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Impact of atherosclerotic plaque composition on the development of acute coronary syndrome
Kopřiva, Karel ; Kovárník, Tomáš (advisor) ; Kaňovský, Jan (referee) ; Toušek, Petr (referee)
Thin fibrous cap atheroma with a high lipid content is the most common morphological substrate for acute coronary syndrome. Lipid content can be reliably determined by near infrared spectroscopy (NIRS) imaging. Optical coherence tomography (OCT) is a commonly available morphological imaging method in the guidance of coronary interventions. In our study, we examined a single coronary lesion in patients with acute coronary syndrome using both OCT and NIRS. Based on OCT, we performed a detailed morphological analysis using semi-automated software. Using NIRS, we determined the lipid content of each lesion. In the first part of the study, we used noninvasive CT coronary angiography to detect the progression of atherosclerotic plaques between the first and second year after the initial examination and attempted to demonstrate that morphological characteristics and lipid content of plaques were risk factors for plaque progression. In the second part of the study, we assessed the ability of detailed morphological analysis based on OCT examination to identify the lipid content of plaques using NIRS as a reference method. We observed no significant linear correlation when assessing the relationship between morphological parameters and plaque volume progression. In the analysis of plaque lipid content,...
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Key factors in soil organic matter accumulation
Vindušková, Olga ; Frouz, Jan (advisor) ; Borůvka, Luboš (referee) ; Šarapatka, Bořivoj (referee)
Soil organic matter (SOM) is highly important for soil quality and the global carbon cycle. SOM content is influenced by a complex interplay of many different factors such as time, climate, parent material, vegetation, and others. The effect of time is often studied using the chronosequence approach using a set of study sites differing in age but comparable in other soil-forming factors. The effect of other factors can be studied by comparing two or more chronosequences. An important assumption of these approaches is that the SOM quantification methods produce comparable results both among sites of each sequence and among different sequences. In this thesis, I explored the key factors in SOM accumulation and dealt with SOM quantification methods. I studied SOM accumulation in two model situations - in post-mining sites after open-cast coal and oil shale mining and in landslides in the Western Carpathians. The results of this thesis are summarized in one book chapter accepted for publication and four papers, out of which three have been published and one is prepared for publication in an international journal with impact factor. The key factor affecting the rate of SOM accumulation after a major disturbance is time. The accumulation rates found in the first 40 to 100 years in both post-mining sites...
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Key factors in soil organic matter accumulation
Vindušková, Olga
Soil organic matter (SOM) is highly important for soil quality and the global carbon cycle. SOM content is influenced by a complex interplay of many different factors such as time, climate, parent material, vegetation, and others. The effect of time is often studied using the chronosequence approach using a set of study sites differing in age but comparable in other soil-forming factors. The effect of other factors can be studied by comparing two or more chronosequences. An important assumption of these approaches is that the SOM quantification methods produce comparable results both among sites of each sequence and among different sequences. In this thesis, I explored the key factors in SOM accumulation and dealt with SOM quantification methods. I studied SOM accumulation in two model situations - in post-mining sites after open-cast coal and oil shale mining and in landslides in the Western Carpathians. The results of this thesis are summarized in one book chapter accepted for publication and four papers, out of which three have been published and one is prepared for publication in an international journal with impact factor. The key factor affecting the rate of SOM accumulation after a major disturbance is time. The accumulation rates found in the first 40 to 100 years in both post-mining sites...
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Key factors in soil organic matter accumulation
Vindušková, Olga
Soil organic matter (SOM) is highly important for soil quality and the global carbon cycle. SOM content is influenced by a complex interplay of many different factors such as time, climate, parent material, vegetation, and others. The effect of time is often studied using the chronosequence approach using a set of study sites differing in age but comparable in other soil-forming factors. The effect of other factors can be studied by comparing two or more chronosequences. An important assumption of these approaches is that the SOM quantification methods produce comparable results both among sites of each sequence and among different sequences. In this thesis, I explored the key factors in SOM accumulation and dealt with SOM quantification methods. I studied SOM accumulation in two model situations - in post-mining sites after open-cast coal and oil shale mining and in landslides in the Western Carpathians. The results of this thesis are summarized in one book chapter accepted for publication and four papers, out of which three have been published and one is prepared for publication in an international journal with impact factor. The key factor affecting the rate of SOM accumulation after a major disturbance is time. The accumulation rates found in the first 40 to 100 years in both post-mining sites...
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Key factors in soil organic matter accumulation
Vindušková, Olga ; Frouz, Jan (advisor) ; Borůvka, Luboš (referee) ; Šarapatka, Bořivoj (referee)
Soil organic matter (SOM) is highly important for soil quality and the global carbon cycle. SOM content is influenced by a complex interplay of many different factors such as time, climate, parent material, vegetation, and others. The effect of time is often studied using the chronosequence approach using a set of study sites differing in age but comparable in other soil-forming factors. The effect of other factors can be studied by comparing two or more chronosequences. An important assumption of these approaches is that the SOM quantification methods produce comparable results both among sites of each sequence and among different sequences. In this thesis, I explored the key factors in SOM accumulation and dealt with SOM quantification methods. I studied SOM accumulation in two model situations - in post-mining sites after open-cast coal and oil shale mining and in landslides in the Western Carpathians. The results of this thesis are summarized in one book chapter accepted for publication and four papers, out of which three have been published and one is prepared for publication in an international journal with impact factor. The key factor affecting the rate of SOM accumulation after a major disturbance is time. The accumulation rates found in the first 40 to 100 years in both post-mining sites...
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The Efficient Application of Near Infrared Spectroscopy with Fourier Transformation for Prediction of Wheat Technological Parameters
Dvořáček, Václav ; Prohasková, Anna ; Štočková, Lenka
This method brings to the users basic information about principles and features of NIR spectroscopy as well as more detailed view of the state-of-the-art capabilities of NIR spectroscopy in wheat quality prediction. The agriculture professionals will use supportive information about possible utilization of the method including practical tips for proper NIR spectrometer selection. For both, the current and prospective users, the method provides practical guidance to device handling, management of calibration sets and calibration models development. The objective evaluation of the 21 predictive models based on FT-NIR measurement, covering the results of 14 reference analytical methods aimed at wheat quality. Furthermore, it offers information useful directly in breeding programs, mill and bakery production and also in agriculture sector, government control and at universities.
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