Abstract

To investigate the mechanisms of cold-induced hypertension, the systolic blood pressure (SBP) and average daily water consumption were measured weekly in 6-month-old male Wistar rats; they were subsequently acclimated to thermoneutrality (26°C for 7 weeks), to cold temperature (6°C for 9 weeks), and then again reacclimated to 26°C for 5 weeks. Circulating plasma volume and whole blood viscosity were measured in subgroups of rats at the end of acclimation to 26°C after 2 days, after 1, 6, and 8 weeks of cold, and after 2 and 5 weeks of rewarming. The control values obtained at the end of thermoneutral period were: SBP = 130.8 ±18.6 mm Hg, plasma volume = 41.9 ± 4.64 mL/kg, whole body viscosity at shear rate of 22.5 per sec = 6.7 ± 0.48 cps, and daily water consumption = 42.25 ± 16.81 mL. After 48 h of cold exposure there was almost a 50% increase in plasma volume that persisted to a lesser degree throughout the whole period of cold exposure ( P < .05). After 2 weeks of cold exposure the daily water consumption increased and SBP began to increase. After 6 weeks of cold exposure the SBP was 30 mm Hg above that of the control level ( P < .001) and was accompanied by a 25% increase in whole blood viscosity ( P < .05). At the end of 8 weeks of cold exposure the plasma volume was 56.8 ± 9.51 mL/kg and the whole blood viscosity was 8.0 ± 1.79 cps at the 22.5 per sec shear rate. During the 5 weeks of rewarming the elevation of SBP and increased whole blood viscosity persisted, whereas the increased daily water consumption and expanded plasma volume returned to normal. Therefore, the acclimation to cold is accompanied by the development of a volume-associated hypertension, which is sustained after rewarming without volume expansion.

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