt for organics on Mars has long
complicated history. It starts with NASA’s twin Viking
lander, which spotted two chlorinated chemicals,
chloromethane and dichloromethane. After analyzing
the results from Viking lander scientists thought that red
planet was dead planet. NASA’s Phoenix lander found
chorine containing chemicals called perchlorates in the
Martian soil. Perchlorates can destroy organics in a
heated sample. The Curiosity rover launched on 2011
and was landed on Gale crater, Mars. From Curiosity
rover data, scientist found that Gale hosted a long-lived,
potentially habitable lake-and-stream system billions of
years ago.
7.4 Morphological Analysis of Mars
Different Martian landforms have been analyzed and
mapped by using different datasets such as MCC,
CTX, HiRISE etc.
7.5 Mineral exploration
Different minerals have been explored by using
different data sets. Two types of phyllosilicates were
identified by using OMEGA datasets. Gamma Ray
Spectrometer of Mars Odyssey Mission is used to
determine the chemical elements such as hydrogen in
Martian environment
Conclusion
In most of the Mars missions have planned for
identifying the possibility of habitable world in Mars
and also help to understand how geologic, climatic and
process have worked to shape Mars and its environment
over time. NASA has planned to send astronaut to Mars
and return back to earth safely.
Taurian Innovative Journal/Volume 1/ Issue 1
Corresponding Author: Nayama Valsa Scariah 73
ISRO plans to next Mars Orbiter Mission on 2020 with
orbiter and rover spacecraft with great scientific
payload
References
[1] Audourd (2014), Thermophysical properties of gale
crater plains along curiosity traverse, Lunar and Planetary
Science Conference, vol.45, 1784-1785
[2] Bennett K.A. , Fenton L. , J.F. Bell III (2016), The albedo
of martian dunes: Insights into aeolian activity and dust devil
formation, Aeolian Research
[3] Fenton K.L, Joshua L. Bandfield and A. Wesley Ward
(2003), Aeolian processes in Proctor Crater on Mars:
Sedimentary history as analyzed from multiple data sets,
Journal of geophysical research, vol. 108, no. E12, 5129
[4] Hobbs W.S. , David J. Paull, Mary C. Bourke (2010),
Aeolian processes and dune morphology in Gale Crater,
Icarus, vol.210, 102-115
[5]Singh R. P. (2015), Thermal Infrared Imaging
Spectrometer for Mars Orbiter Mission, Current Science,
Vol. 109 Issue 6, p1097-1105
[6]Tanaka and Hayward (2008), Mars’ north circum-polar
dunes: distribution, sources, and migration history, Planetary
dunes workshop
Corresponding Author: Nayama Valsa Scariah
Institution: BIT, Mesra, Ranchi
E-mail id: [email protected]