148 research outputs found

    Power formulas for mixed effects models with random slope and intercept comparing rate of change across groups

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    We have previously derived power calculation formulas for cohort studies and clinical trials using the longitudinal mixed effects model with random slopes and intercepts to compare rate of change across groups [Ard & Edland, Power calculations for clinical trials in Alzheimer’s disease. J Alzheim Dis 2011;21:369–77]. We here generalize these power formulas to accommodate 1) missing data due to study subject attrition common to longitudinal studies, 2) unequal sample size across groups, and 3) unequal variance parameters across groups. We demonstrate how these formulas can be used to power a future study even when the design of available pilot study data (i.e., number and interval between longitudinal observations) does not match the design of the planned future study. We demonstrate how differences in variance parameters across groups, typically overlooked in power calculations, can have a dramatic effect on statistical power. This is especially relevant to clinical trials, where changes over time in the treatment arm reflect background variability in progression observed in the placebo control arm plus variability in response to treatment, meaning that power calculations based only on the placebo arm covariance structure may be anticonservative. These more general power formulas are a useful resource for understanding the relative influence of these multiple factors on the efficiency of cohort studies and clinical trials, and for designing future trials under the random slopes and intercepts model

    The Chronic Progressive Repeated Measures (CPRM) Model for Clinical Trials Comparing Change Over Time in Quantitative Trait Outcomes

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    Repeated measures analysis is a common analysis plan for clinical trials comparing change over time in quantitative trait outcomes in treatment versus control. Mixed model for repeated measures (MMRM) assuming an unstructured covariance of repeated measures is the default statistical analysis plan, with alternative covariance structures specified in the event that the MMRM model with unstructured covariance does not converge. We here describe a parsimonious covariance structure for repeated measures analysis that is specifically appropriate for longitudinal repeated measures of chronic progressive conditions. This model has the parsimonious features of the mixed effects model with random slopes and intercepts, but without restricting the repeated measure means to be linear with time. We demonstrate with data from completed trials that this pattern of longitudinal trajectories spreading apart over time is typical of Alzheimer’s disease. We further demonstrate that alternative covariance structures typically specified in statistical analysis plans using MMRM perform poorly for chronic progressive conditions, with the compound symmetry model being anticonservative, and the autoregressive model being poorly powered. Finally, we derive power calculation formulas for the chronic progressive repeated measures model that have the advantage of being independent of the design of the pilot studies informing the power calculations. When data follow the pattern of a chronic progressive condition. These power formulas are also appropriate for sizing clinical trials using MMRM analysis with unstructured covariance of repeated measures

    Platinum Group Element Mineralization in the Reinfjord Ultramafic Complex - A geochemical and petrological study of the PGE-enriched parts of the RF-4 drill core

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    The Reinfjord Ultramafic Complex (RUC), a part of the Seiland Igneous Province (SIP), is located in Nord-Troms, Norway. The RUC constitutes parts of deep seated magmatic conduit system that comprises a low tenor PGE-reef. In the RF-4 drill core, the reef is located at a depth of approximately 62 m, where the Pd+Pt concentration reaches around 0.8 ppm. This thesis places its emphasis on investigating the PGE mineralization of the RF-4 drill core, in order to obtain knowledge regarding the formation mechanisms of the reef. The thesis also compares the results with the mineralization found in the RF-1 drill core. Chemical data was provided by ICP spectrometry, SEM and EPMA, while preliminary investigations was done by optical microscopy. The PGE host rock in RF-4 is a dunite, containing mostly olivine, with minor clinopyroxene and orthopyroxene. Interstitial carbonates and amphibole is also present. The RF-4 drill core revealed a wide variety of PGM's, where bismuthotellurides, arsenides and sulfurarsenides are the most common phases. Other phases comprise antimonides and PGE alloys. The PGM's are often BMS associated, where both pentlandite and pyrrhotite are common hosts. The presence of the PGE-arsenides-and sulfurarsenides, set the mineralization in RF-4 apart from that of RF-1. Possible scenarios explaining the differences in PGM assemblage are localized gain of As from surrounding rocks, removal by hydrothermal fluids or vertical displacement of As-rich zones due to tectonics. The author suggest that the PGM's formed from sulfide fractionation, and the concentration process is thus magmatic. Further, the author propose the possibility of PGM's exsolving from an iss, due the PGM's often showing an affinity to Cu-rich pyrrhotite. PGM's can also be found associated with serpentine, sometimes showing remainders of BMS, indicating high degrees of serpentinization. Serpentinization is also responsible for the breakdown of chalcopyrite, leading to the formation of native Cu. Stability field calculations with constant bulk composition a.k.a a pesudosection was done for a mineral assemblage comprising amphibole, orthopyroxene, olivine and magnesite, which represents a secondary volatile phase. The model propose that re-mobilization of PGE and Au could happen at high P (>6>6 bar) and mid-to-high T (>800>800 K) conditions. Pd would be more soluble in the fluid compared to Pt, and the Pd-cluster in RF-1 could thus be the result of such processes

    The MAX Statistic is Less Powerful for Genome Wide Association Studies Under Most Alternative Hypotheses

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    Genotypic association studies are prone to inflated type I error rates if multiple hypothesis testing is performed, e.g., sequentially testing for recessive, multiplicative, and dominant risk. Alternatives to multiple hypothesis testing include the model independent genotypic c2 test, the efficiency robust MAX statistic, which corrects for multiple comparisons but with some loss of power, or a single Armitage test for multiplicative trend, which has optimal power when the multiplicative model holds but with some loss of power when dominant or recessive models underlie the genetic association. We used Monte Carlo simulations to describe the relative performance of these three approaches under a range of scenarios. All three approaches maintained their nominal type I error rates. The genotypic c2 and MAX statistics were more powerful when testing a strictly recessive genetic effect or when testing a dominant effect when the allele frequency was high. The Armitage test for multiplicative trend was most powerful for the broad range of scenarios where heterozygote risk is intermediate between recessive and dominant risk. Moreover, all tests had limited power to detect recessive genetic risk unless the sample size was large, and conversely all tests were relatively well powered to detect dominant risk. Taken together, these results suggest the general utility of the multiplicative trend test when the underlying genetic model is unknown
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