47 research outputs found
Shape reconstruction from gradient data
We present a novel method for reconstructing the shape of an object from
measured gradient data. A certain class of optical sensors does not measure the
shape of an object, but its local slope. These sensors display several
advantages, including high information efficiency, sensitivity, and robustness.
For many applications, however, it is necessary to acquire the shape, which
must be calculated from the slopes by numerical integration. Existing
integration techniques show drawbacks that render them unusable in many cases.
Our method is based on approximation employing radial basis functions. It can
be applied to irregularly sampled, noisy, and incomplete data, and it
reconstructs surfaces both locally and globally with high accuracy.Comment: 16 pages, 5 figures, zip-file, submitted to Applied Optic
Microdeflectometry - a novel tool to acquire 3D microtopography with nanometer height resolution
We introduce "microdeflectometry", a novel technique for measuring the
microtopography of specular surfaces. The primary data is the local slope of
the surface under test. Measuring the slope instead of the height implies high
information efficiency and extreme sensitivity to local shape irregularities.
The lateral resolution can be better than one micron whereas the resulting
height resolution is in the range of one nanometer. Microdeflectometry can be
supplemented by methods to expand the depth of field, with the potential to
provide quantitative 3D imaging with SEM-like features.Comment: 3 pages, 11 figures, latex, zip-file, accepted for publication at
Optics Letter
“A very orderly retreat”: Democratic transition in East Germany, 1989-90
East Germany's 1989-90 democratisation is among the best known of East European transitions, but does not lend itself to comparative analysis, due to the singular way in which political reform and democratic consolidation were subsumed by Germany's unification process. Yet aspects of East Germany's democratisation have proved amenable to comparative approaches. This article reviews the comparative literature that refers to East Germany, and finds a schism between those who designate East Germany's transition “regime collapse” and others who contend that it exemplifies “transition through extrication”. It inquires into the merits of each position and finds in favour of the latter. Drawing on primary and secondary literature, as well as archival and interview sources, it portrays a communist elite that was, to a large extent, prepared to adapt to changing circumstances and capable of learning from “reference states” such as Poland. Although East Germany was the Soviet state in which the positions of existing elites were most threatened by democratic transition, here too a surprising number succeeded in maintaining their position while filing across the bridge to market society. A concluding section outlines the alchemy through which their bureaucratic power was transmuted into property and influence in the “new Germany”
ECCD-induced sawtooth crashes at W7-X
The optimised superconducting stellarator W7-X generates its rotational transform by means of
external coils, therefore no toroidal current is necessary for plasma confinement. Electron
cyclotron current drive experiments were conducted for strikeline control and safe divertor
operation. During current drive experiments periodic and repetitive crashes of the central
electron temperature, similar to sawtooth crashes in tokamaks, were detected. Measurements
from soft x-ray tomography and electron cyclotron emission show that the crashes are preceded
by weak oscillating precursors and a displacement of the plasma core, consistent with a
(m, n)=(1, 1) mode. The displacement occurs within 100μs, followed by expulsion and
redistribution of the core into the external part of the plasma. Two types of crashes, with
different frequencies and amplitudes are detected in the experimental program. For these
non-stationary parameters a strong dependence on the toroidal current is found. A 1-D heuristic
model for current diffusion is proposed as a first step to explain the characteristic crash time.
Initial results show that the modelled current diffusion timescale is consistent with the initial
crash frequency and that the toroidal current rise shifts the position where the instability is
triggered, resulting in larger crash amplitudes
Advanced electron cyclotron heating and current drive experiments on the stellarator Wendelstein 7-X
During the first operational phase (OP 1.1) of Wendelstein 7-X (W7-X) electron cyclotron resonance heating (ECRH) was the exclusive heating method and provided plasma start-up, wall conditioning, heating and current drive. Six gyrotrons were commissioned for OP1.1 and used in parallel for plasma operation with a power of up to 4.3 MW. During standard X2-heating the spatially localized power deposition with high power density allowed controlling the radial profiles of the electron temperature and the rotational transform. Even though W7-X was not fully equipped with first wall tiles and operated with a graphite limiter instead of a divertor, electron densities of n e > 3·1019 m-3 could be achieved at electron temperatures of several keV and ion temperatures above 2 keV. These plasma parameters allowed the first demonstration of a multipath O2-heating scenario, which is envisaged for safe operation near the X-cutoff-density of 1.2·1020 m-3 after full commissioning of the ECRH system in the next operation phase OP1.2
Analysis of hydrogen fueling, recycling, and confinement at Wendelstein 7-X via a single-reservoir particle balance
Fluxes of biogenic components from sediment trap deployment in circumpolar waters of the Drake Passage
Circumpolar surface waters dominate the circulation of the Southern Ocean and sustain one of the ocean's largest standing stocks of biomass thereby producing a significant output of biogenic components, mainly diatoms, to the bottom sediments. Generally transit of biogenic matter from the sea surface to the sea floor affects nutrient regeneration fuels benthic life and transfers signals to the sediment record1–5. Reliable quantification of the relationship between biological production, fractionation of skeletal and tissue components and bottom sediment accumulation depends on direct vertical flux measurements from sediment trap deployments6–9, which have proved to be most scientifically productive10–13. We now present data on vertical mass fluxes from the Southern Ocean and evidence for strong biogeochemical fractionation between organic carbon-, nitrogen- and phosphorus-containing compounds, siliceous and calcareous skeletal remains, and refractory aluminosilicates
