Multiple-reaction monitoring (MRM) transitions, declustering potentials (DP), collision energies (CE) and collision cell exit potential (CXP) for the 8 steroids and deuterated internal standards.

CERN-LHC. The ALICE collaboration at the CERN LHC reports novel measurements of jet substructure in pp collisions at $\sqrts~= 7$ TeV and central Pb--Pb collisions at $\sqrtsNN~= 2.76$~TeV. Jet substructure of track-based jets is explored via iterative declustering and grooming techniques. We present the measurement of the momentum sharing of two-prong substructure exposed via grooming, the \zg, and its dependence on the opening angle, in both pp and Pb--Pb collisions. We also present the first measurement of the distribution of the number of branches obtained in the iterative declustering of the jet, which is interpreted as the number of its hard splittings. In Pb--Pb collisions, we observe a suppression of symmetric splittings at large opening angles and an enhancement of splittings at small opening angles relative to pp collisions, with no significant modification of the number of splittings. The results are compared to predictions from various Monte Carlo event generators to test the role of important concepts in the evolution of the jet in the medium such as color coherence.

Test data of two integrated electricity and heat systems

The 2021 National Seismic Hazard Model for Hawaii considers the full catalog and several declustered catalogs in calculating earthquake rates and seismic hazard. Events associated with a caldera collapse are treated differently within the model and were separated from the full catalogs. The catalogs are separated into two time periods, pre- and post-1959. The pre-1959 catalog was declustered using both the Reasenberg and nearest neighbor declustering methods. The post-1959 full catalog was split into summit (volcanic) and non-summit events, and those catalogs being separated into shallow (h ≤ 20 km) and deep (h > 20 km). These catalogs were declustered using the Reasenberg and nearest neighbor methods. The declustered, shallow events were further separated into events near the island of Hawai`I (south) and events associated with the islands to the northwest (north). All of these catgalogs are included here and are described in more detail in the paper by Petersen and others (2021). The coordinates that define the summit, caldera, and north/south seismicity zones are also included here.

Supplementary Material 2.

A research model (RM) was prepared, which incorporates declustered rate grids that are scaled to account for the total number of earthquakes in the full catalog (with no declustering) using factors shown in Table 1 of Petersen et al. (2021), based on Marzocchi and Taroni (2014). A comparison of the 2021 research model and the 2021 National Seismic Hazard Model for Hawaii was performed by creating difference and ratio maps for a uniform-hazard with a 2% probability of excedance in 50 years for spectral accelerations at 0.2 and 1.0 second periods. The data are for a reference site condition of Vs30 equal to 760 m/s. The maps and gridded data used to make the maps are availble here for download.

Ratio of fully corrected $n_{\rm SD}$ distribution in pp collisions for $40 \leq p_{\rm T,jet}^{\rm ch} < 60$ GeV/{\it c}...

2a Charge-deconvoluted mass spectrum of apolipoprotein CIII from serum 2b Charge-deconvoluted mass spectrum of apolipoprotein CIII from dried blood spot

Method SCIEX API4500 Triple-Quad, gas temperature 120°C, curtain gas 10 psi, ion source gas 16 psi, IonSpray voltage 5.5 kV, declustering potential 100 V, and entrance potential 10 V

This submission includes a fault map of the Oregon Cascades and backarc, a probability map of heat flow, and a fault density probability layer. More extensive metadata can be found within each zip file.

For information about "Oregon Faults," contact John David Trimble, Oregon State University. trimbljo@onid.oregonstate.edu This is a probability map of heat flow in the Cascades in Oregon where a threshold of 80 wM/m squared was used. Probability was calculated using simple kriging with declustering. The data used for this statistical surface were down-loaded from the Southern Methodist University Geothermal Laboratory.

Ratio of Detector-level Pb--Pb distributions of $n_{\rm SD}$ for $R=0.4$ jets in the range $80 \leq p_{\rm T,jet}^{\rm ch} <...

DP, declustering potential; EP, entrance potential; CE, collision energy; CXP, collision cell exit potential.

Q1  =  1st Quadrupole setting; Q3  =  3rd Quadrupole setting; DP  =  Declustering Potential; CE  =  Collision Energy; CXP  =  Collision Cell Exit Potential; DWELL  =  Dwelling time; INT STD  =  Internal Standard.Optimized MRM parameters.