词条 | Venera 4 |
释义 |
| name = Venera 4 | image = Venera 4 (MMA 2011) (1).JPG | image_size = 230px | image_caption = Venera 4 model | insignia = The Soviet Union 1968 CPA 3623 stamp (Venera 4 Space probe).jpg | insignia_size = 60px | mission_type = Venus lander and flyby spacecraft | operator = Lavochkin | COSPAR_ID = 1967-058A | SATCAT = 2840 | mission_duration = 127 days | spacecraft = 1V (V-67) s/n 310[1] | manufacturer = Lavochkin | launch_mass = {{convert|1106|kg|lb|abbr=on}}[2] | dry_mass = {{convert|377|kg|lb|abbr=on}} | launch_date = 12 June 1967, 02:40 UTC[2][3] | launch_rocket = Molniya 8K78M[2] | launch_site = Baikonur 1/5 | last_contact = {{end_date|18 October 1967}}, 04:34 UT | orbit_reference = Heliocentric | orbit_periapsis = 0.71 AU | orbit_apoapsis = 1.02 AU | orbit_inclination = 4.3° | orbit_period = 293 days | apsis = helion | interplanetary = |type = lander_impact |note = disintegrated |object = Venus |arrival_date = 18 October 1967, 04:34 UT |location = {{Venus coords and quad cat|19|N|38|E}} (Eisila region) | programme = Venera | previous_mission = Kosmos 96 | next_mission = Kosmos 167 }} Venera 4 ({{lang-ru|Венера-4}} meaning Venus 4), also designated 1V (V-67) s/n 310[1] was a probe in the Soviet Venera program for the exploration of Venus. The probe comprised an entry probe, designed to enter the Venus atmosphere and parachute to the surface, and a carrier/flyby spacecraft, which carried the entry probe to Venus and served as a communications relay for the entry probe. In 1967 it was the first successful probe to perform in-place analysis of the environment of another planet. It may also have been the first probe to land on another planet, with the fate of its predecessor Venera 3 being unclear.[4] Venera 4 provided the first chemical analysis of the Venusian atmosphere, showing it to be primarily carbon dioxide with a few percent of nitrogen and below one percent of oxygen and water vapors. The station detected a weak magnetic field and no radiation field. The outer atmospheric layer contained very little hydrogen and no atomic oxygen.{{citation needed|date = October 2017}} The probe sent the first direct measurements proving that Venus was extremely hot, that its atmosphere was far denser than expected, and that it had lost most of its water long ago. DesignThe main carrier spacecraft 4 stood {{convert|3.5|m}} high, its solar panels spanned {{convert|4|m}} and had an area of {{convert|2.5|m2}}. The carrier spacecraft included a 2-meter long magnetometer, an ion detector, a cosmic ray detector and an ultraviolet spectrometer capable of detecting hydrogen and oxygen gases. The devices were intended to operate until entry into the Venusian atmosphere. At that juncture, the station was designed to release the probe capsule and disintegrate. The rear part of the carrier spacecraft contained a liquid-fuel thruster capable of correcting the flight course. The flight program was planned to include two significant course corrections, for which purpose the station could receive and execute up to 127 different commands sent from the Earth.[8] The front part of the carrier spacecraft contained a nearly spherical landing capsule {{convert|1|m}} in diameter and weighing {{convert|383|kg}}. Compared to previous (failed) Venera probes, the capsule contained an improved heat shield which could withstand temperatures up to {{convert|11000|C}}. Instead of the previous liquid-based cooling design, a simpler and more reliable gas system was installed.[5] The durability of the capsule was checked by exposing it to high temperatures, pressures and accelerations using three unique testing installations. The heat resistance was checked in a high-temperature vacuum system emulating the upper layers of the atmosphere.[10] The capsule was pressurized up to 25 atmospheres. (The surface pressure on Venus was unknown at the time. Estimates ranged from a few to hundreds of atmospheres.)[6] Finally, it was subjected to accelerations of up to 450 g in a centrifuge. The centrifuge test caused cracking of electronic components and cable brackets, which were replaced shortly before launch. The timing for launch was rather tight, so as not to miss the launch window—the days of the year when the path to the destination planet from Earth is energetically least demanding.{{citation needed|date = October 2013}} The capsule could float in case of a water landing. Considering the possibility of such a landing, its designers made the lock of the capsule using sugar;[8][10][7] it was meant to dissolve in liquid water, releasing the transmitter antennas. The capsule contained a newly developed vibration-damping system, and its parachute could resist temperatures up to 450 °C.[8] The capsule contained an altimeter, thermal control, a parachute and equipment for making atmospheric measurements. The latter included a thermometer, barometer, hydrometer, altimeter and a set of gas analysis instruments. The data were sent by two transmitters at a frequency of 922 MHz and a rate of 1 bit/s; the measurements were sent every 48 seconds. The transmitters were activated by the parachute deployment as soon as the outside pressure reached {{convert|0.6|atm}}, which was thought to occur at the altitude about {{convert|26|km}} above the surface of the planet. The signals were received by several stations, including the Jodrell Bank Observatory.[5][8] The capsule was equipped with a rechargeable battery with a capacity sufficient for 100 minutes of powering the measurement and transmitter systems. To avoid becoming discharged during the flight to Venus, the battery was kept charged using the solar panels of the carrier spacecraft. Before the launch, the entire Venera 4 station was sterilized to prevent possible biological contamination of Venus.[5] MissionTwo nominally identical 4V-1 probes were launched in June 1967. The first probe, Venera 4, was launched on 12 June by a Molniya-M carrier rocket flying from the Baikonur Cosmodrome.[2] A course correction was performed on 29 July when it was 12 million km away from Earth; otherwise the probe would have missed Venus. Although two such corrections had been planned, the first one was accurate enough and therefore the second correction was canceled. On 18 October 1967, the spacecraft entered the Venusian atmosphere with an estimated landing place near {{Venus coords and quad cat|19|N|38|E}}.[9] The second probe, Kosmos 167, was launched on 17 June but failed to depart low Earth orbit.[10] During entry into the Venusian atmosphere, the heat shield temperature rose to {{convert|11000|C}} and at one point the cabin deceleration reached 300 G.[11] The descent lasted 93 minutes. The capsule deployed its parachute at an altitude of about {{convert|52|km}}, and started sending data on pressure, temperature and gas composition back to Earth. The temperature control kept the inside of the capsule at {{convert|−8|C}}. The temperature at 52 km was recorded as {{convert|33|C}}, and the pressure as less than {{convert|1|atm}}. At the end of the 26-km descent, the temperature reached {{convert|262|C}} and pressure increased to {{convert|22|atm}}, and the signal transmission terminated. The atmospheric composition was measured as 90–93% carbon dioxide, 0.4–0.8% oxygen, 7% nitrogen and 0.1–1.6% water vapor.[9] Radar altimeterAltitude of the Venera probe relative to the surface was measured during using a radar altimeter operating at 770 MHz. The altimeter had an integer ambiguity of 30 km: that is, the same radar signal would be given at an altitude of X, X plus 30 km, X plus 60 km, etc.[12] (an effect known as "aliasing"). At the time the distance of the cloudtops above the surface was not known, and due to this ambiguity, the first radar return, now believed to be at an actual altitude of about {{convert|55|km}}, was initially misinterpreted as {{convert|26|km}}. Therefore, based on the misinterpreted radar results, the Soviet team initially announced the probe descended to the surface.[13][14] This result was quickly dismissed as inconsistent with the planetary diameter measured by radar,[15][16] and the pressure readings by the capsule were much lower than predicted by the recently-developed models of the Venus atmosphere.[5][8] AchievementsFor the first time, in situ analysis of the atmosphere of another planet was performed and the data sent back to Earth; the analysis included chemical composition, temperature and pressure. The measured ratio of carbon dioxide to nitrogen of about 13 corrected the previous estimates so much (an inverse ratio was expected in some quarters) that some scientists contested the observations. The main station detected no radiation belts; relative to Earth, the measured magnetic field was 3000 times weaker, and the hydrogen corona was 1000 times less dense. No atomic oxygen was detected. All the data suggested that water, if it had been present, had leaked from the planet long before. This conclusion was unexpected considering the thick Venusian clouds. Because of the negligible humidity, the sugar lock system, employed on Venera 4 in case of a water landing, was abandoned in subsequent Venus probes.[5][9] The mission was considered a complete success, especially given several previous failures of Venera probes.[5] Although the Venera 4 design did allow for data transmission after landing, the Venera 3–6 probes were not built to withstand the pressures at the Venusian surface. The first successful landing on Venus was achieved by Venera 7 in 1970. See also{{Portal|Spaceflight}}
References1. ^1 Venera 1V (V-67). Encyclopedia Astronautica {{Venera}}{{Orbital launches in 1967}}{{Venus spacecraft}}{{DEFAULTSORT:Venera 04}}2. ^1 2 {{cite web|url=http://planet4589.org/space/log/launchlog.txt|title=Launch Log|first=Jonathan|last=McDowell|work=Jonathan's Space Page|accessdate=11 April 2013}} 3. ^{{cite web|url=http://nssdc.gsfc.nasa.gov/nmc/spacecraftDisplay.do?id=1967-058A |title=Spacecraft – Details |publisher=National Space Science Data Center |date= |accessdate=2013-11-05}} 4. ^{{cite book|pages=74|url=https://books.google.com/books?id=DulLuzqJLw8C&pg=PA74|title=New cosmic horizons|author=David Leverington|publisher=Cambridge University Press|year=2000|isbn=978-0-521-65833-1}} 5. ^1 2 3 4 5 6 {{cite web|url=http://www.laspace.ru/rus/venera4.php|accessdate=2009-07-07|title=Venera 4 (in Russian)}} 6. ^{{cite journal |author=V. M. Vakhnin|year=1968|title=A Review of the Venera 4 Flight and Its Scientific Program |journal=J. Atmos. Sci. |volume=25 |issue=4|pages= 533–534 |doi=10.1175/1520-0469(1968)025<0533:AROTVF>2.0.CO;2|bibcode = 1968JAtS...25..533V }} 7. ^[https://web.archive.org/web/20090807234459/http://www.novosti-kosmonavtiki.ru/phpBB2/viewtopic.php?t=1424&highlight=&sid=5900d3fa070e9b19160a25cbcde8d6a4 Photo of the lock]. novosti-kosmonavtiki.ru, 18 February 2005. 8. ^1 2 3 {{cite book|url=https://books.google.com/books?id=Fi1mCYJWBwAC&pg=PA56|pages=55–56|title=Robotic Exploration of the Solar System: The golden age 1957–1982|author=Paolo Ulivi, David Michael Harland|publisher=Springer|year= 2007|isbn=978-0-387-49326-8}} 9. ^1 2 3 4 5 {{cite book|pages=98–101|title=Russian planetary exploration|author=Brian Harvey|url=https://books.google.com/books?id=jKmIclMIwPAC&pg=PA101|publisher=Springer|year=2007|isbn=978-0-387-46343-8}} 10. ^{{Cite web |author= |date= |url=http://nssdc.gsfc.nasa.gov/nmc/spacecraftDisplay.do?id=1967-063A |title=Cosmos 167 |work=National Space Science Data Center |publisher=National Aeronautics and Space Administration }} 11. ^{{cite book|url=https://books.google.com/books?id=Fi1mCYJWBwAC&pg=PA63|page=63|title=Robotic Exploration of the Solar System: The golden age 1957–1982|author=Paolo Ulivi, David Michael Harland|publisher=Springer|year= 2007|isbn=978-0-387-49326-8}} 12. ^Mitchell, Don P., "Plumbing the Atmosphere of Venus". 2003. Accessed December 8, 2017. 13. ^David E. Reese and Paul R. Swan, [https://www.jstor.org/stable/1723876 "Venera 4 Probes Atmosphere of Venus"], Science, Vol. 159, No. 3820, Mar. 15 1968, pp. 1228-1230. Accessed December 8, 2017. 14. ^V. M. Vakhnin, "A Review of the Venera 4 Flight and Its Scientific Program", 1968. Accessed December 8, 2017. 15. ^M. E. Ash, D. B. Campbell, R. B. Dyce, R. P. Ingalls, R. Jurgens, G. H. Pettengill, I. I. Shapiro, M. A. Slade and T. W. Thompson, "The Case for the Radar Radius of Venus," Science, Vol. 160, No. 3831, May 31, 1968, pp. 985-987 16. ^Eshleman V.R., Fjeldbo G., Anderson J.D., Kliore A., and Dyce R.B., "Venus: lower atmosphere not measured", Science, 162 (3854), Nov. 8 1968, pp. 661-5. DOI: 10.1126/science.162.3854.661 ([https://www.ncbi.nlm.nih.gov/pubmed/17736042 abstract]). 5 : Venera program|Derelict landers (spacecraft)|Spacecraft launched in 1967|1967 in the Soviet Union|1MV |
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