MASTER'S THESIS
Geometry Considerations for the Radio and Plasma Waves Instrument on the ESA Jupiter Icy Moons Explorer (JUICE)
Pedro Cervantes 2015
Master of Science (120 credits) Space Engineering - Space Master
Luleå University of Technology
Department of Computer Science, Electrical and Space Engineering
I would like to thank my supervisor Dr. Anders Eriksson (IRFu) for always being able to find a moment to assist and guide me during the course of this thesis. His knowledge and communication skills really helped me with the development of the project. I am also very thankful of his corrections and contribution of ideas to the document.
I also want to thank my supervisor and master program coordinator from LTU Dr.
Victoria Barabash. I really appreciate all the time and work she invested helping me find some funds to help support myself during my studies as well as finding a master thesis. The time she spend and the degree of detail in which she inspected this document is also much appreciated.
Finally, I want to express my gratitude to ESA’s Human Spaceflight and Operations Directorate and the Erasmus+ Programme of the European Union for co-funding this project.
i
Contents
Acknowledgements i
Abbreviations iv
1 Introduction 1
1.1 Introduction to the project . . . . 1
1.1.1 The JUICE Mission . . . . 1
1.1.2 The Radio Plasma Wave Instrument . . . . 2
1.2 Introduction to this document . . . . 3
2 Project Background 5 2.1 The Langmuir Probes . . . . 5
2.1.1 General principles . . . . 6
2.1.2 Bias voltage sweeps . . . . 9
2.1.3 Electric fields and waves . . . 10
2.1.4 Density fluctuations and plasma flow velocity . . . 12
2.1.5 Dust detection . . . 13
2.1.6 MIME . . . 13
2.2 Langmuir probe measurement disturbances . . . 14
2.2.1 The Shadow effect . . . 14
2.2.2 The Wake effect . . . 16
2.3 Project Objectives . . . 19
3 Model Design 20 3.1 Starting Point . . . 20
3.2 The Spacecraft Model . . . 22
3.2.1 The Spacecraft Dimensions . . . 22
3.2.2 The Langmuir Probes . . . 23
3.2.3 The Spacecraft Initial Position . . . 24
3.2.4 The Spatial Constraints . . . 25
3.3 The Shadow Model . . . 31
3.4 The Wake Model . . . 35
4 Results 41 4.1 Phase 4: Jupiter High Latitudes . . . 42
4.1.1 Shadow . . . 43
4.1.2 Wake . . . 45
ii
4.2 Phase 6: In-orbit around Ganymede . . . 47
4.2.1 Shadow . . . 49
4.2.2 Wake . . . 50
4.3 Overall Results . . . 51
4.3.1 Shadow . . . 51
4.3.2 Wake . . . 53
4.3.3 Shadow/Outside Wake . . . 54
5 Conclusions 56 5.1 Discussion of the results . . . 56
5.2 Final Remarks . . . 58
A Full results 59 A.1 Phase 1: PRM (Perijove raising maneuver) . . . 59
A.1.1 Shadow . . . 61
A.1.2 Wake . . . 63
A.2 Phase 2: EVI reduction (Energy, v
infand inclination reduction) . . . 65
A.2.1 Shadow . . . 67
A.2.2 Wake . . . 69
A.3 Phase 3: Europa Phase . . . 71
A.3.1 Shadow . . . 72
A.3.2 Wake . . . 74
A.4 Phase 4: Jupiter High Latitudes . . . 76
A.4.1 Shadow . . . 77
A.4.2 Wake . . . 79
A.5 Phase 5: Transfer to Ganymede . . . 81
A.5.1 Shadow . . . 82
A.5.2 Wake . . . 84
A.6 Phase 6: In-orbit around Ganymede . . . 86
A.6.1 Shadow . . . 88
A.6.2 Wake . . . 89
A.7 Phase 6: GCO-500 . . . 90
A.7.1 Shadow . . . 91
A.7.2 Wake . . . 92
A.8 Phase 6: GCO-200 . . . 93
A.8.1 Shadow . . . 94
A.8.2 Wake . . . 95
Bibliography 96
Abbreviations
AU Astronomical Unit
DC Direct Current
ESA European Space Agency EVI Energy Vinf and Inclination GCO Ganymede Circular Orbit GEO Ganymede Elliptical Orbit JUICE JUupiter ICy Moon Explorer
LP Langmuir Probe
LP-PWI Langmuir Probe - Plasma Wave Instrument MIME Mutual IMpedance Measurements
NAC Narrow Angle Camera PRM Perijove Raising Maneuver
RPWI Radio and Plasma Wave Instrument RWI Radio Wave Instrument
SCM Search Coil Magnetometer
S/C SpaceCraft
UV UltraViolet
iv
Introduction
1.1 Introduction to the project
1.1.1 The JUICE Mission
The JUICE (JUpiter ICy moon Explorer) is a European Space Agency (ESA) mission that will send a spacecraft to the Jovian system to perform a thorough investigation of Jupiter and some of its moons, in particular of Ganymede, Callisto and Europa.
There have been numerous ground and space based observations of the Jovian system, ever since Galileo discovered the four largest moons known today as Galilean Moons.
Since then, not only ground based observations have evolved enough to shed an enormous amount of light on this system, but also space exploration has developed to the point where a celestial body that is more than 5 AU from the Sun has been visited on several occasions, particularly by the Pioneer, Voyager and Galileo missions.[ESA, 2012]
Today we have a substantial amount of information about this system. However, there are a few strong reasons that led to the desire of taking it to the next level.
First, the scientific attractiveness of being able to characterize several potential habitable worlds ”in one shot”. Ganymede, Europa and Callisto are believed to posses internal liquid water oceans which reasonably makes them the central object of study when dealing with icy worlds potential habitability.
1
Chapter 1. Introduction 2
Secondly, the Jovian system can be compared to a certain extent to the entire Solar System. The dynamics of Jupiter’s magnetosphere and the electrodynamic coupling between the planet and its satellites can be of great help for being able to understand the dynamics of larger astrophysical bodies or systems. Jupiter will also serve as an archetype for an exoplanetary gas giant, which is also a very important piece of puzzle to understand the formation of the Solar System and our own habitable world.
1.1.2 The Radio Plasma Wave Instrument
The Radio Plasma Wave Instrument (RPWI) is one of the instruments selected by ESA to fly on board of JUICE [Wahlund, 2013]. The RPWI consists of a set of sensors (Figure 1.1) that measures the near DC electric field (Langmuir Probe-Plasma Wave Instrument or LP-PWI), the electric component of plasma waves (LP-PWI and Radio Wave Instrument or RWI), magnetic field component of electromagnetic waves (Search Coil Magnetometer or SCM), radio emissions (RWI) as well as some detailed character- istics of the thermal plasma (LP-PWI) including electric conductivity.
Figure 1.1. Current baseline configuration of RPWI.[ Wahlund, 2013]
The RPWI contributes to a wide range of the mission’s science objectives, which can be divided in 5 main points [ESA, 2012]:
• Determination of the electrical conductivity, properties and dynamics of the exo- spheric cold plasma of the moons and its effects on these moons surfaces.
• Characterize the particle populations within Ganymede, Europa and Callisto exo- spheres, the induced fields coupling to their conducting subsurface oceans and its interaction with Jupiter’s magnetosphere. Investigate Ganymede’s aurora genera- tion mechanisms.
• Contribute to characterize the surface composition of both icy satellites and the role of the internal (Ganymede) and induced magnetic field in controlling surface sputtering processes, and investigating subsurface outflow processes through direct in situ measurements of the ionized component of exhaust plumes if they do exist.
• Contribute to the study processes acting in Jupiter’s magnetodisc, study the large scale coupling process between Jupiter’s magnetosphere, ionosphere and upper atmosphere and study response to solar wind variability and the role of solar wind and planetary rotations on magnetospheric dynamics.
• Contribute to the characterization of the Jovian system radiation environment and its variability over time, radio emissions and contribute to the study of the auroral footprint of the moons.
The RPWI will focus on cold plasma studies and the global understanding of how through electrodynamic and electromagnetic coupling, the momentum and energy trans- fer occur in the Jovian system.[Wahlund, 2013]
1.2 Introduction to this document
In Chapter 1 an overview and the science objectives of the JUICE mission are is pre-
sented. Some of these objectives will determine the measurements that need to be taken,
and determine the conditions for the proper geometrical arrangement of the RPWI, hence
the importance of this section.
Chapter 1. Introduction 4
Chapter 2 is dedicated to a general overview of the basic modes of Langmuir Probe operation. A qualitative explanation of how the spacecraft (S/C) wake and the shadow periods disturb the plasma environment is given. This chapter provides an insight of why different geometrical configurations and plasma disturbances are key factors to consider if plasma measurements are to be taken by the instrument. Finally, the objectives of this project are presented.
Chapter 3 covers the creation process of the simulation model from the starting point, i.e. a few points stored in a database, to a fully functional 3D simulator which is able to ascertain the position of any of the Langmuir probes and whether it is going to be in an undisturbed plasma or not.
Chapter 4 presents the simulation results, i.e. relevant plots and statistics for the whole JUICE mission. Due to the extremely repetitive nature of some results, only a couple of phases will be presented on this chapter, saving the whole series for Appendix A.
Chapter 5 contains the discussion of the results, the conclusions and other remarks.
Appendix A includes all the results omitted in Chapter 4.
Project Background
2.1 The Langmuir Probes
A Langmuir probe is a conductor used to determine the electric potential, electric tem- perature and electric density of a plasma. By introducing one or more electrodes in the plasma and varying the electric potential among the probes or between them and the spacecraft, different properties of the plasma can be obtained analyzing the mea- sured potentials and currents in each mode. The LP is a widely used instrument in space missions. The Cassini mission to Saturn and the Rosetta mission to the comet Churyomov-Gerasimenko include some of the most recent predecessors of the RPWI.
Figure 2.1. Picture of one of the Langmuir probes on board of Rosetta. Image by [Swedish Institute of Space Physics, http://www.space.irfu.se/rosetta/galleri.html].
The RPWI will include four probes, which consist of four 50 mm (diameter) identical spheres of titanium with a golden surface layer of titanium nitride. Each probe is mounted on a 200 mm long titanium stub also coated in titanium nitride, as shown in Figure 2.1. The stubs are mounted on 3 m long (approximately) booms, which are
5
Chapter 2. Project Background 6
attached to the spacecraft body. The positioning of these booms (and the probes) with respect to the spacecraft is the main issue motivating this study.
2.1.1 General principles
Assuming a spherical probe smaller than the Debye length and that the probe is at rest with respect to the plasma, the electron I
eand ion current I
iexpressions are[H¨ oymork, 2002]:
Positive probe potential:
I
e= I
e0(1 − χ
e) (2.1)
I
i= I
i0e
−χi(2.2)
Negative probe potential:
I
i= I
i0(1 − χ
i) (2.3)
I
e= I
e0e
−χe(2.4)
where
χ
j= q
jV
P Pk
BT
j(2.5) and
I
j0= −A
Pn
jq
js
k
BT
j2πm
j, (2.6)
where A
Pis the area of the probe, j is the index that denotes the corresponding particle
species, n is the number density of the surrounding plasma (number of free electrons
and ions per unit volume), q is the charge, k
Bis the Boltzmann constant and T is the
particle species temperature. The probe potential with respect to the plasma is given
by:
V
P P= V
probe− V
plasma. (2.7)
In addition to electron and ion currents, a sunlit probe will also emit a photoelectron cur- rent. The solar incoming UV photons will knock out electrons from the probe provided that they carry sufficient energy to trigger this process. Then, depending on whether the probe’s potential is negative or positive, the emitted photoelectrons will be ejected away from the probe or attracted back respectively, as illustrated in Figure 2.2 (showing a positive probe). Note that in the case of the positive potential, if the emitted electron has sufficient energy it can overcome the potential and eventually escape the probe’s field. This effect is of special importance in tenuous plasmas, since the photocurrent becomes dominant for the negative potential region.
Figure 2.2. Photoelectric effect on the Langmuir probe. Image by [Swedish Institute of Space Physics, http://cluster.irfu.se/efw/ops/dummies, downloaded 2013-03-06].
Once this effect has been described, it is much easier to make sense out of the current- voltage or I-V curves and the effect that the photocurrent has on them. Figure 2.3 illustrates the difference between two I-V curve examples from the Langmuir probe instrument (LAP) on board of Rosetta.
It can be seen that the photocurrent for the negative potential reaches a constant value
fairly quickly, given that at a certain point all electrons can escape the probe regardless
of how negative the potential is, reaching a saturation point.
Chapter 2. Project Background 8
Figure 2.3. Top: I-V curve with no photoelectron current. Bottom: I-V curve with photoelectron current.[Billvik, 2005]
I
ph= −I
ph0, V
probe< 0 (2.8)
For a positive potential the current value goes to zero very fast; while the potential
value is still small (compared to the typical energy of a photoelectron at emission),
some electrons might still have enough energy to escape the probe and still remain as a significant photocurrent value, but at some point this is not possible anymore, resulting in a null current. Also note how the photoelectron current creates a stable low impedance zone in the curve; where the slope becomes the steepest. This low impedance connection to the plasma is necessary when useful electric field measurements need to be taken. The following equation is used to describe approximately the exponential decay of the photocurrent with the increase of the potential:
I
ph= I
ph0(1 + V
P PV
ph)e
−VP P
Vph
, V
P P> 0 (2.9)
Finally, the total current for a sunlit probe becomes:
I = I
e+ I
i+ I
ph(2.10)
To highlight the relevance of this study with respect to the Langmuir probes functioning, it is important to have a basic understanding of how these operate and their main operating modes. Keep in mind that the only goal of this description is to provide an overview of the basic parameters that can be measured by Langmuir probes as well as the physical quantities upon which these measurements depend on. For a more detailed description, see chapter 7 from [H¨ oymork, 2002] and [Merlino, 2007].
2.1.2 Bias voltage sweeps
The bias voltage sweep mode is used to estimate both ion and electron temperature as well as the densities. The bias voltage of the probe with respect to the spacecraft V
biasis swept over an interval from a negative to a positive value while at the same time the
current is being measured. This will generate a current function dependent on the bias
voltage, which is then represented as a current-voltage or I-V curve. As can be seen in
Equations (2.1) - (2.10) above and also illustrated in Figure 2.4, this current depends
on the plasma parameters n and T , so we can use the sweep to derive these parameters.
Chapter 2. Project Background 10
Figure 2.4. I-V curve example for electrons. Note how the slope of the curves in the linear region of the positive bias is characteristic for every pair of density and temperature values, as well as how the exponential decay with increasingly negative voltage below V = 0 depends on the electron temperature T
e.[Wahlund, 2013]
The values for n
i, n
e, T
iand T
ecan then be derived combining equations 2.1-2.6 and assuming that T
e>> T
iand m
e<< m
i.
2.1.3 Electric fields and waves
The variation of the electric field can be estimated by using a constant bias current on the probe. The quantity that is measured is the potential between the probe and the spacecraft, V
P S. The bias is chosen in order to have the resistance between the probe and the plasma as low as possible, which is the point where the I-V curve is steepest.
Due to the high sensitivity to fluctuations in the spacecraft potential for a single probe, usually two probes are used separated by a distance ~ d.
δE
m= V
P S2− V
P S1d ' ~ δE
t· ~ d (2.11)
where δE
mis the measured electric field, V
P Siis the spacecraft-probe with index i potential difference and ~ δE
tis the true electric field. “In practice, the measured voltage difference will also be affected by differences between the probes and their environments, and the presence of the spacecraft can significantly change the ideal dependence on ~ δE
t[Pedersen, Mozer, and Gustafsson, 1998]”
This double-probe setup has much less sensitivity to fluctuations in the spacecraft po- tential, but also requires that the changes in the potential of the field vary slowly enough in space to be able to be resolved with the chosen separation distance of the probes.
In other words, only fluctuations with wavelengths much larger than d (∼ 6 m) will be correctly measured.
The LPs allow measurements of full electric field from DC up to 1.6 MHz (measurement frequency). This range has never been possible to achieve on previous missions to outer planets, which makes it even more of a crucial key factor to be able to meet the science goals. Furthermore, it is required to have the 4 LPs extended as far as possible from each other and from the spacecraft, i.e. in a diverging configuration, since the LPs should avoid contamination from the photoelectron cloud surrounding the spacecraft and the solar panels. It is also important to keep the configuration as symmetric as possible. In addition, there are several other effects that will condition the measurement performance, i.e. photoelectron emission from the spacecraft, differential charging of large insulating surfaces, asymmetric surfaces affecting the S/C potential pattern and the plasma environment itself. It is also important that the exterior surfaces of the spacecraft as well as the solar panels are conductive to limit the disturbances.
Depending on the geometrical configuration of the LP, different magnitudes can be mea- sured. If the LP directions span a volume, the full electric field vector can be obtained.
If on the other hand all probes happen to be on a plane, it is possible to measure a
2-dimensional electric field. Then it can be used to determine the full 3-dimensional
electric field assuming that the electric field component parallel to the ambient mag-
netic field is small, which works well for low frequency plasma processes. If there is at
least two probes on a plane, it is possible to use interferometry to measure the phase
speed of waves supported by the electric field, since each pair of probes will measure
a phase different than the other pair, which is eventually used to compute the wave
vector.[RPWI-Consortium, 2013]
Chapter 2. Project Background 12
If instead of the potential difference between two probes, we introduce the spacecraft body as a third probe and measure its respective potential differences with the two probes P
1and P
2collinearly, the phase difference of the two signals can be used to deduce the component of the wave vector ~ k project along their common axis. Logically this setup will be sensitive to spacecraft potential fluctuations, since both differences, V
P1− V
S/Cand V
P2− V
S/C, depend explicitly on this potential. This drawback can be easily overcome if instead of the spacecraft body we introduce two additional probes.
With two double probes the setup becomes essentially independent of V
S/C.
All these constraints for the probes are crucial to understand the relevance of this study, since they will determine the starting point in regards of the optimal LP configuration.
2.1.4 Density fluctuations and plasma flow velocity
If a probe is biased with a positive potential V
P Srelative to the S/C, the relative plasma density fluctuations δn/n can be obtained by sampling the current fluctuations at the probe. The resistance has to be as high as possible, making the measurements less sensitive to fluctuations in the potential. Assuming that n is proportional to the current I and that the current fluctuations are small with respect to the magnitude of the intensity, the following expression holds:
δI I = δn
n (2.12)
If instead of a single probe, one uses a pair of them separated by a distance d, they can
be used as an interferometer. The temporal delay between two signals on each probe can
be used to estimate the plasma flow velocity. If this is done with several non-coplanar
probe pairs, the full velocity vector can computed.
2.1.5 Dust detection
Another interesting application of the LP is the detection of micrometer sized dust particles. The impact between a dust particle and the surface of the spacecraft can take place at a relative velocity of a few tens of kilometers per second (due to the orbital velocities of S/C and dust particle), which in turn translates into a large impact energy.
This energy is enough to vaporize the particle and even to partially ionize the released gas, typically reaching temperatures ∼ 10
5K [H¨ oymork, 2002]. This expanding wave of newly formed plasma is then detected by the probe as a δE pulse in the kHz region.
The charge collected by the probe is proportional to the mass of the original impacted dust grain and therefore it can be estimated using the relation:
Q = km (2.13)
where Q is the charge, m the mass of the dust particle and k is a constant that contains the relative velocity of the impact, the material of the impact surface, composition of the dust particle and the angle of incidence among other factors. [H¨ oymork, 2002]
2.1.6 MIME
The last example of measurement technique is the MIME (Mutual Impedance Measure-
ments). It consists of a pair of LPs transmitting a stimulating signal which is then
received by the other pair of LPs. By sweeping across different frequencies, the fre-
quency response of the plasma can be obtained. This is used to measure the complex
impedance of the plasma, which dictates what kind of wave modes can be supported by
that plasma. For example, the local electron plasma density can be calculated from the
local electron plasma resonance frequency, which is derived from a sharp peak in the
MIME frequency spectrum [RPWI-Consortium, 2013]. Since this electron density mea-
surement is determined with high accuracy, it is then used to calibrate density estimates
obtained by other subsystems/techniques.
Chapter 2. Project Background 14
2.2 Langmuir probe measurement disturbances
2.2.1 The Shadow effect
The first disturbance considered in this study will be the shadow casted over the LPs by the body and/or solar panels of the S/C. Please note that the terms shadow and eclipse will be used interchangeably in this context from now on, unless explicitly indicated otherwise.
Figure 2.5. Artist impression of a spacecraft orbiting Jupiter. Differentially lit sur- faces can be distinguished along the spacecraft. Credit: NASA
Technically speaking, the effects of the shadow affect the probe’s functioning, rather than the plasma itself. The eclipse time that a certain volume of plasma undergoes with the passage of the S/C is not enough to alter the plasma parameters in a substantial way. In other words, if we think of this eclipsed portion of the plasma as the volume
“illuminated” by the spacecraft shadow, one can see that the S/C, moving at speeds of several km/s, will be shadowing completely different parcels of plasma approximately each millisecond, assuming length scales for the LPs of a few meters.
Therefore, the main contrast of a sunlit region versus an eclipsed one is the photoelec-
tron density. The sunlit region of the spacecraft will be emitting photoelectrons, which
will form a frontal cloud of electrons. This means that from the point of view of the
instrument, the electron density is higher in this cloud than on the surrounding plasma
not affected by S/C. However, this asymmetry is neither necessarily beneficial nor in- convenient for the instrument: it actually depends on the operation mode for the probes we intend to execute at that moment.
Let us begin with the advantage of having the probe/s in sunlight. It has already been explained that a sunlit probe will emit a photoelectron current and also how this is desirable to achieve a stable low-impedance connection to the plasma if electric field measurements are to be taken. However, even in shadow one could find a region where the I-V curve is steepest. The major difference is that if there is a part of the curve dominated by I
phit is independent of n, such that any possible density fluctuations will not affect the E-field measurements.
On the other hand, the mutual impedance and LP sweep measurements might benefit for being in shadow, since there is less contamination from photoelectrons. After all, a photoelectron is simply a regular electron renamed for the only purpose of indicating its source and therefore for most applications and specially from the point of view of the instrument there is no difference between them. Consequently, if the measurements we are taking are dealing with electron frequencies, they might be affected by an external source of electrons, contaminating the space plasma we want to measure. This would result in spurious electron densities.
Another undesired effect is the asymmetric illumination of two probes performing electric field measurements. A sunward facing probe will emit its electrons away from the boom, since the lit face of the sphere is in the opposite side of the boom-probe joint and also the boom’s shaft. Conversely, a probe facing away from the Sun, will have the boom in the same plane of illumination and therefore some of the photoelectrons emitted by the probe will be captured again by the boom. This will generate an asymmetric electric field in the Sun’s direction, which can lead to spurious electric field measurements [Pedersen, Mozer, and Gustafsson, 1998].
All these effects lead to the conclusion that a precise knowledge of the position of each
probe with respect to the Sun and the S/C body is of vital importance if one wants to
plan beforehand the right times to perform each type of measurement.
Chapter 2. Project Background 16
2.2.2 The Wake effect
Similarly to an aircraft in the terrestrial atmosphere, a spacecraft also generates a wake in its pass through space. However, the properties of the two fluids, air and plasma, are radically different and so is the behavior of the two wakes. Nevertheless the basic physical principle behind this effect is still the same and the same result holds under a qualitative comparison; a region of lower particle density is generated behind the vehicle’s body.
Figure 2.6. Numerical simulation of the wake behind a spacecraft. Top: XZ-plane projection. Bottom: XY-plane projection. The S/C is modeled as a box with two rectangular solar panels on each side. The relative velocity between the S/C and the plasma is along the x direction.[Sj¨ ogren, 2009]
In the simulation shown in Figure 2.6, it can be clearly seen how this density-altered
regions are very significant in size relative to the spacecraft span (35 m). Assuming the
Langmuir probes are mounted on booms of about 2-3 meters, in general there will be
periods in which at least one probe will be inside the wake, given that the length scale
of this disturbance will generally be more than a few meters.
In the case of a spacecraft traveling through plasma, the thermal speed of the ions usually cannot keep up with the velocity of the vehicle, resulting in the effect of the ions and electrons being swept away. In other words, the ions cannot refill the void left by the spacecraft in its pass fast enough to prevent the formation of a substantial wake.
The thermal speed v
thcan be defined as:
v
th=
r 2K
BT
m (2.14)
where k
Bis the Boltzmann constant, T is the particle species temperature and m the mass of the particle. Therefore, the intensity of the wake will strongly depend on these two parameters. Nevertheless, as far as the RPWI is concerned we are only going to be dealing with cold plasma (K
BT
i= 0.02 − 20 eV), where the most common species consist of various charge states of S and O [Saur et al., 1998]. Therefore, the range of ion thermal speeds that JUICE will be most likely to encounter can be estimated by taking the two opposite extreme cases:
• O
+and K
BT
O+= 20 eV:
v
th= q
2KBTO+
mO+
=
q
2·2016·1.0344·10−8
= 1.55 · 10
4m/s = 15.5 Km/s
• S
+and K
BT
S+= 0.02 eV:
v
th= q
2KBTS+
mS+
=
q
2·0.0232·1.0344·10−8
= 347.62 m/s = 0.347 Km/s
On the other hand, the spacecraft will be orbiting Jupiter with a range of velocities v
S/C= 4 − 14 Km/s (from SPICE kernels data). One can see that the two ranges of velocities, v
S/Cand v
thhave a big overlap, which would imply a very weak wake at the most, given that the thermal speed of the ions will be always in the order of the S/C velocity (except for the least energetic particles).
However, one must not forget that the plasma is corotating with Jupiter. The bulk velocity of this plasma at 10 Jupiter radii (roughly the closest approach of JUICE to Jupiter) is given by:
v
bulk= ω · 10 · R
J= 1.7610
−4· 10 · 71492 = 125.72 Km/s
Chapter 2. Project Background 18
where ω is Jupiter’s angular velocity in rad/s and R
Jis Jupiter’s radius in Km. It can be seen that even at this point, where the difference between the speed of the spacecraft and the bulk velocity of the corotating plasma is minimal, there is still one order of magnitude of difference between the two. Therefore, the effect of the spacecraft velocity to the wake can be neglected and the effect of the bulk velocity of the corotating plasma can be considered as the sole cause.
It can also be observed that v
bulkv
th, thus it is fair to assume for the purpose of this project that a wake significant enough in size will form at all times during the trajectory of JUICE.
Another effect that has to be taken into account is the local space charge that appears in the wake. Due to the much higher thermal velocity of the electrons (since they have a much smaller mass), the ion wake will be filled by the electrons, thus creating a local charge. The thermal velocity for the electrons, for the case of the coldest plasma K
BT
i= 0.02 eV, is given by:
v
th= q
2KBTe−
me−
=
q
2·0.025.678·10−12
= 8.39 · 10
4m/s = 83.93 Km/s
This thermal speed is in the same order of magnitude as the speed of the Jupiter coro- tating plasma. However, so far only the extreme case of JUICE’s closest approach with the encounter of the coldest part of the plasma’s temperature range has been consid- ered. During JUICE’s journey, both the electron thermal speed and the speed of the corotating plasma will be constantly changing, as the spacecraft moves closer or further away from Jupiter. Hence, the extent up to which the wake is filled with electrons will also be a variable.
Consequently, we will have a local charge in the wake that will be constantly changing, and so will the potential this charge generates. This effect will cause disturbances in the electric field that will make any attempts to make measurements futile.
Finally, these disturbances of the plasma will affect all of the LP measurement modes.
Consequently, it is going to be desirable to come up with a design where no more than
two probes are going to be inside the wake for long periods of time.
2.3 Project Objectives
This master thesis has the following goals:
1• Create a mathematical code that is capable to simulate the whole trajectory of the JUICE mission, as well as the shadow and plasma wake created by the S/C in its course.
• Provide a set of useful results from the design point of view regarding the ade- quateness of any feasible Langmuir probe configuration, both custom chosen and the ones designed by the two companies competing for the S/C construction based on a prediction of wake and sunlight conditions at the probes. In other words, the results should be able to provide with hints about which configuration aspects are of importance for the instrument to contribute to the fulfillment of the science objectives described in Chapter 1.
• Extend the code to be able to be easily tailored to any other current or future mission, not only JUICE.
1Note that some objectives are constrained by the fact that the two configurations from the Consortia cannot be disclosed in this document. Therefore, even though they are still project objectives, they might not be described in this document.