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Institute
The "Large Hadron Collider" (LHC) is currently the most powerful particle accelerator. It provides particle collisions at a center of mass energy in the Tera-electronvolt range, which had never been reached in a laboratory before. Thereby a new era in high energy particle physics has began. Now it is possible to test one of the most precise theories in physics, the Standard Model of particle physics, at these high energies. The purpose is particularly served by four large experiments installed at the LHC, namely "A Toroidal LHC ApparatuS" (ATLAS), the "Compact-Muon-Solenoid" (CMS), the "Large Hadron Collider beauty" (LHCb) and "A Large Ion Collider Experiment" (ALICE). Besides exploring the high energy behavior of the well-established portions of the Standard Model, one of the main objectives is to find the Higgs boson included in the model, but not discovered by any preceding effort. It is of tremendous importance since fermions and heavy electroweak gauge bosons acquire mass because of this boson. Although the success of the Standard Model in describing nature is already undisputed, there are some flaws due to observations inexplicable within this theory only. Therefore searches for physics beyond the Standard Model are promoted at the LHC experiments as well. In order to achieve the defined goals, crucial aspects are firstly precise measurements, to verify Standard Model predictions in detail, and secondly an evaluation of as much information as accessible by the detectors, to recognize new phenomena as soon as possible for subsequent optimizations. Both challenges are only possible with a superior understanding of the detectors. An inevitable contribution to attain this knowledge is a realistic simulation, partially requiring new implementation techniques to describe the very complex instrumentation. The research presented here is performed under the patronage of the ATLAS collaboration with a special focus on measurements done with muon spectrometer. Thus a first central issue is the performance of the spectrometer in terms of physics objects that are recognized by the device, the compatibility of data and the existing simulation as well as its improvement and finally the extension of the acceptance region. Once the excellent behavior and comprehension of the muon spectrometer is demonstrated, a second part addresses one physics use case of reconstructed muons. The electroweak force is part of the Standard Model and causes the interaction of heavy electroweak gauge bosons with fermions as well as their self-interaction. In proton-proton collisions such gauge bosons are produced. However, they decay immediately into a pair of fermions. In case of the Z boson, which is one of the gauge bosons, oppositely charged fermions of the same generation, including muons, emerge. The various decay modes are determined precisely at particle accelerators other than the LHC. However, the associated production of two Z bosons is measured less exactly at those facilities because of a very low cross section. The corresponding results acquired with the ATLAS experiment exceed all previous measurements in terms of statistics and accuracy. They are reported in this thesis as obtained from the observation of events with four charged leptons. The enhancement of the signal yield based on the extension of the muon spectrometer acceptance is especially emphasized as well as alternative methods to estimate background events. Furthermore, the impact on the probing of couplings of three Z bosons and intersection with the search for the Standard Model Higgs boson are pointed out.
Motivation
The BioTIME database contains raw data on species identities and abundances in ecological assemblages through time. These data enable users to calculate temporal trends in biodiversity within and amongst assemblages using a broad range of metrics. BioTIME is being developed as a community-led open-source database of biodiversity time series. Our goal is to accelerate and facilitate quantitative analysis of temporal patterns of biodiversity in the Anthropocene.
Main types of variables included
The database contains 8,777,413 species abundance records, from assemblages consistently sampled for a minimum of 2 years, which need not necessarily be consecutive. In addition, the database contains metadata relating to sampling methodology and contextual information about each record.
Spatial location and grain
BioTIME is a global database of 547,161 unique sampling locations spanning the marine, freshwater and terrestrial realms. Grain size varies across datasets from 0.0000000158 km2 (158 cm2) to 100 km2 (1,000,000,000,000 cm2).
Time period and grain
BioTIME records span from 1874 to 2016. The minimal temporal grain across all datasets in BioTIME is a year.
Major taxa and level of measurement
BioTIME includes data from 44,440 species across the plant and animal kingdoms, ranging from plants, plankton and terrestrial invertebrates to small and large vertebrates.
Software format
.csv and .SQL.