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  • 1
    ISSN: 1436-6215
    Keywords: Homoarginine labeling ; guanidination ; racemization ; D-amino acids ; protein digestibility ; Homoargininmarkierung ; Guanidinierung ; Razemisierung ; D-Aminosäuren ; Proteinverdaulichkeit
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition , Medicine
    Description / Table of Contents: Zusammenfassung Die Homoargininmarkierung (Guanidinierung) dient zur Bestimmung der wahren präcaecalen Proteinverdaulichkeit. Die Proteinguanidinierung erfolgt bei alkalischem pH, was möglicherweise zur Bildung von D-Aminosäuren führt. Da D-Aminosäuren enthaltende Proteinein vitro eine verminderte Verdaulichkeit zeigen, könnte die Homoargininmethode eine falsch niedrige Proteinverdaulichkeit ergeben. Daher wurde das Ausmaß der Proteinrazemisierung während der Guanidinierung von Casein bei pH-Werten zwischen 9 und 11 und bei Temperaturen zwischen 4 und 65°C bestimmt. Optimale Guanidinierungsbedingungen lagen bei 4°C und einem pH-Wert von 10,5–11 oder bei 22°C und pH 10. Höhere pH-Werte bei 22°C führten ebenso wie Temperaturen über 22°C zur Bildung nicht mehr vernachlässigbarer Mengen von D-Aminosäuren.
    Notes: Summary Homoarginine labeling (guanidination) is used to calculate true prececal protein digestibility. A particular worry is that guanidination of proteins at alkaline pH might cause formation of D-amino acids. If D-amino acids show decreased protein digestibility in vivo, as seen in vitro, then the homoarginine method would underestimate protein digestibility. Therefore, the degree of protein racemization was measured during guanidination of casein at pH values between pH 9 and 11 and temperatures between 4o and 65°C. Optimal conditions for the guanidination reaction were 4°C and pH 10.5–11 or 22°C and pH 10. A higher pH value at 22°C or temperatures above 22°C at each pH leads to the formation of appreciable amounts of D-amino acids.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 1994-12-01
    Print ISSN: 0044-264X
    Electronic ISSN: 1435-1293
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition , Medicine
    Published by Springer
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  • 3
    Publication Date: 2024-05-14
    Description: Global coupled climate models are in continuous need for evaluation against independent observations to reveal systematic model deficits and uncertainties. Changes in terrestrial water storage (TWS) as measured by satellite gravimetry missions GRACE and GRACE-FO provide valuable information on wetting and drying trends over the continents. Challenges arising from a comparison of observed and modelled water storage trends are related to gravity observations including non-water related variations such as, for example, glacial isostatic adjustment (GIA). Therefore, correcting secular changes in the Earth's gravity field caused by ongoing GIA is important for the monitoring of long-term changes in terrestrial water from GRACE in particular in former ice-covered regions. By utilizing a new ensemble of 56 individual realizations of GIA signals based on perturbations of mantle viscosities and ice history, we find that many of those alternative GIA corrections change the direction of GRACE-derived water storage trends, for example, from gaining mass into drying conditions, in particular in Eastern Canada. The change in the sign of the TWS trends subsequently impacts the conclusions drawn from using GRACE as observational basis for the evaluation of climate models as it influences the dis-/agreement between observed and modelled wetting/drying trends. A modified GIA correction, a combined GRACE/GRACE-FO data record extending over two decades, and a new generation of climate model experiments leads to substantially larger continental areas where wetting/drying trends currently observed by satellite missions coincide with long-term predictions obtained from climate model experiments.
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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