Role of core body temperature in nephrolithiasis

被引:1
|
作者
Srirangapatanam, Sudarshan [1 ]
Wiener, Scott [2 ]
Stoller, Marshall L. [1 ]
机构
[1] Univ Calif San Francisco, Dept Urol, San Francisco, CA USA
[2] SUNY Upstate Med Univ, Dept Urol, Syracuse, NY 13210 USA
关键词
nephrolithiasis; urolithiasis; kidney stones; body temperature; thermoregulation; physiopathology; STONE; PLAQUE;
D O I
10.1111/bju.15185
中图分类号
R5 [内科学]; R69 [泌尿科学(泌尿生殖系疾病)];
学科分类号
1002 ; 100201 ;
摘要
Objectives To assess the role of core body temperature in urinary stone formation using a large clinical dataset. Patients and Methods We retrospectively collected 14 519 039 individual temperature measurements from 580 416 patients with medical history, laboratory values and medication history between 2013 and 2018 at a single institution. After exclusions and matching 2:1 (controls:cases) to account for confounding variables, 7104 patients with a history of urinary stones were identified. Results Patients with a history of urinary stones (cases) had an elevated mean (SD) oral temperature compared to matched controls, at 36.666 (0.17) vs 36.659 (0.20)degrees C (P = 0.012). Logistic regression of matched samples showed that higher core body temperature was predictive of a history of nephrolithiasis (odds ratio 1.21, 95% confidence interval 1.04-1.4;P = 0.015). Conclusion Core body temperature was significantly higher in patients with a history of urinary stones compared to matched controls, contrary to the anticipated thermodynamic considerations leading to crystal aggregation. Given that the core body temperature is elevated, rather than decreased, thermodynamic process driving stone formation is unlikely.
引用
收藏
页码:620 / 624
页数:5
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