Agarwal R, Afzalpurkar R, Fordtran J S
Department of Internal Medicine, Baylor University Medical Center, Dallas, Texas.
Gastroenterology. 1994 Aug;107(2):548-71. doi: 10.1016/0016-5085(94)90184-8.
When normal people ingest 90 mEq/day of K+ in their diet, they absorb about 90% of intake (81 mEq) and excrete an equivalent amount of K+ in the urine. Normal fecal K+ excretion averages about 9 mEq/day. The vast majority of intestinal K+ absorption occurs in the small intestine; the contribution of the normal colon to net K+ absorption and secretion is trivial. K+ is absorbed or secreted mainly by passive mechanisms; the rectum and perhaps the sigmoid colon have the capacity to actively secrete K+, but the quantitative and physiological significance of this active secretion is uncertain. Hyperaldosteronism increases fecal K+ excretion by about 3 mEq/day in people with otherwise normal intestinal tracts. Cation exchange resin by mouth can increase fecal K+ excretion to 40 mEq/day. The absorptive mechanisms of K+ are not disturbed by diarrhea per se, but fecal K+ losses are increased in diarrheal diseases by unabsorbed anions (which obligate K+), by electrochemical gradients secondary to active chloride secretion, and probably by secondary hyperaldosteronism. In diarrhea, total body K+ can be reduced by two mechanisms: loss of muscle mass because of malnutrition and reduced net absorption of K+; only the latter causes hypokalemia. Balance studies in patients with diarrhea are exceedingly rare, but available data emphasize an important role for dietary K+ intake, renal K+ excretion, and fecal K+ losses in determining whether or not a patient develops hypokalemia. The paradoxical negative K+ balance induced by ureterosigmoid anastomosis is described. The concept that fecal K+ excretion is markedly elevated in patients with uremia as an intestinal adaptation to prevent hyperkalemia is analyzed; we conclude that the data do not convincingly show the existence of a major intestinal adaptive response to chronic renal failure.
正常人饮食中摄入90mEq/天的钾时,他们吸收约90%的摄入量(81mEq),并在尿液中排出等量的钾。正常粪便钾排泄平均约为9mEq/天。绝大多数肠道钾吸收发生在小肠;正常结肠对钾的净吸收和分泌贡献微不足道。钾主要通过被动机制吸收或分泌;直肠以及可能的乙状结肠有主动分泌钾的能力,但这种主动分泌的定量和生理意义尚不确定。醛固酮增多症使肠道正常的人粪便钾排泄量每天增加约3mEq。口服阳离子交换树脂可使粪便钾排泄量增加至每天40mEq。腹泻本身不会干扰钾的吸收机制,但腹泻性疾病中粪便钾的丢失会因未吸收的阴离子(与钾结合)、主动分泌氯离子继发的电化学梯度以及可能的继发性醛固酮增多症而增加。在腹泻中,总体钾可通过两种机制减少:由于营养不良导致肌肉量减少以及钾的净吸收减少;只有后者会导致低钾血症。对腹泻患者进行的平衡研究极为罕见,但现有数据强调饮食钾摄入、肾脏钾排泄和粪便钾丢失在确定患者是否发生低钾血症方面的重要作用。文中描述了输尿管乙状结肠吻合术引起的矛盾性负钾平衡。分析了尿毒症患者粪便钾排泄显著升高作为肠道适应以预防高钾血症的概念;我们得出结论,数据并未令人信服地表明存在对慢性肾衰竭的主要肠道适应性反应。