Damage sustained by an ischaemic kidney is reduced by cooling the organ. For this reason kidneys are rapidly cooled during the retrieval operation and preserved at low temperature before implantation. When the kidney is removed from cold storage for implantation into the recipient it gradually rewarms (second warm ischaemic time) and a prolonged second warm ischaemic time has been shown to be a cause of acute tubular necrosis following transplantation. The temperature rise in a kidney during implantation has been poorly investigated and little work to minimize that rise has been carried out. This study investigates, in an animal model, the changes that occur in the core temperature of kidneys during the second warm ischaemic time. A jacket has been designed which greatly reduces the rate of kidney rewarming during simulated operative conditions. Kidneys unprotected by the test system showed a rapid rise in temperature from a mean of 1 degrees C to a mean of 20 degrees C after 45 min, compared with those kidneys placed in the protective jacket in which the temperature rose to a mean of only 8 degrees C in the same time. The jacket is not bulky and is simple to use. Maintaining a low kidney core temperature during the second warm ischaemic time will reduce injury to the kidney and should be part of routine clinical practice.
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http://dx.doi.org/10.1002/bjs.1800761004 | DOI Listing |
PLoS One
January 2025
Department of Physiology and Biochemistry, Faculty of Physical Education and Sport Science, Wroclaw University of Health and Sport Sciences, Wroclaw, Poland.
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View Article and Find Full Text PDFSci Rep
January 2025
School of Earth Sciences, China University of Geosciences, Wuhan, 430074, Hubei, China.
Soil magnetic records in Quaternary red earth (QRE) deposits contain a valuable record of paleoclimate information, providing insights into controls on Earth's climate system in the past and potentially helping to predict its response to perturbations in the future. Here, analysis of the environmental magnetism and mineralogy of the Xuancheng QRE (Anhui Province, South China) shows that magnetic variation was strongly linked to production of authigenic ferrimagnetic minerals such as maghemite. Fine-grained maghemite formed during the weathering-related transformation of iron-bearing illite to vermiculite, generating aggregates of vermiculite or mixed-layer illite-vermiculite.
View Article and Find Full Text PDFPlants (Basel)
January 2025
Institute of Crop Science, Ministry of Agriculture and Rural Affairs Key Laboratory of Spectroscopy Sensing, Zhejiang University, Hangzhou 310058, China.
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View Article and Find Full Text PDFPhytopathology
January 2025
Centre for Horticultural Science, Queensland Alliance for Agriculture and Food Innovation, The University of Queensland, Brisbane, Queensland, Australia;
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View Article and Find Full Text PDFEnviron Sci Pollut Res Int
January 2025
Earth Sciences, Engineering Faculty, Autonomous University of San Luis Potosi, Av. Manuel Nava 8, San Luis Potosí, SLP, Mexico.
Ecosystems such as wetlands have karst groundwater as their primary source of preserving their services and functions. Karst systems are complex hydrogeological systems that are difficult to study because of their complicated functioning mechanism, which requires an interdisciplinary effort based on hydrodynamic assessment and characterization of the hydrogeology of the system. The study area is the Ramsar wetland Ciénaga de Tamasopo (Mexico), which is dependent on the discharge of karst groundwater that is affected by water extraction of extensive sugarcane agriculture and is also the main water source for the rural towns.
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