Objects with recently assigned numbers/names: 1994 JQ1 (16684)
There were 42 new TNO discoveries announced since the previous issue of the Distant EKOs Newsletter:
2000 PA30, 2000 PB30, 2000 PC30, 2000 PD30, 2000 PE30, 2000 PF30, 2000 PG30, 2000 PH30, 2000 PJ30, 2000 PK30, 2000 PL30, 2000 PM30, 2000 PN30, 2000 PU29, 2000 PV29, 2000 PW29, 2000 PX29, 2000 PY29, 2000 PZ29, 2000 QB226, 2000 QC226, 2000 QD226, 2000 QE226, 2000 QF226, 2000 QG226, 2000 QH226, 2000 QJ226, 2000 QL226, 2000 AB255, 2000 AC255, 2000 AD255, 2000 AE255, 2000 AF255, 2000 PQ30, 2000 PR30, 2000 OH67, 2000 OJ67, 2000 OK67, 2000 OL67, 2000 OM67, 2000 ON67, 2000 QA243
and 6 new Centaur/SDO discoveries:
2000 QK226, 2000 PS30, 2000 QB243, 2000 QC243, 2000 OO67, 2000 OP67
and 2 reclassified objects:
2000 OY51 (SDOTNO),
2000 PF30 (TNOSDO)
Current number of TNOs: 329 (and Pluto & Charon)
Current number of Centaurs/SDOs: 55
Starting with this issue, I will be including a new section: ``Other Papers of Interest''. The intention is to make note of papers that, though not directly related to the Kuiper belt/Centaurs/Pluto, may be of interest the readers of this Newsletter. When I started Distant EKOs, I explicitly wanted to avoid getting too far off topic, since my goal was to provide a focused resource for Kuiper belt studies. Now that this seems to be reasonably well established, I think it would be appropriate to encourage some cross-communication. Only the titles, author list, publication info, and contact/reprint links will be included for these other papers.
I would be interested in any feedback from readers regarding the editorial policy to include full abstracts only for accepted papers, and not include abstracts for submitted but not yet accepted papers, conference papers, other papers of interest, etc. Let me know if you would like to have full abstracts for all or some of those submissions (thus increasing length of each issue), or if you prefer the current format.
We investigate the orbital evolution of both real and hypothetical Edgeworth-Kuiper Objects in order to determine whether any conclusions can be drawn regarding the existence, or otherwise, of the tenth planet postulated by Murray (1999). We find no qualitative difference in the orbital evolution, and so conclude that the hypothetical planet has been placed on an orbit at such a large heliocentric distance that no evidence for the existence, or non-existence, can be found from a study of the known Edgeworth-Kuiper Objects.
Published in: Monthly Notices of the Royal Astronomical Society, 318, 101
For preprints, contact s.c.brown@qub.ac.uk
or on the web at http://www.blackwell-synergy.com/Journals/toc.asp?IssueID=3649
We have investigated excitations of orbital eccentricities and inclinations of
Kuiper Belt objects (KBOs) caused by the sweeping secular resonances during the
primitive solar nebula depletion. Since nebula gravitational potential rotates
the longitudes of perihelia and the ascending node, the nebula depletion leads
to migration of secular resonances. In the outer (classical) Kuiper belt (the
region beyond 42 AU), inclinations and eccentricities are respectively
distributed up to 0.6 (radian) and 0.2, and their root mean squares are about
0.2 (radian) and 0.1. These large values are not explained by present
planetary perturbations alone. We have investigated the sweeping secular
resonances in the Kuiper belt with both direct orbital integration and
analytical method and found that the sweeping secular resonances can account
for the eccentricity and inclination in the outer belt. Inclinations of
objects in the outer belt are excited to the observational level if the
residual nebula with about 0.1% of the density in the minimum mass nebula
model is depleted in a timescale of 107-108 years. For inclination
excitation, Jovian perturbations and nebula potential is the most important and
Neptunian perturbations do not play an important role during the residual
nebula depletion, although Neptune with more than 1/5 of present mass is needed
for enough eccentricity excitation. If further observation of the KBOs at
semimajor axis
50AU confirms our model, it would give
important clues about Neptune formation and the depletion of solar nebula.
To appear in: The Astronomical Journal
For preprints, contact nagasawa@geo.titech.ac.jp
or on the web at
http://www.geo.titech.ac.jp/nakazawalab/nagasawa/mypaper/nandi2000.html
We describe gravitational stirring models of planetary debris disks
using a new multi-annulus planetesimal evolution code. The current
code includes gravitational stirring and dynamical friction; future
studies will include coagulation, fragmentation, Poynting-Robertson
drag, and other physical processes. We use the results of our
calculations to investigate the physical conditions required for
small bodies in a planetesimal disk to reach the shattering velocity
and begin a collisional cascade. Our results demonstrate that disks
composed primarily of bodies with a single size will not undergo a
collisional cascade which produces small dust grains at 30-150 AU
on timescales of 1 Gyr or smaller. Disks with a size distribution
of bodies reach conditions necessary for a collisional cascade in
10 Myr to 1 Gyr if the disk is at least as massive as a minimum mass
solar nebula and if the disk contains objects with radii of 500 km
or larger. The estimated
500 Myr survival time for these
disks is close to the median age of
400 Myr derived for
nearby stars with dusty disks.
To appear in: The Astronomical Journal (2001 January)
For preprints, contact skenyon@cfa.harvard.edu
or on the web at http://xxx.arXiv.org/abs/astro-ph/0009185
We explore the possibility of detecting small Kuiper Belt Objects (KBO) by
serendipitous observation of stellar occultations: We show that such
unpredictable occultations may allow us to detect a population of very small
objects (typically of 100 m radius at 40 AU), invisible by any other
observational method, as long as (i) the assumed population fills up a
sufficient area on the sky plane, (ii) the instrumental sensitivity and
acquisition frequency are high enough and (iii) the observed star has a small
angular radius. This result is basically due to the diffractive broadening of
the geometric shadow of small (assumed numerous) occulting objects. This
diffractive broadening is more pronounced for smaller stellar disks and better
photometric precision. Assuming there exist about 1011 objects of radius
km, located between 30 and 50 AU near the Ecliptic, and that the
differential size distribution varies as
with the index q = 4extending down to decameter-sized objects, we expect a number of valid
occultations (i.e., a
event) between a few to several tens per night,
if we may obtain an r.m.s. signal fluctuation
and observe a
star in the ecliptic with an angular radius
0.01 mas. Since this
occultation rate is very sensitive to the index slope q and plummets when
,
a KBO occultation observation campaign could provide a decisive
constraint on the actual slope of the KBO size distribution for
sub-kilometer-sized objects. Blue O class stars are the best candidates for
detecting KBOs since they have the smallest angular radius for a given visual
magnitude. The occultation events are typically very brief (
1 s) and they
are shorter but more numerous when observed in the antisolar direction, so
rapid photometry(>1 Hz) is required and high speed photometry(
Hz) is
preferred. The French space mission Corot will provide an excellent opportunity
to observe occultations by KBOs using high precision photometry.
Published in: Icarus, 147, 530 (2000 October)
For preprints, contact roques@obspm.fr
or on the web at http://despa.obspm.fr/~roques/odksweb.html
We have conducted a large-area search for the brightest members of the Transneptunian and Centaur/Scattered-Disk asteroid populations by reprocessing archival scans from the Spacewatch 0.9 meter telescope at Kitt Peak. Our survey encompasses 331 scans taken from September of 1995 to September of 1999 and has a raw sky coverage of 1483.8 square degrees. We discovered five Transneptunians and five Centaur/Scattered Disk objects using an automated motion detection code. In addition, we serendipitously found four Transneptunians and two Centaur/Scattered-Disk objects that had been previously discovered. This survey is unique in that it involves a method which has a reasonable chance to re-acquire its lost objects.
In this paper we develop techniques to aid our understanding of our software
efficiency and survey procedures. We use this understanding to ``convolve" our
raw sky coverage with our measured detection efficiency and a model of our scan
coverage to estimate what fraction of survey areas can be considered ``new".
Our large sky coverage extends the cumulative luminosity function of the
Transneptunians into a region previously constrained only by upper limits and
allows a power law fit to be attempted to the Centaur cumulative luminosity
function. In objects per square degree brighter than R=21.5, we find
cumulative surface densities of Centaurs to be
,
of
Transneptunians to be
and Scattered Disk Objects to be
.
We extrapolate these values to estimate the number of each class
in the Ecliptic brighter than R=21.5: 100 Centaurs, 400 Transneptunians, and
70 Scattered Disk Objects.
Orbit analysis by the Minor Planet Center suggests that three of our five Transneptunians are resonators: 1998 VG44 is in the 3:2, 1995 SM55appears to be in the 5:3, and 1998 SN165 appears to be in the 7:5 resonance.
To appear in: The Astronomical Journal
For preprints, contact jlarsen@lpl.arizona.edu
We present the results obtained by the simulations of different thermal models of 5145 Pholus, one of the known Centaurs. Pholus orbit is highly eccentric, similar to that of comets but its dimension is more similar to larger asteroids. Pholus cannot be clearly numbered into either class. The most likely source of Centaurs is the Edgeworth-Kuiper Belt: dynamical studies and physical properties suggest that Pholus recently entered in the planetary zone. Here we assume that the nature of Pholus is that of a cometary body made by different ices and dust. We have computed the thermal evolution of this object under different conditions: as a ``new'' object, namely an undifferentiated body, and an ``old'' one, differentiated and aged in the Kuiper Belt. We have tried to see also the effects induced by the presence of an organic dust on the overall evolution. Both the ``new'' and the ``old'' object show low, but different, levels of gas activity.
Published in: Astronomical Journal, 120, 1571 (2000 September)
For preprints, contact M.C. De Sanctis at cristina@ias.rm.cnr.it
or on the web at
http://www.journals.uchicago.edu/AJ/journal/issues/v120n3/200048/200048.html
Near-infrared, 1-2 m, spectra of the Centaur 8405 Asbolus (1995 GO)
have been obtained by HST/NICMOS. Strong and variable absorption
features indicate a significantly inhomogeneous surface characterized by water
ice mixed with additional unknown constituents. Over a 1.7 hour interval, the
observed spectra varied from nearly featureless to a very complicated
absorption spectrum and the integrated flux varied in a manner consistent with
previous lightcurve observations. The accepted rotation period of 8.9351 hours
assumes a shape-dominated lightcurve. Our observations indicate that the
lightcurve may in fact be albedo-dominated with a period of 4.47 hours, i.e.,
half the previous value.
Published in: The Astrophysical Journal Letters, 542, L155 (2000 October 20)
For preprints, contact susank@olympus.as.arizona.edu
or on the web at
http://www.journals.uchicago.edu/ApJ/journal/issues/ApJL/v542n2/005502/005502.html
See also: http://oposite.stsci.edu/pubinfo/PR/2000/31/index.html
We present new 1.4-2.5 m geometric albedo spectra of Charon taken
with HST/NICMOS in 1998. These new data provide global coverage of the
surface with four spectra at evenly spaced longitudes. The surface of
Charon is seen to be globally dominated by H2O ice. The data indicate
the ice is in the crystalline phase at a temperature consistent with its
heliocentric distance. The spectrum of Charon has only weak variations
with longitude. There is an indication of a slightly stronger H2O
ice absorption on the leading hemisphere. No variations in the spectrum
are seen in response to differing solar phase angle. From model fits
there is no indication of any of the volatile species that are seen on
Pluto, i.e., CO, CH4, or N2. There is spectroscopic evidence
for a contaminant with an absorption coefficient which increases with
wavelength past
2
m. This contaminant is unidentified but is
similar to what is seen on other icy satellites in the outer solar system.
We also present a standard spectrophotometric model for Charon that
can be used to subtract Charon light from ground based spectra of the
combined Pluto-Charon system.
To appear in: Icarus
For preprints, contact buie@lowell.edu
We present the results of the near-infrared spectroscopy of the Pluto-Charon
system, conducted in the K band at two different sub-Earth longitudes. The
spatially resolved images resulted in separated spectra with a spectral
resolution of approximately 530. The spectrum of Charon showed a broad
absorption feature at 2 m during both orbital phases, suggesting a uniform
distribution of water ice. In the separated spectrum of Pluto obtained in June,
we confirmed the absorption bands of solid methane, carbon monoxide, and
nitrogen ices. Additional weak dips have been found at 2.28, 2.32, and
2.40
m in the spectrum of the opposite side observed in May. In order to
examine the carrier of these dips, we performed model calculations of the
reflectance of Pluto using Hapke's bidirectional reflectance model for icy
intimate mixtures. By adding a small amount of solid ethane into the mixture,
we successfully reproduced the dips at 2.28 and 2.31
m, but the absorption
at 2.40
m is more distinct than that in the observed spectrum.
Published in: Publications of the Astronomical Society of Japan, 52, 551
For preprints, contact ryo@eorc.nasda.go.jp
Nitrogen ice, probably the dominant high albedo surface material on Pluto
and Triton, has optical constants that are more strongly absorbing in
the thermal infrared than at visible wavelengths. This optical behavior
results in absorption of sunlight, on average, at greater depths than
the depths from which thermal emission emerges, producing a vertical
imbalance between heating and cooling of a sunlit nitrogen ice surface.
Assuming the ice is sufficiently permeable to gas flow that the bulk
ice is in vapor pressure equilibrium with the nitrogen atmosphere, this
vertical distribution of heating and cooling drives net sublimation at
depth and condensation closer to the surface. Over time scales much
shorter than seasonal time scales on Triton and Pluto, this process
of solar gardening will tend to produce a characteristic textural and
compositional distribution which has important photometric, spectroscopic,
and seasonal consequences. Solar gardening may help explain several
previously puzzling observations including the anomalously strong
spectral absorption by methane ice in spectra of Triton and Pluto in
the 0.7-1.1 m range and the surprising persistence of Triton's south
polar cap at low latitudes during southern summer.
To appear in: Icarus
For preprints, contact grundy@lowell.edu
or on the web at http://www.lowell.edu/users/grundy/gardening.html
The Kuiper Belt and Olbers Paradox
Scott J. Kenyon1 and Rogier A. Windhorst2
1 Smithsonian Astrophysical Observatory, 60 Garden Street,
Cambridge, MA 02138, USA
2 Dept of Physics & Astronomy, Arizona State University, Box 871504,
Tempe , AZ 85287-1504, USA
Submitted to: Astrophysical Journal Letters
For preprints, contact skenyon@cfa.harvard.edu
or on the web at http://xxx.arXiv.org/abs/astro-ph/0009162
The Inclination Distribution of the Kuiper Belt
Michael E. Brown1
1 Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA
Submitted to: The Astronomical Journal
Preprints on the web at http://www.gps.caltech.edu/~mbrown/papers
Cometary Collisional Evolution During Ejection to the Oort Cloud
S.A. Stern1 and P.R. Weissman2
1 Southwest Research Institute, Suite 426, 1050 Walnut Street, Boulder, CO 80302, USA
2 Jet Propulsion Laboratory, California Institute of Technology,
Pasadena, CA 91109, USA
Submitted to: Nature
For preprints, contact alan@boulder.swri.edu
The Activity of Comet 29P/Schwassmann-Wachmann 1 Monitored Through its CO J=2-1 Radio Line
M.C. Festou1, M. Gunnarsson2, H. Rickman2, A. Winnberg3, and G. Tancredi4
1 Southwest Research Institute, Dept. of Space Studies, Boulder, USA
2 Astronomiska Observatoriet, Uppsala, Sweden
3 Onsala Rymdobservatorium, Onsala, Sweden
4 Dpto. Astronomia, Fac. Ciencias, Igua 4225, Montevideo, Uruguay
To appear in: Icarus
For preprints, contact festou@ast.obs-mip.fr
or on the web at http://webast.ast.obs-mip.fr/people/festou/papers.html
The Discovery of Argon in Comet Hale-Bopp
S.A. Stern1, D.C. Slater2, M.C. Festou1,3, J.Wm. Parker1,
R. Gladstone2, M.F. A'Hearn4, and E. Wilkinson5
1 Southwest Research Institute, Boulder, CO 80302, USA
2 Southwest Research Institute, San Antonio TX 78256, USA
3 Observatoire Midi-Pyrenées, Toulouse, France
4 Department of Astronomy, University of Maryland, College Park, MD 20742, USA
5 CASA, University of Colorado, Boulder, CO 80302, USA
To appear in: The Astrophysical Journal Letters
For preprints, contact alan@boulder.swri.edu
or on the web at http://www.boulder.swri.edu/~joel/papers.html
[The DPS meeting will begin soon after this issue of the Newsletter is sent
out, so below I include the Kuiper Belt related papers that I found in the
program (http://www.aas.org/dps2000/
). Since the IAU meeting has
already passed, I will include the titles only of those contributions that were
submitted to the Newsletter, though the full program and Kuiper belt related
talks can be found at: http://www.iau.org/ffscp.htm#JD4
-- Ed.]
Regarding the Criteria for Planethood and Proposed Classification Schemes
S.A Stern1 and H.F. Levison1
1 Southwest Research Institute, Suite 426, 1050 Walnut Street, Boulder, CO 80302, USA
To appear in: IAU Proceedings
For preprints, contact alan@boulder.swri.edu
or on the web at http://www.boulder.swri.edu/~alan/papers.html
Resonant Gaps in the Scattered Cometary Population of the Trans-Neptunian Region
Tanya Taidakova1, Leonid M. Ozernoy2, and Nick N. Gorkavyi3
1 Computational Consulting Service, MD, simeiz@aol.com
2 5C3, School of Computational Sciences and Department of Physics
& Astronomy, George Mason U., Fairfax, VA 22030-4444;
ozernoy@science.gmu.edu
3 NASA/GSFC, Greenbelt, MD 20771;
gorkavyi@stars.gsfc.nasa.gov
To appear in: IAU Proceedings
DPS Meeting
http://www.aas.org/publications/baas/v32n3/dps2000/S190.htm
http://www.aas.org/publications/baas/v32n3/dps2000/423.htm
http://www.aas.org/publications/baas/v32n3/dps2000/69.htm
http://www.aas.org/publications/baas/v32n3/dps2000/419.htm
http://www.aas.org/publications/baas/v32n3/dps2000/152.htm
http://www.aas.org/publications/baas/v32n3/dps2000/S200.htm
http://www.aas.org/publications/baas/v32n3/dps2000/18.htm
http://www.aas.org/publications/baas/v32n3/dps2000/28.htm
http://www.aas.org/publications/baas/v32n3/dps2000/62.htm
http://www.aas.org/publications/baas/v32n3/dps2000/469.htm
http://www.aas.org/publications/baas/v32n3/dps2000/530.htm
http://www.aas.org/publications/baas/v32n3/dps2000/425.htm
http://www.aas.org/publications/baas/v32n3/dps2000/272.htm
http://www.aas.org/publications/baas/v32n3/dps2000/280.htm
http://www.aas.org/publications/baas/v32n3/dps2000/6.htm
http://www.aas.org/publications/baas/v32n3/dps2000/7.htm
http://www.aas.org/publications/baas/v32n3/dps2000/600.htm
http://www.aas.org/publications/baas/v32n3/dps2000/368.htm
http://www.aas.org/publications/baas/v32n3/dps2000/S210.htm
http://www.aas.org/publications/baas/v32n3/dps2000/604.htm
http://www.aas.org/publications/baas/v32n3/dps2000/263.htm
http://www.aas.org/publications/baas/v32n3/dps2000/160.htm
http://www.aas.org/publications/baas/v32n3/dps2000/266.htm
http://www.aas.org/publications/baas/v32n3/dps2000/43.htm
http://www.aas.org/publications/baas/v32n3/dps2000/57.htm
http://www.aas.org/publications/baas/v32n3/dps2000/51.htm
http://www.aas.org/publications/baas/v32n3/dps2000/386.htm
http://www.aas.org/publications/baas/v32n3/dps2000/265.htm
http://www.aas.org/publications/baas/v32n3/dps2000/56.htm
http://www.aas.org/publications/baas/v32n3/dps2000/109.htm
http://www.aas.org/publications/baas/v32n3/dps2000/S450.htm
http://www.aas.org/publications/baas/v32n3/dps2000/210.htm
http://www.aas.org/publications/baas/v32n3/dps2000/349.htm
http://www.aas.org/publications/baas/v32n3/dps2000/259.htm
http://www.aas.org/publications/baas/v32n3/dps2000/118.htm
http://www.aas.org/publications/baas/v32n3/dps2000/560.htm
http://www.aas.org/publications/baas/v32n3/dps2000/550.htm
http://www.aas.org/publications/baas/v32n3/dps2000/S460.htm
http://www.aas.org/publications/baas/v32n3/dps2000/588.htm
http://www.aas.org/publications/baas/v32n3/dps2000/567.htm
http://www.aas.org/publications/baas/v32n3/dps2000/414.htm
We accept submissions for the following sections:
Distant EKOs is not a refereed publication, but is a tool for furthering communication among people interested in Kuiper belt research. Publication or listing of an article in the Newsletter or the web page does not constitute an endorsement of the article's results or imply validity of its contents. When referencing an article, please reference the original source; Distant EKOs is not a substitute for peer-reviewed journals.