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PubMed1988

Interactions of concanavalin A with asparagine-linked glycopeptides: formation of homogeneous cross-linked lattices in mixed precipitation systems.

We have previously shown that certain oligomannose and bisected hybrid type glycopeptides are bivalent for binding to concanavalin A (Con A) [Bhattacharyya, L., Ceccarini, C., Lorenzoni, P., & Brewer, C. F. (1987) J. Biol. Chem. 262, 1288-1293]. Each glycopeptide gives a quantitative precipitation profile with the protein which consists of a single peak that corresponds to the binding stoichiometry of glycopeptide to protein monomer (1:2). We have shown that the affinities of the primary and secondary sites of the glycopeptides influence their extent of precipitation with the lectin [Bhattacharyya, L., & Brewer, C. F. (1988) Eur. J. Biochem. (in press)]. In the present study, we demonstrate that equimolar mixtures of any two of the glycopeptides result in a quantitative precipitation profile which shows two protein peaks. Using radiolabeled glycopeptides, the precipitation profiles of the individual glycopeptides were determined. The results show that each glycopeptide forms its own precipitation profile with the protein which is independent of the profile of the other glycopeptide. For mixtures containing an equimolar ratio of two glycopeptides, the glycopeptide with lower affinity shows a precipitation maximum at a lower concentration than the one with higher affinity. However, this can be reversed by increasing the ratio of the lower affinity glycopeptide in the mixture. Thus, the relative precipitation maxima of the glycopeptides are determined by mass-action equilibria involving competitive binding of the two carbohydrates to the protein. These equilibria, in turn, are sensitive to the relative amounts and affinities of the carbohydrates at both their primary and secondary sites.(ABSTRACT TRUNCATED AT 250 WORDS)

Asparagine↗

PubMed2003

Effects of daily precipitation and evapotranspiration patterns on flow and VOC transport to groundwater along a watershed flow path.

MTBE and other volatile organic compounds (VOCs) are widely observed in shallow groundwater in the United States, especially in urban areas. Previous studies suggest that the atmosphere and/or nonpoint surficial sources could be responsible for some of those VOCs, especially in areas where there is net recharge to groundwater. However, in semiarid locations where annual potential evapotranspiration can exceed annual precipitation, VOC detections in groundwater can be frequent. VOC transport to groundwater under net discharge conditions has not previously been examined. A numerical model is used here to demonstrate that daily precipitation and evapotranspiration (ET) patterns can have a significant effect on recharge to groundwater, watertable elevations, and VOC transport. Ten-year precipitation/ET scenarios from six sites in the United States are examined using both actual daily observed values and "average" pulsed precipitation. MTBE and tetrachloroethylene transport, including gas-phase diffusion, are considered. The effects of the precipitation/ET scenarios on net recharge and groundwater flow are significant and complicated, especially under low-precipitation conditions when pulsed precipitation can significantly underestimate transport to groundwater. In addition to precipitation and evapotranspiration effects, location of VOC entry into the subsurface within the watershed is important for transport in groundwater. This is caused by groundwater hydraulics at the watershed scale as well as variations in ET within the watershed. The model results indicate that it is important to consider both daily precipitation/ET patterns and location within the watershed in order to interpret VOC occurrence in groundwater, especially in low-precipitation settings.

Carcinogens↗

PubMed2005

Simulation of a crossover from the precipitation wave to moving Liesegang pattern formation.

Model simulations to investigate the precipitation wave phenomenon and a crossover from the precipitation wave to moving Liesegang patterns were performed. The chemical scheme contains four chemical species via the interaction of precipitation and redissolution (complex formation), in which the precipitation reaction term was based on Ostwald's supersaturation theory. In this article, for the first time, all the features and behaviors of the heterogeneous traveling waves are reproduced, which were observed experimentally in the work of Zrínyi et al. (Zrínyi, et al. J. Phys. Chem. 1991, 95, 1618.). The detailed investigation of the pattern formation showed three possible states of the system, which depend on the initial concentration of the inner and outer electrolytes, respectively. These are the precipitation wave (single moving precipitation band), the moving Liesegang pattern (moving precipitation bands), and the state where these two patterns coexist.

Journal Article↗

PubMedDate not supplied

Trace element patterns and seasonal variability of dust precipitation in a low polluted city--the example of Karlsruhe/Germany.

Urban areas of different land uses can be distinguished by their specific patterns of atmospheric dust and trace element precipitation. Dusts emitted from industrial areas with fossil fuel processing, for instance, are enriched in V, Ni and Co. Cluster analysis groups sampling sites based on their specific element patterns. The resulting groups correspond to the surrounding land use: Urban sampling sites were identified showing similar patterns of dust and trace element precipitation as a reference site; dusts of other urban sites were influenced by diffuse pollution (caused by non-point and dispersed pollution sources), or by specific industrial emissions. Cluster analysis was also used to characterize the chemical dust composition. Three clusters of typical element associations were distinguished. These clusters represent the dust matrix, diffuse urban pollution and pollution due to fossil fuel processing. Dust precipitation and chemical dust composition show seasonal variations. Dust precipitation and concentrations of trace elements in the precipitated dust are negatively correlated during the annual courses. The highest concentrations of trace elements occur during winter, whereas the highest precipitations of dust were found during summer. This finding stresses that both, precipitation and concentration have to be addressed for the environmental assessment of urban dusts.

Air Pollutants↗

PubMed2004

Development and characterization of a scalable controlled precipitation process to enhance the dissolution of poorly water-soluble drugs.

PURPOSE: Poorly water-soluble compounds are being found with increasing frequency among pharmacologically active new chemical entities, which is a major concern to the pharmaceutical industry. Some particle engineering technologies have been shown to enhance the dissolution of many promising new compounds that perform poorly in formulation and clinical studies (Rogers et. al., Drug Dev Ind Pharm 27:1003-1015). One novel technology, controlled precipitation, shows significant potential for enhancing the dissolution of poorly soluble compounds. In this study, controlled precipitation is introduced; and process variables, such as mixing zone temperature, are investigated. Finally, scale-up of controlled precipitation from milligram or gram to kilogram quantities is demonstrated. METHODS: Dissolution enhancement capabilities were established using two poorly water-soluble model drugs, danazol and naproxen. Stabilized drug particles from controlled precipitation were compared to milled, physical blend, and bulk drug controls using particle size analysis (Coulter), X-ray powder diffraction (XRD), scanning electron microscopy (SEM), dissolution testing (USP Apparatus 2), and residual solvent analysis. RESULTS: Stabilized nano- and microparticles were produced from controlled precipitation. XRD and SEM analyses confirmed that the drug particles were crystalline. Furthermore, the stabilized particles from controlled precipitation exhibited significantly enhanced dissolution properties. Residual solvent levels were below FDA limits. CONCLUSIONS: Controlled precipitation is a viable and scalable technology that can be used to enhance the dissolution of poorly water-soluble pharmaceutical compounds.

Chemistry, Pharmaceutical↗

PubMed1990

Role of precipitating and nonprecipitating antibodies in glomerular immune complex formation.

The present study compared directly the ability of precipitating and nonprecipitating antibodies to form and sustain glomerular immune deposits. The antigen phenylated gelatin (DNP-GL) was injected i.v. into rats. DNP-GL is cleared from the circulation rapidly and becomes localized in glomeruli. Two hours later, rats received either precipitating or nonprecipitating mouse monoclonal anti-DNP antibodies. These antibodies were comparable with respect to size, affinity, number of antigen combining sites and isoelectric point. However, in vitro, nonprecipitating antibodies demonstrated a faster dissociation rate from antigen than precipitating antibodies. Control rats received DNP-GL alone or antibody alone. Antibody deposition in glomeruli was quantitated by Computerized Image Analysis (CIA) of immunoperoxidase stained tissue sections and by glomerular radioactive counts in experiments using 125I labelled antibodies. We demonstrated that glomerular uptake of anti-DNP antibody was similar two hours after injection of precipitating and nonprecipitating antibodies. However, six or more hours after injection, significantly less antibody was present in the glomeruli of rats injected with nonprecipitating antibodies. These differences could not be explained by a greater rate of antigen removal from kidney in rats injected with nonprecipitating antibodies. To assess whether nonprecipitating antibodies modify the glomerular binding and retention of precipitating antibody, in a separate series of experiments rats were injected with equal amounts of precipitating and nonprecipitating antibodies. Both types of antibody bound to glomeruli. However, with time glomerular antibody levels paralleled those found in rats injected with nonprecipitating antibody alone. We conclude that the precipitating characteristics of antibodies do not affect their ability to deposit in kidney.(ABSTRACT TRUNCATED AT 250 WORDS)

Animals↗

PubMed2003

Mercury and trace elements in cloud water and precipitation collected on Mt. Mansfield, Vermont.

The lack of high quality measurements of Hg and trace elements in cloud and fog water led to the design of a new collector for clean sequential sampling of cloud and fog water. Cloud water was collected during nine non-precipitating cloud events on Mt. Mansfield, VT in the northeastern USA between August 1 and October 31, 1998. Sequential samples were collected during six of these events. Mercury cloud water concentrations ranged from 7.5 to 71.8 ng l(-1), with a mean of 24.8 ng l(-1). Liquid water content explained about 60% of the variability in Hg cloud concentrations. Highest Hg cloud water concentrations were found to be associated with transport from the Mid-Atlantic and Ohio River Valley, and lowest concentrations with transport from the north of Mt. Mansfield out of Canada. Twenty-nine event precipitation samples were collected during the ten-week cloud sampling period near the base of Mt. Mansfield as part of a long-term deposition study. The Hg concentrations of cloud water were similar to, but higher on average (median of 12.5 ng l(-1)) than Hg precipitation concentrations (median of 10.5 ng l(-1)). Cloud and precipitation samples were analyzed for fifteen trace elements including Mg, Cu, Zn, As, Cd and Pb by ICP-MS. Mean concentrations were higher in cloud water than precipitation for elements with predominately anthropogenic, but not crustal origin in samples from the same source region. One possible explanation is greater in-cloud scavenging of crustal elements in precipitating than non-precipitating clouds, and greater below-cloud scavenging of crustal than anthropogenic aerosols.

Air Pollutants↗

PubMed2005

Precipitation in light extinction reconstruction.

The U.S. Environmental Protection Agency (EPA) published the Regional Haze Rule (RHR) in 1999. The RHR default goal is to reduce haze linearly to natural background in 2064 from the baseline period of 2000-2004. The EPA default method for estimating natural and baseline visibility uses the Interagency Monitoring of Protected Visual Environments (IMPROVE) formula. The IMPROVE formula predicts the light extinction coefficient from aerosol chemical concentrations measured by the IMPROVE network. The IMPROVE light scattering coefficient formula using data from 1994-2002 underestimated the measured light scattering coefficient by 700 Mm(-1), on average, on days with precipitation. Also, precipitation occurred as often on the clearest as haziest days. This led to estimating the light extinction coefficient of precipitation, averaged over all days, as the light scattering coefficient on days with precipitation (700 Mm(-1)) multiplied by the percent of precipitation days in a year. This estimate added to the IMPROVE formula light extinction estimate gives a real world estimate of visibility for the 20% clearest, 20% haziest, and all days. For example, in 1993, the EPAs Report to Congress projected visibility in Class I areas would improve by 3 deciviews by 2010 across the haziest portions of the eastern United States because of the 1990 Clean Air Act Amendments. Omitted was the light extinction coefficient of precipitation. Adding in the estimated light extinction coefficient of precipitation, the estimated visibility improvement declines to <1 deciview.

Air Pollutants↗

PubMed2002

Precipitation of swine and cattle manure phosphorous using limestone dust.

The effectiveness of SPS and PULPRO, fine limestone dusts, in precipitating swine and dairy manure phosphorous (P) was determined in the laboratory. Both manures were sieved before being treated with limestone, to reproduce the treatment of mechanically separated manure and to observe the precipitation effect of limestone without that of the large manure solid particles. P precipitation was optimized by varying precipitation conditions (propeller blade speeds, mixing time and limestone levels) and limestone particle size. P precipitation was optimized using a propeller blade mixing speed of 0.3 m s(-1) for at least 5 minutes, using 3% limestone (dry limestone mass over wet manure mass). In terms of particle size, PULPRO 20 (limestone with a particle size of 0.02 mm) produced the most P precipitation and the smallest volume and mass of sludge, as compared to PULPRO 10, PULPRO 3 and SPS (limestone with a particle size of 0.01, 0.003 and 0.3 to 0.003 mm, respectively). For both 9.5% TS (total solids) dairy and 8.8% TS swine manure, mechanical separation followed by limestone precipitation concentrated 90% of manure TS and TP in a sludge volume representing 45% of the initial raw manure mass.

Animals↗

PubMed2002

Luminescence intensity in coral skeletons from Mona Island in the Caribbean Sea and its link to precipitation and wind speed.

This study investigates the potential of using changes of interannual luminescence intensity in hermatypic Montastraea coral skeletons in the northeastern Caribbean as a proxy of precipitation and (trade) wind speed. In order to find wavelength pairs that are well suited to detect variations in the concentration of incorporated terrestrial humic substances in coral skeletons, and thus to reconstruct past run-off and rainfall, three-dimensional excitation-emission matrix fluorescence spectra of seawater samples were investigated on their relationships to local precipitation. Three prominent excitation-emission peaks at 310/430, 425/480 and 390/530 nm were identified. The fluorescence intensities of the wavelength pair 310/430 nm showed a weak relationship, while the wavelength pairs at 425/480 and 390/530 nm showed strong relationships with local precipitation. Variations in luminescence intensities from scans on the coral surface along the growth axis using the wavelengths identified were then compared with instrumental records of regional precipitation and wind speed. In the coral skeleton as well, the wavelength pairs at 425/480 and 390/530 nm were more strongly correlated with regional precipitation and wind speed. This indicates that these two wavelength pairs are well suited to reconstruct past precipitation and wind speed. In order to evaluate the use as a proxy of trade wind variability in the Caribbean, tropical Atlantic region, variations in luminescence intensity were compared with a record of trade wind variability from the southern Caribbean. The two records are strongly correlated, which suggests that luminescence intensity in coral skeletons, at least from Mona Island, can be used as proxy of trade wind variability and precipitation.

Anthozoa↗

PubMed1967

Copper sulfide precipitation by yeasts from Acid mine-waters.

Two strains of Rhodotorula and one of Trichosporon precipitated dissolved copper with H(2)S formed by reducing elemental sulfur with glucose. Iron stimulated this activity under certain conditions. In the case of Rhodotorula strain L, iron stimulated copper precipitation aerobically at a copper concentration of 18 but not 180 mug/ml. Anaerobically, the L strain required iron for precipitation of copper from a medium with 180 mug of copper per ml. Rhodotorula strain L was able to precipitate about five times as much copper anaerobically as aerobically. The precipitated copper was identified as copper sulfide, but its exact composition could not be ascertained. Iron was not precipitated by the H(2)S formed by any of the yeasts. Added as ferric iron, it was able to redissolve copper sulfide formed aerobically by Rhodotorula strain L from 18 but not 180 mug of copper per ml of medium. Since the yeasts were derived from acid mine-waters, their ability to precipitate copper may be of geomicrobial importance.

Journal Article↗

PubMed1999

A precipitation reaction found in patients with hepatitis C as a marker for the purification of virus-like particles.

Even after the molecular cloning of the hepatitis C virus (HCV), an HCV-specific precipitation reaction has not yet been identified. We attempted to develop a precipitation system exclusively for anti-HCV-positive sera as a first step in finding an HCV-specific antigen and HCV-associated particles. In some patients being in a final stage of different liver diseases, we found sera (179/132,761; designated 'a-CK') which specifically precipitated with anti-HCV- and HCV-RNA-positive sera (designated 'CK'). When CK-positive sera were searched for in patients with various liver diseases using standard a-CK-positive plasma, CK was detected in 420 (57.9%) of 726 anti-HCV-positive sera and in none of the 1,630 anti-HCV-negative ones. The nature of CK and a-CK has not been fully clarified yet; CK demonstrated inter-betagamma mobility, whereas a-CK showed beta-globulin mobility; CK was not detected in cryoprecipitate, but HCV RNA was present in precipitates of CK-positive plasma incubated with one that was a-CK positive. Transmission electron microscopy revealed two size ranges of particles in the precipitate of CK- and a-CK-positive plasmas, 23-38 nm and 48-65 nm. We have found a novel precipitation system which is exclusive to anti-HCV-positive sera and which specifically precipitates an HCV-RNA-containing serum fraction and particles. This system can be useful for the purification and characterization of the circulating particles. Furthermore, it may be a new approach to the nature of HCV-RNA-carrying material.

Centrifugation↗

PubMed1988

C4-mediated inhibition of immune precipitation and differences in inhibitory action of genetic variants, C4A3 and C4B1.

The inhibition of immune precipitation is mediated by the classical complement pathway. We report here that the rate of precipitate formation depends on the genetic form of human C4 present during immune precipitation. C4A3 is more effective than C4B1 in its capacity to inhibit the rate of immune precipitate formation in serum and in serum-free reaction mixtures containing C1 and C4. Immune precipitates form within seconds after antigen is mixed with antibody, and the activation of the classical pathway is known to occur within seconds after C1 binds to antibody molecules. The covalent deposition of C4b on immune complexes is an essential step in the inhibition of immune precipitate formation, and if any of the reactions that lead to covalent C4b deposition become limiting, the rate of immune precipitation could exceed the complement system's inhibitory capacity. Hence, the inhibition of this rate may be an important function underlying the complement-mediated processing of immune complexes, and a decreased ability of the complement system to mediate this process in the presence of C4B1, in contrast to C4A3, could explain, at least in part, the association between the C4A-null phenotype and autoimmune diseases such as systemic lupus erythematosus.

Animals↗

PubMed1977

Interactions among heparin, cold-insoluble globulin, and fibrinogen in formation of the heparin-precipitable fraction of plasma.

Fibrinogen and the cold-insoluble globulin of plasma (CIg) are the main protein components of the heparin-precipitable fraction of normal plasma. The interactions among these proteins and heparin were examined. Heparin formed a cold-precipitable complex with purified CIg or with mixtures of CIg and fibrinogen but not with purified fibrinogen alone. Cryoprecipitation was augmented by addition of Ca(++) or by selection of optimal heparin levels; it was reduced or even abolished by raising the ionic strength or pH or both, or by raising the heparin concentration above that for maximum precipitation of CIg. Fibrinogen reduced the threshold for heparin-induced CIg cryoprecipitation and, by coprecipitating with heparin and CIg, increased the amount of precipitate that formed. In contrast to the heparin-precipitable fraction of normal plasma which contained both fibrinogen and CIg, that from a patient with congenital afibrinogenemia contained CIg but lacked fibrinogen. Normal plasma depleted of CIg by immunoabsorption failed to form a heparin-induced cryoprecipitate. Thus, CIg is essential for heparin-induced cryoprecipitation to occur. Fibrinogen, as assessed by chromatographic experiments with heparin-Sepharose columns, had a considerably lower binding affinity for heparin than did CIg, suggesting that it participates in precipitate formation mainly, if not entirely, by virtue of its affinity for CIg. The region of the fibrinogen molecule accounting for its precipitation with CIg appears to be localized in the carboxy-terminal segment of the Aalpha-chain; fibrinogen subfractions lacking this region failed to augment cryoprecipitation of heparin-CIg mixtures and, even though such species were present in normal plasma, they failed to coprecipitate in the heparin-induced complex.

Calcium↗

PubMed1995

Effects of fluoride on the calcium phosphate precipitation method for dentinal tubule occlusion.

Use of the calcium phosphate precipitation (CPP) method makes possible the occlusion of dentinal tubules to approximately 10 to 15 microns from the dentinal surface, and thus shows good potential for the treatment of dentin hypersensitivity. The precipitate formed in the dentinal tubules by the CPP method is, however, not apatite [HAP; Ca10(PO4)6(OH)2], a component of tooth and bone, but dicalcium phosphate dihydrate (DCPD; CaHPO4.2H2O). Since fluoride enhances the conversion of DCPD to HAP, we evaluated the effects of fluoride on the texture of the precipitate formed by the CPP method and on its capacity to occlude dentinal tubules in this in vitro study. CPP solution (1.0 mol/L CaHPO4.2H2O dissolved in 2.0 mol/L H3PO4) was applied to a dentin disk and was subsequently neutralized with a post-treatment solution (1 mol/L NaOH, from 0 to 0.1 mol/L NaF). Scanning electron microscopy revealed that the precipitate occluded dentinal tubules to a depth of approximately 10 to 15 microns from the dentinal surface, regardless of the NaF concentration (from 0 to 0.1 mol/L) in the post-treatment solution. Also, dentin permeability was reduced to 15% by the CPP treatment regardless of the NaF concentration. The Ca/P molar ratio of the precipitate, measured by x-ray micro-analysis, was higher (1.25 +/- 0.04) in the presence of NaF than in its absence (1.03 +/- 0.01). For further identification of the precipitate formed in the dentinal tubules, the same procedure was used in glass tubes (diameter, 1 mm), so that a larger amount of precipitate would be obtained.(ABSTRACT TRUNCATED AT 250 WORDS)

Calcium Phosphates↗

PubMed1999

Modification of the expression of naloxone-precipitated withdrawal signs in morphine-dependent mice by diabetes: possible involvement of protein kinase C.

The involvement of cyclic AMP-dependent protein kinase (PKA) and protein kinase C (PKC) in the modulation of naloxone-precipitated withdrawal jumping in morphine-dependent mice by diabetes was examined. Naloxone-precipitated withdrawal jumps were significantly less in morphine-dependent diabetic mice than in morphine-dependent non-diabetic mice. I.c.v. pretreatment with either calphostin C, a PKC inhibitor, or KT-5720, a PKA inhibitor, attenuated naloxone-precipitated withdrawal jumps in morphine-dependent non-diabetic mice. However, naloxone-precipitated withdrawal jumps in morphine-dependent diabetic mice were not attenuated by i.c.v. pretreatment with either calphostin C or KT5720. Moreover, i.c.v. pretreatment with phorbol-12,13-dibutyrate (PDBu), a PKC activator, attenuated naloxone-precipitated withdrawal jumps in morphine-dependent non-diabetic mice, but not in morphine-dependent diabetic mice. The noradrenaline (NA) turnover in the frontal cortex in morphine-dependent non-diabetic mice, but not in morphine-dependent diabetic mice, was significantly increased 5 min after administration of naloxone. Naloxone-induced enhancement of NA turnover in morphine-dependent non-diabetic mice, but not in morphine-dependent diabetic mice, was blocked by i.c.v. pretreatment with either calphostin C or KT5720 1 hr before naloxone challenge and blocked by PDBu 1 hr before the last injection of morphine. These results suggest that the co-activation of PKC and PKA is needed to elicit naloxone-precipitated withdrawal jumps and enhancement of turnover rate of NA in the frontal cortex in morphine-dependent non-diabetic mice. Furthermore, the attenuation of naloxone-precipitated withdrawal jumps in morphine-dependent diabetic mice may be due, in part, to the desensitization of mu-opioid receptors by the activation of PKC.

Animals↗

PubMed2003

Effects of LDL, cholesterol, and their oxidized forms on the precipitation kinetics of calcium phosphates.

BACKGROUND: LDL, cholesterol, and their oxidized forms are known cardiovascular risk factors and are often found in atherosclerotic lesions of various stages. Little is known, however, about whether they are directly involved in the formation of calcium phosphate compounds. METHODS: We used the pH-stat technique to follow the kinetics of calcium phosphate precipitation at pH 7.4, 37 degrees C, and ionic strength 0.150 mol/L, in the presence or absence of LDL, oxidized LDL, cholesterol, cholestane-3beta,5alpha,6beta-triol, and cholesteryl linoleate. The precipitates were characterized by x-ray diffraction, scanning and transmission electronic microscopy coupled with energy-dispersion x-ray analysis, and inductively coupled plasma atomic emission spectroscopy. RESULTS: Under the experimental conditions, LDL (14.8 and 43.1 mg/L protein) had no significant effect on the precipitation kinetics. Oxidized LDL (14.8 and 43.1 mg/L protein) prolonged the nucleation phase and diminished the amount of total precipitate, and both the extent of oxidation and the concentration of the protein affected the kinetics. Cholesterol microcrystals (71.4 and 143 mg/L) made the nucleation phase shorter (300 min vs 390 min for the control), and the precipitated particles had an organic core and a shell composed of calcium phosphates. L-alpha-Phosphatidylcholine vesicles (143 mg/L), cholesterol (71.4 mg/L)/phospholipid (143 mg/L) mixed vesicles, cholesteryl linoleate (143 mg/L), and cholestane-3beta,5alpha,6beta-triol (71.4 mg/L) prolonged the nucleation phase. CONCLUSIONS: LDL is not involved directly in the precipitation of calcium phosphates. Oxidized LDL inhibits both nucleation and crystal growth, possibly by attracting calcium ions in the solution and thus reducing supersaturation. Cholesterol microcrystals serve as seeds for the precipitation of hydroxyapatite, whereas L-alpha-phosphatidylcholine, cholesteryl linoleate, and cholestane-3beta,5alpha,6beta-triol exhibit inhibitive effects on the nucleation of calcium phosphates.

Calcium Phosphates↗

PubMed1984

Precipitation of LDL with sulphopolyanions: a comparison of two methods for LDL cholesterol determination.

Two commercially available tests for the determination of LDL cholesterol were compared. The determination principle lies in the precipitation of LDL using heparin (Merck, Darmstadt test) or using polycyclic surface activated anions (bioMérieux test), as well as ascertaining LDL cholesterol by subtracting cholesterol in the supernatant from total cholesterol (Merck, Darmstadt test) or the direct determination of cholesterol in the redissolved precipitate (bioMérieux test). Regression analysis of the LDL cholesterol values obtained by precipitation and the LDL cholesterol values obtained by the combination of ultracentrifugation and HDL cholesterol determination (cholesterol in the d greater than 1.006 kg/l ultracentrifugation fraction- HDL cholesterol) resulted in a good correlation (precipitation using polycyclic surface activated anions: r = 0.95, y = 1.01x - 0.14, n = 34; heparin precipitation: r = 0.94, y = 0.86x + 0.10, n = 28). In sera containing triglycerides ranging from 2.28 mmol/l to 10.9 mmol/l there was an adequate agreement between the values obtained by precipitation with polycyclic surface activated anions and those of the reference method (r = 0.94, y = 0.9x + 0.47, n = 51), whereas the data obtained by heparin precipitation clearly deviated from the data of the reference method (r = 0.69, y = 0.75x + 0.003, n = 32).

Anions↗