添加沸石A钠对饲喂草青贮的干性、非妊娠奶牛的生理影响。

J M Enemark, A M Frandsen, T Thilsing-Hansen, R J Jørgensen
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引用次数: 0

摘要

本研究的目的是监测奶牛在口服合成硅酸铝钠(沸石a)期间和之后的血清和尿液生化变化。选择了一项前瞻性纵向研究,涉及4头未怀孕和未泌乳的奶牛。奶牛随机分为对照组和试验组。观察期为3周。在第一周(第1期),奶牛维持基本日粮,以记录基线值。第2周(第2期),对照奶牛饲喂基础饲粮(草青贮),试验组奶牛在基础饲粮的基础上添加1 kg沸石颗粒,每日1次。第3周(第3期),两组均饲喂基础日粮,观察停用沸石后是否有持续效果。每日取样包括血液和尿液。比较第2期和第3期各组间选定的生理参数,比较第1、2和3期各组内的平均值。添加沸石对钙稳态有显著影响。实验组在开始补充时血清钙和肾钙排泄量略有下降,而在停止补充沸石后,这些参数均有所增加。据推测,在补充期间,沸石导致膳食钙的可用性减少,这可能引起钙动员的激活。从监测血清钙调节激素(PTH、1,25(OH)2D3、25(OH)VitD)浓度或骨吸收标志物的肾脏排泄情况来看,沸石对钙稳态的影响并不明显。因此,在本实验条件下,肠道主动钙吸收和骨吸收的增强在钙动员中被认为是微不足道的。沸石去除后血清和尿液中钙含量增加的原因目前尚不清楚,但有人认为,骨中易于动员的钙池是一个促成因素。实验组的血清浓度和分数排泄值均显著低于对照组,证实了沸石对磷酸盐和镁稳态的影响。沸石对磷和镁的影响被认为是由于沸石干扰肠道吸收和少量补充这些矿物质的综合结果。
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Aspects of physiological effects of sodium zeolite A supplementation in dry, non-pregnant dairy cows fed grass silage.

The objective of the present study was to monitor serum and urine biochemical changes in dairy cows during and after oral administration of a synthetic sodium aluminium-silicate (zeolite A). A prospective longitudinal study involving four non-pregnant and non-lactating cows was chosen. Cows were randomly allocated to either a control or experimental group. The period of observation was three weeks. During the first week (period 1) cows were maintained on basic ration for the purpose of recording baseline values. During the second week (period 2) control cows were fed a basic diet (grass silage), while cows in the experimental group were fed the basic diet and supplemented with 1 kg zeolite pellets once daily. During the third week (period 3) both groups were fed the basic ration only and observed for any persistent effects after zeolite withdraw. Daily sampling included blood and urine. Selected physiological parameters were compared between groups during period 2 and 3, whereas mean values from period 1, 2 and 3 were compared within the groups. Zeolite supplementation revealed a significant influence on calcium homeostasis. A slight decrease in serum Ca and in renal excretion of calcium was observed in the experimental group at initiation of supplementation, whereas an increment in these parameters was recorded after withdrawal of zeolite supplementation. It is assumed, that zeolite caused a reduction in the availability of dietary calcium during supplementation, which possibly elicited an activation of calcium mobilisation. The influence of zeolite on calcium homeostasis was not evident from monitoring serum concentration of calcium regulating hormones (PTH, 1,25(OH)2D3, 25(OH)VitD) or renal excretion of markers of bone resorption. Enhanced active intestinal calcium absorption and bone resorption was therefore considered insignificant in the calcium mobilisation under the conditions of this experiment. The origin of the increased amount of Ca, which was observed in serum and urine after zeolite withdraw, is at present unknown, but it is suggested, that the readily mobilized Ca-pool in bone was a contributing factor. An effect of zeolite on phosphate and magnesium homeostasis in the experimental group was evidenced from the values of serum concentration and fractional excretion, which during supplementation were significant lower than in the control group. The influence of zeolite on phosphorus and magnesium is presumed to result from a combination of interference of zeolite with intestinal absorption and a marginal dietary supplementation of these minerals.

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