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Geoverse

About me

I am an experimental geologist and beamline manager at DESY, Hamburg. My beamline is an extreme conditions beamline hosting a Large Volume Press for in situ studies on materials at high pressures and temperatures using synchrotron X-rays.

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My first bushwalk!!

Fun Posted on 2007-03-25 21:47

On Saturday, 25 March 2007, at 8:30
am we set off with 3 cars packed with people for a 100 km drive to Deua National
Park to see the ‘big hole’ and the ‘marble arch’. The drive took a fair while and on our way we briefly stopped in
Captains Flat because one of us, Cheryl, was required to vote in the
NSW state for that days state elections. We had a good laugh when we set off
again and Cheryl’s car would not start so her passengers had to push the car a
fair bit until the engine came alive again. Not much further on Robert, with
whom I sat in the lead car, suddenly noticed a ‘walking rock’ in the bend of
the road. As he observed correctly, however, it was in fact a turtle larger
than the size of your hand! The others of the group soon joined in to watch it
and some took a couple of pictures of it. It was then safely put back on the
ground away from the road.

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At last we arrived at Deua National
Park and started a promising bushwalk to see some
of nature’s incredible phenomena. It didn’t take long before we hit our first
obstacle, the Shaolhaven
River. Most people
managed to get across without getting wet, despite the rocks being very
slippery. For those with sneakers however, many opted to take their shoes off
and wade through the water.

From thereon it was a lovely and casual walk to the first
feature of the trip, the big hole. On our way we also spotted some wallabies
and some joeys.

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The big hole is a morphological
feature properly known as a sink hole. It is over 100 metres deep. Before its
existence, there must have been a large cave underneath the surface that formed
in a thick limestone layer. The limestone was dissolved and carried away by
underground water probably to the Shaolhaven
River. At some point the
cave ceiling composed of siltstone, sandstone and conglomerate rocks must have
collapsed creating the big hole. These sedimentary rocks are about 350 Million
years old, deposited during the Devonian geological era in a coastal
environment.

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We had a short break and then moved on to see the next
highlight of the trip, the Marble Arch. As we walked through the eucalypt
forest massive mounts of dirt were spotted between the trees. These are
presumably abandoned termite mounts. Since we didn’t see the termites
themselves it still leaves me wondering where they went. I had a picture taken
of me on top one of these big mounts.

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We finally arrived at the Marble
Arch, which is a limestone cavern followed by a river gorge. We took out our
torches and headed into the cave. The name Marble arch is rather misleading because there is
no marble to be found, just limestone and limestone breccias.

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The experience was awesome as we made our way through the
cave and the narrow gorge with cleanly polished rocks caused by the action of
the water over a long time. The rocks were extremely slippery too and it didn’t
take long before some of us lost balance and slit into the shallow pools of
water in the gorge. Although getting wet didn’t hurt, the main scare turned out
to be the leeches in the gorge. I managed to get a remarkable shot of one of
the bigger ones. We had lunch in the gorge where we couldn’t go any further
because of a small lake blocking our way. For some great group pictures with us
all having lunch, see the ANUMC website. That is, if they have been uploaded
already. After lunch we made our way back to the cars along the same path we came
and headed back to the SRA and got back by around 5:30 pm.

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All in all, this trip was awesome!!
And I think everyone fully enjoyed themselves as well. Apart from a few wet
feet, nobody took the plunge or got hurt.

I have uploaded the rest of the photos in high res here for your viewing pleasure.



Ultimate frisbee

Fun Posted on 2007-03-23 21:17

Tonight I have been playing ultimate for the first time. I’m surprised how popular the sport is here as professional players don’t actually get paid for playing. I found it good fun though and it’s something new which I like. The frisbee throwing techniques are far more complex than at first sight but I think I did pretty well. The backhand in front of your body is relatively easy but the forehand, like skipping a stone over the pond, requires some more skill and proper handling. The key is to give the disc enough spin so that it flies in a stable trajectory through the air. In two weeks the new season starts so i’ll be joining up with the RSES team (if there are enough players hopefully) and we’ll see how I will fare in the tournaments. In the meanwhile I need to practice, practice and practice 😛

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Tomorrow i’m off for a hike in one of Canberra’s national parks with the mountaineering club. I’ll take some pics as well. The river gorge and the caves are said to be absolutely beautiful!

See ya!



NL vs AUS

Fun Posted on 2007-03-14 08:37

I’m living in another country. But Australia does belong with the developed countries like the USA and countries in western Europe. So what exactly is different apart from the fact that the language spoken is different? Here are some differences i noticed between the Netherlands and Australia:

1) At the supermarket (no matter which one), you are greeted friendly and the cassiere even sorts out your shopping items in plastic bags for you. They also take your keycard (pinpas) and swipe it themselves for you.

2) Pin transactions are similar with a 4 digit pin code but you have the opportunity to select which account you want to use. That’s savings for me.

3) Always when waiting in line, wait until you are called. It’s ‘rude’ to step up when you think the person before you is done and walks away.

4) Cycling on the road is allowed but the roads are not build for cyclists. Cycling on the sidewalk where pedestrians walk is much more common and apparently also allowed. There are some bicycle tracks in Canberra. In Australia people drive on the left side of the road.

5) You must wear a bike helmet by law or face a fine up to $50

6) There are few custards (vla) and yoghurts and a smaller selection of brand cheeses or you have to pay a lot for little.

I’ll add some more things later on.



My work so far

General news Posted on 2007-03-12 18:56

Today I had my first real hands on approach on the experimental work I’ll be doing this year. I cold pressed synthetic iron bearing olivine powder into 5 pellets for sintering in the oven at 1400C overnight so that they become one sample of about 3cm long. On wednesday I will be hot pressing that in other machine to create the final sample which I will be doing preliminary experments on in the wave attenuation machine at pressures up to 200MPa and temps of 1300C.

The last few weeks I have familiarised myself with the various machines i’ll be using. I have witnessed the whole procedure of reassembling the attenuation machine and it’s usage for calibration and proper alignment of the capacitor plates that determine the amount of torsion is produced in the machine by two bottom driver coils. This torsion can be linked to the amount of strain that is produced by shearing the sample in relation to an elastic standard of which the shear modulus and the internal friction 1/Q are known. The tangent of the phase angle that is made with the elastic standard and the sample gives the internal friction of the sample. Likewise the shear modulus can be calculated from two-way wave speeds at different frequencies through the sample (and elastic standard). These values and especially 1/Q, which denotes the wave attenuation in the sample are useful in this experimental project. Ultimately, I will have various samples, pre-deformed with varying dislocation densities (or crystal defects) as sythetic polycrystalline ‘upper mantle material’ and possibly olivine single crystals. These will show different responses to seismic wave attenuation and my goal is to find out to what degree and quantify this relationship and model it for tomographic upper mantle imaging.

This project falls into place in a bigger picture where seismic wave speeds are not only thought to attenuate by dislocation densities but also by:
-Frequency
-Temperature
-Grain size
-Melt fraction
-Chemical composition
-water (<- still needs to be investigated)

The importance of this endeavor lies in the still unresolved phenomenon of the low wavespeed zone in the upper mantle. Whereas previously it has been thought to be caused by widespread melting, it may now seem that dislocations play a large role in dampening the seismic waves instead.

Here are some laboratory pics:

Blog Image Green machine for hot pressing

Blog Image Interface for the attenuation machine

Blog Image Attenuation machine

Blog Image Laboratory

Blog Image My office

Blog Image My workspace (im getting a new desk soonish)

Blog Image Entrance to main building RSES

More photos: here



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