Abstract
The observation of anomalous charge collection in a P-type Point Contact (PPC) High Purity Germanium (HPGe) detector is reported. By studying preamplifier charge signals from the detector, these anomalous events are shown to be consistent with charge carrier drift along the surface of the detector, prior to collection at the contact. It is believed that these events arise from the formation of a surface channel in the detector. By coupling analysis of these experimental signals with field calculations, an estimate of the radial drift velocity of holes at the surface has been made. This value is found to be around 40 times slower than the accepted value for saturated hole drift in the bulk, and is in good agreement with that calculated using a newly developed technique for modelling carrier transport.
| Original language | English |
|---|---|
| Pages (from-to) | 48-55 |
| Number of pages | 8 |
| Journal | Nuclear Instruments and Methods in Physics Research, Section A: Accelerators, Spectrometers, Detectors and Associated Equipment |
| Volume | 680 |
| DOIs | |
| State | Published - Jul 11 2012 |
Funding
Research sponsored by the U.S. Department of Energy Office of Science, Office of Nuclear Physics . Also supported by U.S. Department of Energy Office of Science , Office of Nuclear Physics Grant DE-FG02-07ER84758 . The Joint Institute for Heavy Ion Research has as member institutions: the University of Tennessee, Vanderbilt University, and the Oak Ridge National Laboratory; it is supported by the members and by the U.S. Department of Energy .
Keywords
- HPGe detector
- Mobility
- Modelling
- Surface channel