The effect of electrolyte solutions on the unsaturated hydraulic conductivity of a sodic clay soil

Soil Research ◽  
1985 ◽  
Vol 23 (2) ◽  
pp. 301 ◽  
Author(s):  
DR Scotter

A technique for measuring the effect of different electrolyte solutions on the unsaturated hydraulic conductivity of low permeability soil cores is described. The technique was used to assess the effect of infiltrating gypsum (CaS0,.2H20) solution, sodium chloride solution, and distilled water on the conductivity of a sodic heavy clay at matric potentials between -0.5 and -8 kPa. Percolation of one liquid-filled pore volume of gypsum solution (concentration 29 m.e./l.) induced an approximately fourfold increase in hydraulic conductivity, relative to the conductivity with distilled water. This enhanced conductivity did not change when the permeating solution was changed to sodium chloride solution (30 m.e./l.). But when distilled water was substituted for either the gypsum or sodium chloride solutions, the conductivity declined rapidly, but not to its pretreatment value. Possible mechanisms responsible for the conductivity changes are discussed.

1925 ◽  
Vol 41 (6) ◽  
pp. 707-718 ◽  
Author(s):  
Russell L. Haden ◽  
Thomas G. Orr

Chemical changes are reported occurring in the blood of animals with obstruction of the jejunum, in which distilled water or sodium chloride solutions were introduced directly into the lumen of the intestine below the point of obstruction. Distilled water given daily from the beginning of the obstruction, had no influence on the development or course of the toxemia. 1 and 2 per cent salt solutions prevented a toxemia in uncomplicated cases. One animal so treated lived 30 days. Distilled water, given after the onset of toxemia, did not alter the progress or outcome of the toxemia. 10 per cent sodium chloride solution, administered after the onset of toxemia, controlled it in most cases for a long period. Hydrochloric acid had no effect on the course of the toxemia.


Processes ◽  
2018 ◽  
Vol 6 (8) ◽  
pp. 99 ◽  
Author(s):  
Shuzhao Chen ◽  
Donghua Zhang ◽  
Tao Shang ◽  
Tao Meng

The microstructures of rock gradually evolve with changes in the external environment. This study focused on the microstructure evolution of glauberite and its weakening mechanism under different leaching conditions. The porosity were used as a characteristic index to study the effect of brine temperature and concentration on crack initiation and propagation in glauberite. The research subjects were specimens of ϕ3 × 10 mm cylindrical glauberite core, obtained from a bedded salt deposit buried more than 1000 m underground in the Yunying salt formation, China. The results showed that when the specimens were immersed in solution at low temperature, due to hydration impurities, cracks appeared spontaneously at the centre of the disc and the solution then penetrated the specimens via these cracks and dissolved the minerals around the crack lines. However, with an increase of temperature, the dissolution rate increased greatly, and crack nucleation and dissolved regions appeared simultaneously. When the specimens were immersed in a sodium chloride solution at the same concentration, the porosity s presented gradual upward trends with a rise in temperature, whereas, when the specimens were immersed in the sodium chloride solution at the same temperature, the porosity tended to decrease with the increase of sodium chloride concentration. In the process of leaching, the hydration of illite, montmorillonite, and the residual skeleton of glauberite led to the expansion of the specimen volume, thereby producing the cracks. The diameter expansion rate and the expansion velocity of the specimen increased with temperature increase, whereas, due to the common-ion effect, the porosity of the specimen decreases with the increase of sodium chloride solution concentration.


Medicina ◽  
2007 ◽  
Vol 43 (5) ◽  
pp. 399 ◽  
Author(s):  
Rimantas Barauskas ◽  
Antanas Gulbinas ◽  
Giedrius Barauskas

The aim of this study was to establish a mathematical model of the infiltration of sodium chloride solution into cadaveric liver tissue. Methods. The time law of the flow of the infiltrated fluid at every node of the finite element model was obtained in terms of Darcy’s velocity, pressure, and volumetric saturation fraction. The model equations interpret the liver tissue as a porous medium taking into account the hydraulic conductivity, capacity, and absorption mechanisms. Capability of the cadaveric liver tissue to absorb the fluid is taken into account by means of the nonlinear relationship of hydraulic capacity and absorption coefficients against the volumetric saturation fraction. To explain certain inadequacies between the computational model and experiment, the idealized models of empty blood vessels in the vicinity of the injection probe have been used. The model has been implemented in computational environment COMSOL Multiphysics. Experimental procedures were performed to analyze fluid infiltration and to calculate volume of fluid, which might be injected into certain volume of nonviable liver tissue. Results. The necessary physical constants of hydraulic conductivity, capacity, and absorp- tion of liver tissue have been determined by comparing the simulation results against the experimental data. The congruence of the modeling results against the experiment may be regarded as satisfactory. Conclusion. The established model analyses distribution of injected solution taking into account the hydraulic conductivity, capacity, and absorption mechanisms of liver tissue. The obtained results are of importance developing complex models of electro-thermal heating coupled with heat advection by means of infiltrated sodium chloride solution.


1938 ◽  
Vol 9 (3) ◽  
pp. 339-341 ◽  
Author(s):  
F. H. McDowall ◽  
L. A. Whelan

Measurements are reported of the solubility, in water and in sodium chloride solution of different concentrations, of the protein of cheese at various times after manufacture. The solubility in 3–10 % sodium chloride solutions reached approximately 100% within 7 days after manufacture of the cheese, both for normal and high rennet cheese, and remained at that value throughout the life of the cheese (8 months). Since the proteins of cheese are thus shown to be equally soluble in sodium chloride solutions corresponding in concentration to those encountered in the whole range of commercial cheese(1), the effect of salt concentration on cheese quality is not to be attributed to a variation in the solubility of the protein in the brine.


Author(s):  
Mostafa H. Sharqawy ◽  
John H. Lienhard ◽  
Syed M. Zubair

Seawater is a complex electrolyte solution of water and salts with sodium chloride as the major constituent. However, the thermodynamic properties of seawater are considerably different from those of aqueous sodium chloride solution. In the literature, exergy analyses of seawater desalination systems have sometimes modeled seawater by sodium chloride solutions of equivalent salt content or salinity; however, such matching does not bring all important properties of the two solutions into agreement. Furthermore, some published studies attempt to represent sodium chloride solutions as a specific model for an ideal mixture of liquid water and solid sodium chloride, which is shown to have serious shortcomings. In this paper, the most up-to-date thermodynamic properties of seawater are compared with those of aqueous sodium chloride solution as well as the ideal mixture model. The flow exergy is calculated using various models and the results are compared. In addition, the minimum work required to desalinate a unit mass of fresh water from seawater of varying salinity is calculated using these models. The flow exergy calculated using the ideal mixture model in question is about 50% less than that of seawater. Accordingly, the minimum desalination work is underpredicted by about 50% when calculating it using that ideal mixture model. This consequently shows that exergy analysis and the second law efficiency calculations performed using the ideal mixture model is comparatively far from the actual values.


1909 ◽  
Vol 11 (3) ◽  
pp. 480-488
Author(s):  
Moyer S. Fleisher ◽  
Leo Loeb

1. Animals in which experimental myocarditis has been produced and winch are infused with sodium chloride solutions show a marked decrease in the amount of the secretion of urine. This decrease is even more pronounced than that produced when calcium chloride is added to sodium chloride solution. The intestinal fluid which is markedly decreased, and the peritoneal transudate which is increased by calcium chloride are, on the other hand, not markedly influenced by myocarditic lesions. We may, therefore, conclude that calcium chloride does not exert its specific effect on the quantity of peritoneal fluid through a lowering of blood pressure. 2. Each of the three factors, namely, calcium chloride, adrenalin and myocarditic lesions affects the elimination of fluid through the kidneys, through the mucosa of the small intestine and through the endothelial lining of the peritoneal cavity in a specific way. The conditions influencing the elimination of fluids through these three surfaces seem, therefore, to be different in each case and characteristic for the cells lining these surfaces.


1910 ◽  
Vol 12 (3) ◽  
pp. 288-310 ◽  
Author(s):  
Moyer S. Fleisher ◽  
Leo Loeb

1. Adrenalin injected intraperitoneally increases the rapidity of absorption of fluid from the peritoneal cavity, independently of whether the solution to be absorbed is hypotonic or hypertonic or is approximately isotonic with the blood serum. The intravenous injection of adrenalin also increases the absorption of fluid, but not so markedly as does the intraperitoneal injection. 2. Adrenalin injected either intraperitoneally or intravenously increases the quantity of sodium chloride absorbed. The relative absorption of sodium chloride—the movement from the peritoneal cavity of sodium chloride, as compared with the movement of water—is slightly increased when 0.85 per cent. of sodium chloride solution and adrenalin are injected intraperitoneally; but it is diminished when adrenalin is injected intravenously, or when 1.5 per cent. sodium chloride solution and adrenalin are injected. When distilled water has been injected intraperitoneally, adrenalin decreases the relative amount of sodium chloride in the peritoneal fluid—a fact that is evidently related to the increased elimination of sodium chloride through the kidneys under the influence of adrenalin. 3. When 0.85 per cent. sodium chloride solution is injected into the peritoneal cavity, the blood becomes diluted after two hours and a half. When adrenalin is also injected, the dilution of the blood is less marked, in spite of the increased absorption under the influence of adrenalin. When distilled water is injected into the peritoneal cavity, the blood is diluted equally in control and adrenalin experiments. When 1.5 per cent. sodium chloride solution is injected, the dilution of the blood is very slight, and in adrenalin experiments it is the same as in control experiments or very slightly greater than in control experiments. 4. The increase of absorption from the peritoneal cavity caused by the injection of adrenalin is not due to the increased diuresis caused by the injection of this substance. 5. The injection of adrenalin causes a temporary increase in the osmotic pressure of the blood, which gradually returns to normal. Under certain conditions, after the injection of adrenalin, there is a tendency toward maintaining the higher osmotic pressure of the blood serum, even up to the end of the experiment. We have reason to believe that this increase in the osmotic pressure of the blood is the main factor in increasing the absorption of fluid from the peritoneal cavity. 6. In experiments in which 0.85 per cent. sodium chloride solution has been injected intraperitoneally, either with or without adrenalin, there exists a tendency of the peritoneal fluid to attain a greater osmotic pressure than the blood serum, in spite of the fact that the injected fluid is slightly hypotonic as compared with the blood serum. We note a similar condition in cases of general edema in man, in which the osmotic pressure of the ascitic fluid is greater than that of the other edematous fluids, or even that of the blood serum. There exists, therefore, a mechanism that causes the passage of osmotically active substances from the blood or from the tissues into the peritoneal cavity, and that causes the osmotic pressure of the peritoneal fluid to become higher than that of the blood. It follows from our experiments that this mechanism, which causes the ascites in edematous persons to have such a high osmotic pressure, is not dependent upon certain pathological changes in the lining membranes or upon other pathological conditions, but exists already in normal animals. 7. The addition of 1.22 per cent. calcium chloride solution to 0.83 per cent. sodium chloride solution, in such proportions as we used in our infusion experiments, in which we determined the transudation into the peritoneal cavity, delays the absorption of fluid from the peritoneal cavity but very slightly. Therefore, calcium chloride increases directly the transudation into the peritoneal cavity and does not cause an increase in the amount of fluid in the peritoneal cavity merely by inhibiting the absorption. 8. It follows that adrenalin does not increase the amount of peritoneal transudate found after the intravenous infusion of large quantities of sodium chloride solution, to which adrenalin has been added, by delaying the absorption from the peritoneal cavity. The increased amounts of peritoneal fluid must be due to increased transudation into the peritoneal cavity; and the adrenalin, in view of its marked effect on absorption from the peritoneal cavity, must increase the movement of fluid into the peritoneal cavity much more strongly than could be assumed from the figures obtained in the infusion experiments.


2018 ◽  
Vol 103 (2) ◽  
pp. e1.16-e1
Author(s):  
Allport Grace ◽  
Playfor Stephen

AimBolus administration of 0.9% sodium chloride solution has been associated with hyperchloraemia, acidosis, acute kidney injury and increased mortality. Such adverse effects are believed to be less likely with balanced electrolyte solutions, such as Plasma- Lyte 148 or Hartmann’s solution. Despite existing evidence, 0.9% sodium chloride solution remains a popular choice for intravenous fluid boluses in paediatrics. This project aims to establish current practice of fluid bolus administration in paediatric patients, and to collect testimony from prescribers to help understand why decisions to prescribe specific fluids were made.MethodPaediatric patients in critical care areas (PICU and PHDU), the Emergency Department (PED) and in general ward areas who had been administered intravenous fluid boluses were identified using a pragmatic data collection technique and the dose, type of fluid, indication and patient’s weight were recorded. Where possible, the prescriber was identified and asked to be interviewed. Prescribers were asked what factors had affected their decision to prescribe the type and dose of fluid administered.ResultsMore than 30 individual episodes of intravenous fluid bolus administration were identified. Most fluid boluses were administered in PICU and PHDU, where balanced electrolyte solutions, specifically Plasma-Lyte 148, were the most popular choice. On general paediatric wards and in PED, 0.9% sodium chloride solution remained the most commonly administered fluid bolus solution. While some prescribers were able to give confident explanations of the factors involved in fluid selection, others referred to clinical guidelines. Individual prescribers described how their prescribing practice would vary according to the clinical setting; with senior clinicians and nursing staff being less accepting of balanced electrolyte solutions in general ward areas. Significant lack of knowledge of intravenous fluid physiology was demonstrated by some prescribers.ConclusionOur findings demonstrate an increase in the administration of balanced electrolyte solutions, such as Plasma-Lyte 148, as fluid boluses; this is in keeping with other international surveys of fluid administration.1,2 Similarly, we have also found significant differences in fluid bolus administration practice across different clinical areas as demonstrated by Jonsson and Perner in 2017.We have demonstrated the importance of on-going multi-disciplinary educational efforts in continuing the evolution of intravenous fluid bolus administration practice to reflect current best practice.ReferencesHammond NE, Taylor C, Finfer S, et al. Patterns of intravenous fluid resuscitation use in adult intensive care patients between 2007 and 2014: An international cross-sectional study. PLoS One2017;12:e0176292.Jonsson AB, Perner A. Changes from 2012 to 2015 in intravenous fluid solutions issued to hospital departments. Acta Anaesthesiol Scand2017;61:532–538.


2013 ◽  
Vol 2013 ◽  
pp. 1-6 ◽  
Author(s):  
Stefano Sbrignadello ◽  
Andrea Tura ◽  
Paolo Ravazzani

We investigated possible variations of impedance values in samples of sodium chloride solution (sodium chloride 0.9%) with glucose at different concentrations, ranging from 5000 to around 75 mg/dL. The sodium chloride solution (either saline physiological solution) was chosen since it has similarities to blood but no cell components, which may be confounding factors in this study. Special focus was on the effect of stirring and of temperature variations on the impedance spectrum of samples at different glucose concentrations. We found that variations in glucose concentration directly affect the impedance modulus of the sample both in static conditions and in dynamic conditions due to stirring, as well as at both room temperature and at increased temperature. In fact, even if the impedance variations were often small (around 3-4 mΩper mg/dL), they were usually clearly measurable. These findings may be the basis for possible development of a new approach, based on impedance technology, for the noninvasive monitoring of glycaemia.


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