<?xml version="1.0" encoding="UTF-8"?>
<?xml-model href="https://pds.nasa.gov/pds4/pds/v1/PDS4_PDS_1B00.sch" schematypens="http://purl.oclc.org/dsdl/schematron"?>
<Product_Context xmlns="http://pds.nasa.gov/pds4/pds/v1"
 xmlns:pds="http://pds.nasa.gov/pds4/pds/v1"  xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"
 xsi:schemaLocation="http://pds.nasa.gov/pds4/pds/v1 https://pds.nasa.gov/pds4/pds/v1/PDS4_PDS_1B00.xsd">
    
    <Identification_Area>
        <logical_identifier>urn:nasa:pds:context:instrument:vega1.puma</logical_identifier>
        <version_id>1.0</version_id>
        <title>DUST IMPACT MASS ANALYZER for VEGA1</title>
        <information_model_version>1.11.0.0</information_model_version>
        <product_class>Product_Context</product_class>
        <Alias_List>
            <Alias><alternate_title>urn:nasa:pds:context:instrument:puma.vega1</alternate_title></Alias>  <!-- deprecated LID -->
        </Alias_List>
        <Modification_History>
            <Modification_Detail>
                <modification_date>2021-02-24</modification_date>
                <version_id>1.0</version_id>
                <description>
                    Changed inst LIDs from
                      u:n:p:c:i:instID.scID to
                      u:n:p:c:i:scID.instID
                    And per "Guide toPDS4 Context Products" v1.7,
                    changed all lidvid_reference to lid_reference
                </description>
            </Modification_Detail>
        </Modification_History>
    </Identification_Area>

    <Reference_List>
        <Internal_Reference>
            <lid_reference>urn:nasa:pds:context:instrument_host:spacecraft.vega1</lid_reference>
            <reference_type>instrument_to_instrument_host</reference_type>
        </Internal_Reference>
        <External_Reference>
            <reference_text>
                   Reinhard, R and B. Battrick (eds), &apos;Space Missions to Halley&apos;s Comet&apos;, European
                   Space Agency ESA SP-1066, ESA Pub Div, Moordwijk, Netherlands, 1986.
            </reference_text>
            <description>reference.ESA-SP1066</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   Kissel, J., and F.R. Krueger, The Organic Component in Dust From Comet
                   Halley as Measured by the PUMA Massspectrometer on Board VEGA 1, Nature,
                   326, 755-760, 1987.
            </reference_text>
            <description>reference.KISSEL-KRUEGER1987</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   Kissel, J., Mass Spectrometric Studies of Halley&apos;s Comet, Advances in Mass
                   Spectrometry 1985, 175-184, 1986.
            </reference_text>
            <description>reference.KISSEL1986</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   Kissel, J., D.E. Brownlee, K. Buchler, B.C. Clark, H. Fechtig, E. Grun, K.
                   Hornung, E.B. Igenbergs, E.K. Jessberger, F.R. Krueger, H. Kuczera, J.A.M.
                   McDonnell, G.E. Morfill, J. Rahe, G.H. Schem, Z. Sekanina, N.G. Utterback,
                   H.J. Volk, and H. Zook, Compostition of Comet Halley Dust Particles From
                   GIOTTO Observations, Nature, Vol 321, No. 6067, 336-337, 1986.
                   6067, 280-282, 1986.
            </reference_text>
            <description>reference.KISSELETAL1986</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   Krueger, F.R., and J. Kissel, The Chemical Composition of the Dust of Comet
                   P/Halley as Measured by PUMA on Board VEGA-1, Naturwissenschaften, 74,
                   312-316, 1987.
            </reference_text>
            <description>reference.KRUEGER-KISSEL1987</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   Krueger, F.R., A. Korth, and J. Kissel, The Organic Matter of Comet Halley
                   as Inferred by Joint Gas Phase and Solid Phase Analyses, Space Science
                   Reviews, 56, 167-175, 1991.
            </reference_text>
            <description>reference.KRUEGERETAL1991</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   Langevin, Y., J. Kissel, J.L. Bertaux, and E. Chassefiere, First
                   Statistical Analysis of 5000 Mass Spectra of Cometary Grains Obtained by
                   PUMA 1 (VEGA 1) and PIA (GIOTTO) Impact Ionisation Mass Spectro Meters in
                   the Compressed Modes, Astronomy and Astrophysics, 187, 761-766, 1987.
            </reference_text>
            <description>reference.LANGEVINETAL1987A</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   Langevin, Y., J. Kissel, J.L. Bertaux, and E. Chassefiere, Impact
                   Ionisation Mass Spectrometry of the Cometary Grains On-Board VEGA 1 and
                   GIOTTO, VEGA 1, and VEGA 2 Spacecrafts, Lunar and Planetary Science XVIII,
                   533-534, 1987.
            </reference_text>
            <description>reference.LANGEVINETAL1987B</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   &apos;Encounters with Comet Halley, The first results&apos;, Nature, Volume 321, No.
                   6067, 15 May 1986.
            </reference_text>
            <description>reference.NATURE321</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   Sagdeev, R.Z., G.A. Avanesov, I.V. Barinov, A.I. Debabov, V.A. Krasikov,
                   V.I. Moroz, V.A. Shamis, V.I. Tarnopolski, D.A. Usikov, YA.L. Ziman, B.S.
                   Zhukov, F. Szabo, K. Szego, A. Kondor, E. Merenyi, B.A. Smith, S. Larson,
                   P. Cruvellier, A. Abergel, J.L. Bertaux, J. Blamont, M. Danz, D. Mohlmann,
                   H. Stiller, and H.P. Zapfe, Comet Halley: Nucleus and Jets (Results of the
                   Vega Mission), Advances of Space Research, 5, 95-104, 1986.
            </reference_text>
            <description>reference.SAGDEEVETAL1986A</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   Sagdeev, R.Z., G.A. Avanesov, I.V. Barinov, V.I. Kostenko, V.A. Krasikov,
                   V.A. Shamis, K.G. Sukhanov, V.I. Tarnopolski, YU.K. Zaiko, S.I. Zatsepin,
                   YA.L. Ziman, B.S. Zhukov, F. Szabo, L. Szabo, K. Szego, A. Balazs, G.
                   Endroczi, M. Gardos, M. Kanyo, Z. Nyitrai, I. Renyi, P. Rusznyak, B. Smith,
                   S. Szalai, I. Toth, L. Varhalmi, M. Zsenei, P. Cruvellier, M. Detaille, T.
                   Nguyen-Trong, A. Abergel, J.L. Bertaux, J. Blamont, E. Dimarellis, G.N.
                   Dulnev, G. Tsukanova, and B.I. Valnicek, TV Experiment in Vega Mission:
                   Strategy, Hardware, Software, Proceedings of the 20th ESLAB Symposium, ESA
                   SP-250, Vol II, 289, 1986.
            </reference_text>
            <description>reference.SAGDEEVETAL1986B</description>
        </External_Reference>
        <External_Reference>
            <reference_text>
                   Solc, M., V. Vanysek, and J. Kissel, Carbon Isotope Ratio in PUMA 1 Spectra
                   of P/Halley Dust, Astronomy and Astrophysics, 187, 385-387, 1987.
            </reference_text>
            <description>reference.SOLCETAL1987</description>
        </External_Reference>
    </Reference_List>
    
    <Instrument>
        <name>DUST IMPACT MASS ANALYZER</name>
        <type>Spectrometer</type> <!--RChen/EN was Mass Spectrometer-->
        <naif_instrument_id>not applicable</naif_instrument_id>

        <serial_number>not applicable</serial_number>

        <description>
 
 
    Instrument Overview
    ===================
 
      The dust mass spectrometer measures the chemical
      composition, the size and the spatial density of
      solid particles using a time-of-flight technique,
      with particular emphasis on the determination of
      the Li, C and B isotopic ratios.  The operating
      Principle of PUMA, illustrated in Figure 8a, is
      similar to that of the PIA instrument flown on
      Giotto.  The dust particles enter through a baffle
      and impact on a silver target (M) at a speed of 78
      km/s.  The particles and a certain amount of the
      target material are vaporized and partly ionized.
      The two Vega spacecraft have different targets; one
      type is mounted in a cartridge as in the PIA, the
      second has a corrugated surface such that a larger
      amount of projectile ions enter the analyzer.  The
      target is at + 1020 V; the ions are accelerated by
      a grid (1), which is held at a potential of -2000
      V, and enter the field-free drift tube at zero
      potential (4).  These charged particles are sent by
      the electrostatic reflector (5) into the second
      drift tube (6) and on towards the detector (7).
      The ions trajectories are focused by the lenses
      (9), (10) and (11).  A set of three electrodes
      (12), consisting of an inner grid at +1000 V
      between two grids at zero potential, prevents ions
      with energies less than 1 keV from reaching the
      detector.  The geometry of the reflector is
      designed in such a way as to bunch ions of the same
      species (particles with energies E&gt;E(0) travel a
      larger distance than those with energies E&lt;E(0))
      and to eliminate those with energies that deviate
      too much from E(0).  The purpose of this mirror
      system is to reduce the dispersion of the flight
      times for particles having the same charge-to-mass
      ratios.  The reflector potential is switch- between
      1000 V and 1100 V every 30 s, in order to
      compensate for the higher energies of ions created
      by the impacts of larger particles.  The
      time-of-flight is measured with reference to three
      signals: the light flash recorded by the
      photomultiplier (3), the pulses detected by the
      target (M), and the accelerating grid (1).  The
      signals induced in these sensors, in the first lens
      (9), in the ejecta trap (8) and in the detector
      (7), which are illustrated qualitatively in Figure
      8c, are used to characterize the mass of the
      particles.  Additional information about PUMA is
      given in the table below.
 
 
Table. Dust Mass Spectrometer characteristics
 
Target material                        Silver
Total drift lengt                      1 m
Time of flight                         4 micro s (H+) - 40 micro s (Ag+)
Ion detector                           Secondary electron multiplier
Dust mass range                        3x10**-16  -5x10**-10 g
Atomic mass range                      1-110 amu
Mass resolution, m/delta m,
       at m = 107                      200
Chemical composition accuracy
       per spectrum                    10%
Maximum data acquisition rate          12 spectra/s
Expected number of events              10**3-10**4 impacts during flyby
 
 

        </description>
    </Instrument>
</Product_Context>
