Spontaneous alteration of blood pH by a bicarbonate buffer system during experimental hypercalcaemia in cows
Categoria dell'articolo: Review article
Pubblicato online: 01 ott 2021
Pagine: 539 - 543
Ricevuto: 17 mar 2021
Accettato: 23 set 2021
DOI: https://doi.org/10.2478/jvetres-2021-0053
Parole chiave
© 2021 Y. Ro et al. published by Sciendo
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.
In dairy cows, disturbance of calcium (Ca) homeostasis causes productivity loss and production diseases (2, 7, 14). In the body, endocrine factors are mainly responsible for maintaining the balance of Ca, and their target organs include the intestines, the bones and kidneys (2, 8). However, to facilitate homeostatic processes, the entire environment of the body may be adjusted, including blood pH and the respiratory system (1, 4, 9, 10).
Many endocrine factors are known to control mineral levels, and the most well-known is the parathyroid hormone (PTH), the main function of which is to maintain optimal Ca levels in blood and to regulate Ca uptake or excretion by the bones and kidneys (1, 7, 8, 13, 14). Parathyroid hormone activity is optimal when blood pH is mildly acidic (1, 9, 10). Its antagonist calcitonin is secreted from the thyroid gland in a hypercalcaemic state and inhibits reabsorption of Ca and inorganic phosphate (iP) in the kidneys, thereby increasing the amount of Ca and iP excretion
Our previous study showed a spontaneous decrease in plasma pH in cows that had hypocalcaemia; such a drop in pH is considered to maximise the effect of PTH (3). Although the mechanism of pH change was not explained as the pH was measured using plasma, our study showed that there is a mechanism which regulates the body environment so as to maximise the effectiveness of endocrine factors. Therefore, the purpose of this study was to determine whether a spontaneous change in blood pH in dairy cows is induced by hypercalcaemia and what mechanism underlies such a change.
In the HYC group, the plasma Ca levels were significantly higher than their 0 h values until up to 8 h afterwards (P < 0.05). They were also significantly higher than those seen in the CON group from 1 to 8 h (P < 0.05, Fig. 1A). Furthermore, the HYC group had significantly different Ca /crea ratios from those of the CON group from 1 h to 12 h (P < 0.05), and they were higher from 1 h to 8 h after administration than at 0 h (P < 0.05, Fig. 1B). Mg levels were significantly higher in the HYC group from 1 h to 4 h after administration (P < 0.001, Fig. 1C), this group’s Mg /crea ratios were significantly different from 1 h to 4 h from those of the CON group, and they were significantly higher at 2 h and 4 h than at 0 h (P < 0.05, Fig. 1D).
Fig 1
Changes in plasma mineral concentrations, urinary mineral excretions, and blood gas parameters in the control group (CON) and induced hypercalcaemic group (HYC)
A – Ca concentration in plasma; B – Ca excretion through urine (Ca/creatine (crea)); C – Mg concentration in plasma; D – Mg excretion through urine (Mg/crea); E – blood pH; F – bicarbonate (HCO3−); G – partial pressure of carbon dioxide (pCO2); H – ionised Ca. Data are expressed as means ± standard deviation. * – significant difference compared to 0h (P < 0.05); ** – significant difference compared to 0 h (P < 0.001); a – significant difference compared to CON (P < 0.05); b – significant difference compared to CON (P < 0.001)

Blood pH in the HYC group showed a significant difference at 1 h and 2 h after administration from its 0 h value (P < 0.05), and significant differences between the two experimental groups were confirmed at 1 h and 4 h after administration (P < 0.05, Fig. 1E). HCO3− also differed significantly between the groups at 1 h and 2 h after administration (P < 0.05, Fig. 1F), as did pCO2 at 2 h (P < 0.05, Fig. 1G).
In the correlation analysis, pH was significantly correlated with HCO3− (
Results of Pearson correlation analysis of parameters in blood analyses in all individuals
Test (n) | Mg | Ca/crea | Mg/crea | iCa | pH | HCO3− | pCO2 | ||
---|---|---|---|---|---|---|---|---|---|
Ca | 0.599 | 0.825 | 0.698 | 0.917 | 0.466 | 0.490 | 0.220 | ||
(P value) | 90 | (<0.001)** | (<0.001)** | (<0.001)** | (<0.001)** | (<0.001)** | (<0.001)** | (0.037)* | |
Mg | 0.381 | 0.438 | 0.410 | 0.340 | 0.262 | 0.004 | |||
(P value) | 90 | (<0.001)** | (<0.001)** | (<0.001)** | (0.001)* | (0.013)* | (0.971) | ||
Ca/crea | 0.891 | 0.857 | 0.370 | 0.382 | 0.161 | ||||
(P value) | 90 | (<0.001)** | (<0.001)** | (<0.001)** | (<0.001)** | (0.131) | |||
Mg/crea | 0.712 | 0.345 | 0.380 | 0.181 | |||||
(P value) | 90 | (<0.001)** | (<0.001)** | (<0.001)** | (0.088) | ||||
iCa | 0.309 | 0.348 | 0.175 | ||||||
(P value) | 90 | (0.003)* | (<0.001)** | (0.098) | |||||
pH | 0.781 | 0.085 | |||||||
(P value) | 90 | (<0.001)** | (0.424) | ||||||
− HCO3 | 0.687 | ||||||||
(P value) | 90 | (<0.001)** |
Results of Pearson correlation analysis of Ca concentration with pH in the induced hypercalcaemic group
Test (n) | iCa | Ca/crea | pH | HCO3− | pCO2 | ||
---|---|---|---|---|---|---|---|
Ca | 0.933 | 0.846 | 0.688 | 0.672 | 0.206 | ||
(P value) | 45 | (<0.001)** | (<0.001)** | (<0.001)** | (<0.001)** | (0.174) | |
iCa | 45 | 0.860 | 0.542 | 0.549 | 0.194 | ||
(P value) | (<0.001)** | (<0.001)** | (<0.001)** | (0.201) | |||
Ca/crea | 0.511 | 0.486 | 0.125 | ||||
(P value) | 45 | (<0.001)** | (<0.001)** | (0.412) | |||
pH | 45 | 0.820 | 0.041 | ||||
(P value) | (<0.001)** | (0.788) | |||||
HCO3- | 0.603 | ||||||
(P value) | 45 | (<0.001)** |
Administration of Ca borogluconate caused a significant increase in plasma Ca concentration and urinary Ca excretion. Simultaneously, blood pH was more basic in the HYC group. The changing pattern of blood pH was similar to that of HCO3−, and the two values showed a strong correlation. Even though an acidic solution was administered, mildly alkaline blood pH was confirmed in the HYC group. This alteration was the opposite of the results of our previous study inducing the opposite state, hypocalcaemia, in which the deficit of Ca caused more acidic plasma pH, and probably resulted in the maximisation of the effect of PTH (9, 10, 12). As estimated in previous studies, there is a mechanism by which a decrease in blood pH results in an increase in the activity of PTH (9, 10, 13). The relationship between calcitonin, which lowers Ca levels in blood in a hypercalcaemic state, and blood pH has only been verified experimentally in hypocalcaemic status or
In conclusion, this study confirmed the change in blood pH concomitantly with the change of Ca concentration in blood during the induction of hypercalcaemia and recovery to normocalcaemia. Furthermore, our results suggest that this pH change was caused by the alteration of HCO3− concentration. Although mineralotropic hormones were not measured in the course of the experiment, changes in blood pH and HCO3− are presumed to be mechanisms that maintain Ca homeostasis. Therefore, in further studies, measurement of mineralotropic hormones at varied breeding stages and larger numbers of experimental animals are needed to clarify the mechanism.