Effects of cooling and freezing on pH of semen extender

The pH change of 10 different buffering systems with temperature ranging from room to 5 °C was examined; three were conventional buffers which included phosphate yolk, citrate yolk, and skim milk. Seven were Good's buffers with egg yolk which included TES, TRIS, BES, MOPS, PIPES, MES, and TEST. The pH of the three conventional buffers did not change with decreasing temperature, but Good's buffers showed an increase in pH with decreasing temperature from room to 5 °C. The pH change due to temperature was measured for TEST buffer solution with and without 20% egg yolk containing 2 or 6% of five different cryoprotective compounds. The pH at 5 °C was significantly higher than at room temperature. The addition of egg yolk and/or cryoprotective compound did not alter the pH significantly during cooling, even though a slight drop in pH was noted with the addition of egg yolk indicating that the change in pH is primarily due to the buffer. The pH of TEST yolk buffer (pH 7.2 at room temperature) was measured continuously from 37 °C to below freezing (?18 °C). The pH increased with decreasing temperature to 8.0 ± 0.2 from 37 to ?14 °C at which point it dropped abruptly to pH 6.5 ± 0.2.     

Buffer capacity of biologics—from buffer salts to buffering by antibodies

Controlling pH is essential for a variety of biopharmaceutical process steps. The chemical stability of biologics such as monoclonal antibodies is pH‐dependent and slightly acidic conditions are favorable for stability in a number of cases. Since control of pH is widely provided by added buffer salts, the current study summarizes the buffer characteristics of acetate, citrate, histidine, succinate, and phosphate buffers. Experimentally derived values largely coincide with values calculated from a model that had been proposed in 1922 by van Slyke. As high concentrated protein formulations become more and more prevalent for biologics, the self‐buffering potential of proteins becomes of relevance. The current study provides information on buffer characteristics for pH ranges down to 4.0 and up to 8.0 and shows that a monoclonal antibody at 50 mg/mL exhibits similar buffer capacity as 6 mM citrate or 14 mM histidine (pH 5.0–6.0). Buffer capacity of antibody solutions scales linearly with protein concentration up to more than 200 mg/mL. At a protein concentration of 220 mg/mL, the buffer capacity resembles the buffer capacity of 30 mM citrate or 50 mM histidine (pH 5.0–6.0). The buffer capacity of monoclonal antibodies is practically identical at the process relevant temperatures 5, 25, and 40°C. Changes in ionic strength of ΔI=0.15, in contrast, can alter the buffer capacity up to 35%. In conclusion, due to efficient self‐buffering by antibodies in the pH range of favored chemical stability, conventional buffer excipients could be dispensable for pH stabilization of high concentrated protein solutions. © 2013 American Institute of Chemical Engineers Biotechnol. Prog., 29: 480–492, 2013     

Design of experiments reveals critical parameters for pilot‐scale freeze‐and‐thaw processing of L‐lactic dehydrogenase

Freezing constitutes an important unit operation of biotechnological protein production. Effects of freeze‐and‐thaw (F/T) process parameters on stability and other quality attributes of the protein product are usually not well understood. Here a design of experiments (DoE) approach was used to characterize the F/T behavior of L‐lactic dehydrogenase (LDH) in a 700‐mL pilot‐scale freeze container equipped with internal temperature and pH probes. In 24‐hour experiments, target temperature between –10 and –38°C most strongly affected LDH stability whereby enzyme activity was retained best at the highest temperature of –10°C. Cooling profile and liquid fill volume also had significant effects on LDH stability and affected the protein aggregation significantly. Parameters of the thawing phase had a comparably small effect on LDH stability. Experiments in which the standard sodium phosphate buffer was exchanged by Tris‐HCl and the non‐ionic surfactant Tween 80 was added to the protein solution showed that pH shift during freezing and protein surface exposure were the main factors responsible for LDH instability at the lower freeze temperatures. Collectively, evidence is presented that supports the use of DoE‐based systematic analysis at pilot scale in the identification of F/T process parameters critical for protein stability and in the development of suitable process control strategies.     

Responses of Aquatic Fungal Communities on Leaf Litter to Temperature‐Change Events

Increases of extreme weather events are predicted to occur with ongoing climate change, but impacts to freshwaters have rarely been examined. We assessed the effects of temperature on leaf‐litter associated fungi by exposing leaves colonized in a stream to 18 °C (control), 25 °C, or 18 °C after freezing. Treatments altered fungal dominance on leaves; Lunulospora curvula sporulation was stimulated by increased temperature and stopped by the freeze‐thaw treatment. Fungal biomass and diversity decreased at 18 °C after freezing, but not at 25 °C. Leaf decomposition was retarded by the freeze‐thaw treatment (k = –0.024 day^–1) and stimulated at 25 °C (k = –0.069 day^–1). Results suggest that occasional freezing may constrain fungal diversity and their ecological functions, while warming appears to accelerate plant‐litter decomposition in streams. (© 2009 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)     

The use of pH indicators to identify suitable environments for freezing samples in aqueous and mixed aqueous/nonaqueous solutions

The colours of frozen solutions containing pH indicators are shown to provide a test for changes in pH in the solvent environment which occur on freezing. Yeast alcohol dehydrogenase loses activity on freezing in phosphate buffer (a buffer in which pH indicator colour changes shows a marked decrease in pH on freezing) but when frozen in bis-tris, Hepes, or N-glycylglycine buffers (all of which show little change in the colour of universal pH indicator and hence of pH on freezing) is stable on freezing. The effects of freezing in different buffer systems on the rate of decomposition of NADPH, and on the rate hydrolysis of 4-nitrophenyl acetate, are rationalised in terms of the pH shifts in these buffers which were determined using universal pH indicator. It is proposed that a major reason for the instability of samples on freezing is the pH changes which occur when some systems are frozen. From the results a general scheme for selecting the best environment for safely freezing samples is proposed which is based on the use of pH indicators.     

Bioluminescence characteristics of the fruiting body of Mycena chlorophos

Bioluminescent fungi are widely distributed on land and most belong to the class Basidomycetes. Light of about 530 nm wavelength maximum is emitted continuously. The molecular basis for the light‐emitting process remains unclear. We investigated the characteristics of the bioluminescence using cultivated fruiting bodies of M. chlorophos. Only fresh fruiting bodies exhibited long‐lasting light emission; rapid decay of light emission was observed with frozen and freeze‐dried samples. Freeze‐dried samples can be stored at room temperature under dry conditions and may be useful for the isolation of luciferin. The light emission of the fresh fruiting bodies was maintained in various buffers at varying pH; it could be stopped with pH 4 acetate buffer and could be recovered at pH 6. The isolation of luciferin from the fresh fruiting bodies might be possible by the control of buffer pH. The effect of temperature on the light emission of fruiting bodies indicated that bioluminescence in M. chlorophos may involve enzymatic reaction(s). The solubilization of bioluminescent components from the fruiting bodies could not be achieved with various surfactants. Copyright © 2011 John Wiley & Sons, Ltd.     

Importance of recent shifts in soil thermal dynamics on growing season length, productivity, and carbon sequestration in terrestrial high-latitude ecosystems

In terrestrial high‐latitude regions, observations indicate recent changes in snow cover, permafrost, and soil freeze–thaw transitions due to climate change. These modifications may result in temporal shifts in the growing season and the associated rates of terrestrial productivity. Changes in productivity will influence the ability of these ecosystems to sequester atmospheric CO₂. We use the terrestrial ecosystem model (TEM), which simulates the soil thermal regime, in addition to terrestrial carbon (C), nitrogen and water dynamics, to explore these issues over the years 1960–2100 in extratropical regions (30–90°N). Our model simulations show decreases in snow cover and permafrost stability from 1960 to 2100. Decreases in snow cover agree well with National Oceanic and Atmospheric Administration satellite observations collected between the years 1972 and 2000, with Pearson rank correlation coefficients between 0.58 and 0.65. Model analyses also indicate a trend towards an earlier thaw date of frozen soils and the onset of the growing season in the spring by approximately 2–4 days from 1988 to 2000. Between 1988 and 2000, satellite records yield a slightly stronger trend in thaw and the onset of the growing season, averaging between 5 and 8 days earlier. In both, the TEM simulations and satellite records, trends in day of freeze in the autumn are weaker, such that overall increases in growing season length are due primarily to earlier thaw. Although regions with the longest snow cover duration displayed the greatest increase in growing season length, these regions maintained smaller increases in productivity and heterotrophic respiration than those regions with shorter duration of snow cover and less of an increase in growing season length. Concurrent with increases in growing season length, we found a reduction in soil C and increases in vegetation C, with greatest losses of soil C occurring in those areas with more vegetation, but simulations also suggest that this trend could reverse in the future. Our results reveal noteworthy changes in snow, permafrost, growing season length, productivity, and net C uptake, indicating that prediction of terrestrial C dynamics from one decade to the next will require that large‐scale models adequately take into account the corresponding changes in soil thermal regimes.     

TWO SPECIFIC CAUSES OF CELL MORTALITY IN FREEZE‐THAW CYCLE OF YOUNG THALLI OF PORPHYRA YEZOENSIS (BANGIALES,RHODOPHYTA)1

Porphyra yezoensis Ueda is an important marine aquaculture crop with single‐layered gametophytic thalli. In this work, the influences of thallus dehydration level, cold‐preservation (freezing) time, and thawing temperature on the photosynthetic recovery of young P. yezoensis thalli were investigated employing an imaging pulse‐amplitude‐modulation (PAM) fluorometer. The results showed that after 40 d of frozen storage when performing thallus thawing under 10°C, the water content of the thalli showed obvious effects on the photosynthetic recovery of the frozen thalli. The thalli with absolute water content (AWC) of 10%–40% manifested obvious superiority compared to the thalli with other AWCs, while the thalli thawed at 20°C showed very high survival rate (93.10%) and no obvious correlation between thallus AWCs and thallus viabilities. These results indicated that inappropriate thallus water content contributed to the cell damage during the freeze‐thaw cycle and that proper thawing temperature is very crucial. Therefore, AWC between 10% and 40% is the suitable thallus water content range for frozen storage, and the thawing process should be as short as possible. However, it is also shown that for short‐term cold storage the Porphyra thallus water content also showed no obvious effect on the photosynthetic recovery of the thalli, and the survival rate was extremely high (100%). These results indicated that freezing time is also a paramount contributor of the cell damage during the freeze‐thaw cycle. Therefore, the frozen nets should be used as soon as time permits.     

Cooling rate affects rhesus monkey sperm survival

Background The rate at which lethal intracellular ice formation occurs during cryopreservation is highly dependent on several variables. The objective of this study was to determine the optimal rate at which rhesus sperm can be cooled. Methods Experiments were performed using three rates of cooling. Sperm motility was evaluated by computer‐assisted semen analysis, and post‐thaw viability was determined using propidium iodide labeling and flow cytometry. Semen was frozen at three cooling rates: (i) fast, (ii) slow, and (iii) standard. Straws were thawed for 30 s at 37°C for analysis of motility and viability. Results Post‐thaw motility and viability were comparable between freezing curves. Sperm cryopreserved using the slow freeze curve exhibited lowest motility and viability. Conclusions This study indicates that macaque sperm survive cooling optimally when cooling rates range from ?17 to ?34°C/minute. Conversely, slow cooling was detrimental and resulted in poor quality sperm.     

Characterization of γ-glutamyltranspeptidase in the liver of the frog: 3. Response to freezing and thawing in the freeze-tolerant wood frog Rana sylvatica

The freeze tolerant wood frog Rana sylvatica was studied to determine the impact of the freezing and thawing of this frog on the activity of γ-glutamyltranspeptidase in the liver. On exposure to ?2·5°C, for 1, 12 and 24 h, frogs were found to be cool, covered with ice crystals and frozen, respectively. Thawing for 24 h at 4°C recovered the frogs completely. A 45 per cent decrease in the liver weight: body weight ratio was notable after 1 h at ?2·5°C, suggestive of an early hepatic capacitance response. A glycemic response to freezing was observed: blood glucose levels exhibited a 55 per cent decrease after 1 h at ?2·5°C on cooling; a 10·5-fold increase after 12 h at ?2·5°C on the initiation of freezing; and a 22-fold increase after 24 h at ?2·5°C in the fully frozen state. Blood glucose levels remained elevated four-fold in the thawed state. Plasma insulin levels were increased twofold in the frozen state and 1·8-fold in the thawed state, while plasma ketone levels were increased 1·8-fold in the frozen state and 1·5-fold in the thawed state. Plasma total T₃ levels were decreased by 22 per cent in the frozen state and normalized on thawing. In homogenates and plasma membranes isolated from the livers of Rana sylvatica, the activity of γ-glutamyltranspeptidase was found to be elevated at all stages of the freeze–thaw process. After 1, 12 and 24 h at ?2·5°C, activities were increased 2·5-, 2·3-, 2·4-fold respectively in the homogenates and 2·5-, 2·2-, 2·4-fold respectively in the plasma membranes. After thawing, activities were still increased 1·9-fold in both homogenates and plasma membranes. In homogenates prepared from the kidneys of Rana sylvatica, the activity of γ-glutamyltranspeptidase was increased 1·4-fold after 1 h at ?2·5°C after which it returned to normal. The role of thyroid hormone in producing the increase in γ-glutamyltranspeptidase in the liver of Rana sylvatica in response to freezing is discussed as is the significance of the enzyme increase in terms of hepatic cytoprotection and freeze tolerance.     

Kinetic studies of electron transport reactions at low temperatures in xanthine oxidase.

Samples of rapidly frozen xanthine oxidase reduced with xanthine have been warmed between ?78°C and ?50°C. EPR measurements of oxidation — reduction processes at these temperatures have revealed a new EPR signal which appears to be a disulfide radical involved in xanthine hydrolysis. Other EPR signal changes indicate that at pH 6.5 enzyme reduction by xanthine is rate limiting and at pH 8.5 or higher that some step following enzyme reduction is rate limiting. Evidence is presented for the lack of anaerobicity in most rapid freeze apparatus, the oxygen entering the samples during rapid freeze quenching in isopentane.     

Enthalpy and heat capacity changes for the proton dissociation of various buffer components in 0.1 M potassium chloride

Enthalpy and heat capacity changes for the deprotonation of 18 buffers were calorimetrically determined in 0.1 M potassium chloride at temperatures ranging from 5 to 45°C. The values of the dissociation constant were also determined by means of potentiometric titration. The enthalpy changes for the deprotonation of buffers, except for the phosphate and glycerol 2-phosphate buffers, were found to be characterized by a linear function of temperature. The enthalpy changes for the second dissociation of phosphate and glycerol 2-phosphate where divalent anion is formed on dissociation were fitted with the second order function of temperature rather than the first order. Temperature dependence of buffer pH calculated by using the enthalpy and heat capacity changes obtained was in good agreement with the temperature variation of the pH values actually measured in the temperature range between 0 and 50°C for all the buffers studied. On the basis of the results obtained, a numeric table showing the temperature dependence of pK values for the 18 buffers is presented. Proteins 33:159–166, 1998. © 1998 Wiley-Liss, Inc.     

The dehalogenation of halocytosines by bisulfite buffers

Both 5-bromo- and 5-iodocytosine are rapidly dehalogenated in dilute bisulfite buffers to yield cytosine. With 5-bromocytosine, but not with 5-iodocytosine, extrapolation of semilogarithmic plots of extent reaction versus time indicates the bisulfite buffer concentration-dependent formation of an intermediate which subsequently reacts to control the rate of 5-bromocytosine dehalogenation. The disappearance of both halocytosines has a second-order dependence on bisulfite buffer concentration. Both imidazole and acetate buffers catalyze the reaction of 5-iodocytosine, but not that of 5-bromocytosine, with bisulfite. In the case of acetate buffer catalysis of the reaction of 5-iodocytosine with bisulfite, the dependence of the observed rate constants changes from first order to zero order as a function of increasing buffer concentration. The observed rate constants for 5-bromocytosine dehalogenation increase, reach a maximum at about 4.5, and then decrease as a function of pH. Iodometric titration of sulfite utilization coupled with spectrophotometric analysis of pyrimidine reactants and products indicates that 1 mole of sulfite is consumed per mole of halocytosine dehalogenated. The spectrophotometrically determined pK_a values for the conjugate acids of 5-bromo- and 5-iodocytosine at 25°C and ionic strength 1.0 M are 3.25 and 3.56, respectively. These results are discussed in terms of a multistep reaction pathway which is analogous to the bisulfite-catalyzed dehalogenation of the 5-halouracils.     

Freezing Injury in Onion Bulb Cells: II. Post-thawing Injury or Recovery

Onion (Allium cepa L.) bulbs were subjected for 12 days to either a moderate freeze (−4 C) or a severe freeze (−11 C). They were then thawed slowly over ice. During 7 to 12 days following the thaw, the injury progressed with time in the severely frozen bulbs, but appeared completely repaired in the moderately frozen bulbs. This was shown by the following post-thawing changes.     

Deamidation of glutaminyl residues: dependence on pH, temperature, and ionic strength

We have shown the dependence of the deamidation half-times of the peptides, GlyLeuGlnAlaGly and GlyArgGlnAlaGly upon pH, temperature, and ionic strength. Increase in temperature or ionic strength, variation of pH to pH′s higher or lower than pH 6, and the use of phosphate buffer rather than Tris buffer at high pH all decrease the half-time of dcamidation. Temperature increase of 20°C or pH change of 2 pH units decreases the half-time about fivefold, while increase of one ionic strength unit decreases the half-time about twofold. In pH 7.4, I = 0.2, 37.0°C phosphate buffer, the deamidation half-times are 663 ± 74 and 389 ± 56 days respectively for the two peptides, GlyLeuGlnAlaGly and GlyArgGlnAlaGly.These experiments should serve as a warning to peptide and protein experimenters that even the more stable glutaminyl residues are unstable with respect to deamidation in certain solvent conditions. These experiments also provide, along with previously reported experiments on asparaginyl peptides (7), some quantitative data to help with the extrapolation of in vitro deamidation experiments to in vivo deamidation conditions.     

Spatial extent of winter thaw events in eastern North America: historical weather records in relation to yellow birch decline

An algorithm (Weather Reader) was developed and used to analyze daily weather records from all existing Canadian and American weather stations of eastern North America (in excess of 2100 stations), from 1930 through 2000. Specifically, the Weather Reader was used to compile daily minimum, mean, and maximum air temperatures for weather stations with at least 30 years of data, and was used to calculate accumulated degree days for winter thaw–freeze events relevant to yellow birch (Betula alleghaniensis Britt.) from beginning to end. A thaw–freeze event relevant to yellow birch was considered to take place when (i) the station daily maximum temperature reached or exceeded +4°C after being below freezing for at least 2 months of the winter, (ii) sufficient growing degree days accumulated (>50 growing degree days) to cause the affected yellow birch trees to prematurely deharden, and (iii) the daily minimum temperature dropped below ?4°C causing roots and/or shoots of dehardened trees to experience freeze‐induced injury and possibly dieback. The threshold temperature of +4°C represents the daily temperature above which biological activity occurs in yellow birch. The station growing degree day summaries were subsequently spatially interpolated with the Kriging function in GS+^? and mapped in ArcView^? GIS in order to display the geographic extent of the most severe thaw–freeze events. The ArcView^? maps were then compared with the extent of historically observed yellow birch decline. It was found that the years 1936, 1944, and 1945 were particularly uncharacteristic in terms of region‐wide winter thaw–freeze extremes, and also in terms of observed birch decline events during 1930–1960. An overlay of suspected accumulated birch decline based on thaw–freeze mapping and observed decline maps prepared by Braathe (1995), Auclair (1987) , and Auclair et al. (1997) for 1930–1960 demonstrated similar geographic patterns. The thaw–freeze projection for 1930–1960 was shown to coincide with 83% of the birch decline map appearing in Braathe (1995) and 55% of the geographic range of yellow birch in eastern North America. Thaw–freeze mapping was also applied to two significant events in 1981. Greatest impact was recorded to occur mostly in southern Quebec and Ontario, and several American Great Lake States, specifically in northern Michigan and New York, where the greatest growing degree day accumulation prior to refreeze in late February (February 28th) was projected to have occurred; and in southern Quebec, most of Atlantic Canada, and Maine, prior to a late spring frost in mid‐April (April 17).     

A model-dependent approach to correlate accelerated with real-time release from biodegradable microspheres

The purpose of this study was to determine the feasibility of applying accelerated in vitro release testing to correlate or predict long-term in vitro release of leuprolide poly(lactideco-glycolide) microspheres. Peptide release was studied using a dialysis technique at 37°C and at elevated temperatures (50°C–60°C) in 0.1 M phosphate buffered saline (PBS) pH 7.4 and 0.1 M acetate buffer pH 4.0. The data were analyzed using a modification, of the Weibull equation. Peptide release was temperature dependent and complete within 30 days at 37°C and 3 to 5 days at the elevated temperatures. In vitro release profiles at the elevated temperatures correlated well with release at 37°C. The shapes of the release profiles at all temperatures were similar. Using the modified Weibull equation, an increase in temperature was characterized by an increase in the model parameter, α, a scaling factor for the apparent rate constant. Complete release at 37°C was shortened from ∼30 days to 5 days at 50°C, 3.5 days at 55°C, 2.25 days at 60°C in PBS pH 7.4, and 3 days at 50°C in acetate buffer pH 4.0. Values for the model parameter β indicated that the shape of the release profiles at 55°C in PBS pH 7.4 (2.740) and 50°C in 0.1 M acetate buffer pH 4.0 (2.711) were similar to that at 37°C (2.577). The E_a for hydration and erosion were determined to be 42.3 and 19.4 kcal/mol, respectively. Polymer degradation was also temperature dependent and had an E_a of 31.6 kcal/mol. Short-term in vitro release studies offer the possibility of correlation with long-term release, thereby reducing the time and expense associated with longterm studies. Accelerated release methodology could be useful in the prediction of long-term release from extended release microsphere dosage forms and may serve as a quality control tool for the release of clinical or commercial batches. Selected for the 2005 AAPS Outstanding Graduate Student Research Award in Pharmaceutical Technologies Sponsored by Solvay Pharmaceuticals.     

Magnetic resonance imaging (MRI) as a method for determination of freezing injury in strawberry crowns

In an experiment with controlled freezing, strawberry plants were exposed to 0, ?8, ?12, ?16 and ?20°C at a freeze and thaw rate of 2 °C/hour in March/April 1996. Crowns from the cultivar ‘Korona’ were examined using magnetic resonance imaging (MRI), showing a gradual increase of signal intensity from the centre of the crowns, as a result of the temperature drop, which might be caused by lipids. The increase in signal intensity was in accordance with the tissue browning of crowns, which increased substantially when the temperature dropped below ?12 °C. A similar reaction was shown in a field experiment comparing wintercovered and not wintercovered strawberry plants. The plants which had been exposed to temperatures between ?10 and ?16 °C were severely injured. This demonstrates that MRI has a potential as an objective method to determine freeze injury in the field, by «calibrating» the MRI instrument to freezing profiles in controlled experiments.     

Annual ecosystem respiration is resistant to changes in freeze–thaw periods in semi‐arid permafrost

Warming in cold regions alters freezing and thawing (F–T) of soil in winter, exposing soil organic carbon to decomposition. Carbon‐rich permafrost is expected to release more CO₂ to the atmosphere through ecosystem respiration (Re) under future climate scenarios. However, the mechanisms of the responses of freeze – thaw periods to climate change and their coupling with Re in situ are poorly understood. Here, using 2 years of continuous data, we test how changes in F–T events relate to annual Re under four warming levels and precipitation addition in a semi‐arid grassland with discontinuous alpine permafrost. Warming shortened the entire F–T period because the frozen period shortened more than the extended freezing period. It decreased total Re during the F–T period mainly due to decrease in mean Re rate. However, warming did not alter annual Re because of reduced soil water content and the small contribution of total Re during the F–T period to annual Re. Although there were no effects of precipitation addition alone or interactions with warming on F–T events, precipitation addition increased total Re during the F–T period and the whole year. This decoupling between changes in soil freeze – thaw events and annual Re could result from their different driving factors. Our results suggest that annual Re could be mainly determined by soil water content rather than by change in freeze – thaw periods induced by warming in semi‐arid alpine permafrost.     

Rapid down regulation of insulin receptors in adipocytes artifact of the incubation buffer

Rat adipocytes were incubated with 15 nM insulin in different buffers at 37°C. The cells were washed and reincubated at 16°C in the presence of 18 pM A14-[¹²⁵I]monoiodoinsulin to determine the insulin receptor concentration. After incubation for 2 h in Tris buffer the binding decreased to about 30 %, whereas no decrease was found after incubation in Hepes, phosphate or bicarbonate buffers. Binding of tracer insulin reached a constant level by 45 min in Hepes buffer at 37°C, whereas it continued to increase in Tris buffer. Washout of tracer insulin after incubation in Tris buffer at 37°C showed a large, slowly dissociable fraction. It is suggested that the rapid down regulation of insulin receptors $\text{in}\text{vitro}$ is an artifact of the Tris buffer and that the phenomenon is due to a slowly reversible occupancy of a receptor pool with unlabelled insulin.