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正常和脱水家禽(家鸡)泄殖腔和大肠上皮对氯化钠的吸收及溶质相关的水流。体内灌注研究。

Sodium chloride absorption and solute-linked water flow across the epithelium of the coprodeum and large intestine in the normal and dehydrated fowl (Gallus domesticus). In vivo perfusion studies.

作者信息

Bindslev N, Skadhauge E

出版信息

J Physiol. 1971 Aug;216(3):753-68. doi: 10.1113/jphysiol.1971.sp009551.

Abstract
  1. The transmural net flow of salt and water in the coprodeum and large intestine of normal and dehydrated hens was investigated by means of an intraluminal in vivo perfusion technique. The lumen was perfused with hypo-, iso-, and hyperosmotic salt solutions. Polyethylene glycol (PEG 4000) and [(14)C]inulin served as water markers.2. The maximal net Na(+) flow (J(Na)) from the mucosal to the serosal side was nearly the same in the two states of hydration: normal birds 308 mu-equiv/kg.hr, dehydrated birds 281 mu-equiv/kg.hr, while the J(Na) was half maximal at luminal Na(+) concentrations of 99 and 43 mu-equiv/l. respectively. The ;affinity' for Na(+) in the dehydrated bird was thus twice that in the normal bird. K(+) was secreted into the gut lumen at a constant rate against the electrochemical gradient, J(K) = -97 mu-equiv/kg.hr (S.E. = 5). Cl(-) was absorbed from lumen to plasma down the electrochemical gradient with J(Cl) ranging from 0 to 94 mu-equiv/kg.hr. The low J(Cl) was observed at low luminal NaCl concentrations when the J(Na) was also small.3. The solute-linked water flow, J(vs), occurring in the absence of an osmolality difference across the epithelium, was 1.1 mul. H(2)O/mu-equiv Na(+) in normal birds and 1.5 in dehydrated birds. The J(vs) was calculated as an operational parameter in experiments with luminal osmolalities different from plasma osmolality by subtracting the water flow observed in an experiment without Na(+) in the perfusion fluid from the water flow in an experiment with Na(+) containing perfusion fluids, both fluids being of the same osmolality. J(vs) was maximal at luminal osmolalities close to plasma osmolality. These observations are compatible with the hypothesis that the J(vs) is due to an osmotic flow into a confined region between the cells.4. When the perfusion rate was lowered from 5-9 ml./kg.hr to 0.8-1.0 the incoming perfusion fluid osmolality at which net water flow across the epithelium was zero went up from 100 to 180 m-osmolal higher than plasma osmolality. This observation suggests that a significant fraction of ureteral urine in the dehydrated bird may be absorbed in the coprodeum and large intestine.
摘要
  1. 采用腔内活体灌注技术,研究了正常和脱水母鸡泄殖腔和大肠中盐和水的跨壁净流量。向肠腔灌注低渗、等渗和高渗盐溶液。聚乙二醇(PEG 4000)和[¹⁴C]菊粉用作水标记物。

  2. 两种水合状态下,从黏膜侧到浆膜侧的最大净钠流量(J(Na))几乎相同:正常鸡为308微当量/千克·小时,脱水鸡为281微当量/千克·小时,而在肠腔钠浓度分别为99和43微当量/升时,J(Na)为最大值的一半。因此,脱水鸡对钠的“亲和力”是正常鸡的两倍。钾以恒定速率逆电化学梯度分泌到肠腔中,J(K)= -97微当量/千克·小时(标准误=5)。氯沿电化学梯度从肠腔吸收到血浆中,J(Cl)范围为0至94微当量/千克·小时。当J(Na)也很小时,在低肠腔氯化钠浓度下观察到低J(Cl)。

  3. 在跨上皮不存在渗透压差异时发生的溶质相关水流J(vs),正常鸡为1.1微升H₂O/微当量钠,脱水鸡为1.5。J(vs)是通过从含钠灌注液实验中的水流中减去灌注液中无钠实验中观察到的水流来计算的,这两个实验中两种液体渗透压相同,是在肠腔渗透压与血浆渗透压不同的实验中的一个操作参数。J(vs)在肠腔渗透压接近血浆渗透压时最大。这些观察结果与J(vs)是由于渗透流入细胞间受限区域的假设一致。

  4. 当灌注速率从5 - 9毫升/千克·小时降至0.8 - 1.0时,跨上皮净水流为零时进入的灌注液渗透压比血浆渗透压高出100至180毫渗摩尔。这一观察结果表明,脱水鸡输尿管尿液的很大一部分可能在泄殖腔和大肠中被吸收。

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