I am interested in the rules of stable isotopic
fractionation during various physical, chemical, and biological
processes. These rules can be used to solve problems in natural
sciences. Most of my current research topics are of geological
interests.
Hyperarid Environments
There are
significant accumulations of atmospheric depositions (mainly sulfate
and nitrate) in these
settings. Multiple stable isotopic analyses (O, S, and N) provide
powerful tools in identifying the sources, transport pattern, and
evolution of these salt deposits.
Antarctic
Dry Valleys (supported by NSF
OPP-0125842)
It
has two extremes, dry and cold, combined. It's surface can be as
old
as ~18 million years.
http://www.sciam.com/news/092800/1.html
(Dry Valleys in Scientific American)
http://www.heise.de/tp/deutsch/special/raum/8853/1.html
(Dry Valleys news in German)
The Central Namib Desert
It is dry but not that cold, and it's flat and low in elevation.
A paper on pattern of O-17 anomaly of the desert soils has been
published in EPSL.

http://news.bbc.co.uk/hi/english/sci/tech/newsid_830000/830514.stm
(BBC news on fossil air)
http://www.spacedaily.com/news/earth-00d.html
(O-17 anomaly)
The Atacama Desert
It is extremely dry and not that cold, but
has distinct topographic features.
Mars
Its surface is extremely cold and dry. Hope we’ll have
samples soon.
A Series of Late Oligocene and Miocene (30 -7 Ma)
Volcanic Eruptions
--(Supported by NSF
EAR-0408986)
Mysterious oxygen isotopic signature (O-17 anomaly) are found in
many layers of volcanic ash beds.
Our recent paper on this topic has been listed in AGU Journal
Highlights.

Natural
perchlorate
We have identified a unique
oxygen-17 anomaly among perchlorate of atmospheric origin.
An article
featuring this discovery in "AC Detector" in Analuytical Chemistry, Nov. 1, 2004.
Early
Earth
James Farquhar and his colleagues in
2000
have discovered strange sulfur
isotopic compositions (S-33 anomaly) in Archean sediments (or
metasediments). It has since brought a great new excitement in
Precambrian research.
http://www.spaceflightnow.com/news/n0008/04o2life/
(S-33 anomaly)
Precambrian-Cambrian
Transition
Neoproterozoic
glaciations, rising of metazoa, shelly fossils, and extreme
fluctuations in geochemical and isotopic signatures.
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