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Silicic acid

Silicic acid, a crucial inorganic compound, plays a pivotal role in a wide range of biological and industrial processes.
This silicon-containing acid is involved in the formation of silica and silicate minerals, and is also found in various living organisms, including plants and some marine invertebrates.
Silicic acid has a complex chemistry, with multiple forms and the ability to polymerize, making it an important subject of study in fields such as materials science, geology, and biochemistry.
Researchers utilize a variety of protocols and techniques to investigate the properties and applications of silicic acid, and the PubCompare.ai platform can help optimize these research efforts by providing intelligent comparisons and guiding users to the best available protocols from literature, preprints, and patents.
By leveraging this innovative software, scientists can enhance the reproducibility and efficiency of their silicic acid research, driving their work forward with greater confidence and impact.

Most cited protocols related to «Silicic acid»

The Dashboard is a component of the Pathway Tools software (8 (link)). Pathway Tools powers the BioCyc website, and Pathway Tools is used to construct the organism-specific databases, called Pathway/Genome Databases (PGDBs), that make up the BioCyc database collection. The panel and plot visualizations within the Dashboard are implemented using Google Charts https://developers.google.com/chart/, which in turn is implemented in Javascript. The Dashboard also contains client-side (web browser) components implemented in Javascript, and server-side components implemented in Common Lisp. The pathway and operon diagrams displayed by the Dashboard are generated by existing Pathway Tools algorithms, as is the enrichment analysis operation within the Dashboard.
The Dashboard software defines a mapping from each subsystem (plot) to one or more pathways and/or GO terms. When the Dashboard displays each plot, it dynamically retrieves gene or metabolite lists for each plot from the PGDB for the current organism. For example, it issues PGDB queries to determine what genes (if any) exist in the current organism for the pathway(s) or GO term(s) associated with each plot. More specifically, Dashboard-panel gene groups are obtained from pathways in the PGDB via a Pathway Tools built-in query that returns all genes coding for enzymes catalyzing reactions within a specified metabolic pathway. Similarly, Pathway Tools provides a built-in query for obtaining all genes annotated to a given GO term. When displaying the window of regulators, the Dashboard issues a built-in Pathway Tools query for obtaining a list of all transcriptional regulators of a given gene.
PGDBs within the BioCyc collection are highly variable in terms of the completeness of their GO term annotations and regulatory interactions, but the Dashboard is best suited for use with PGDBs with significant numbers of GO terms and regulatory interactions. Table 1 lists the 16 BioCyc databases containing more than 3000 GO term annotations, and the 10 BioCyc databases containing more than 500 transcriptional regulatory interactions. For our next BioCyc release in 2017 we have downloaded available GO term annotations from UniProt for all of the 42 Tier 2 BioCyc PGDBs (Tier 2 PGDBs have undergone a moderate amount of manual curation). GO annotations will be available for even more organisms in the future.
Given a set of genes (the user could specify all genes, or a set of genes whose changes are computed to be statistically significant), the Dashboard computes an enrichment p-value for every subsystem using a Lisp implementation of Grossmann’s parent–child-union analysis, a variation of the Fisher-exact test in which the enrichment of a given subsystem is determined relative to its parent subsystem rather than to the entire population (10 (link)). An optional multiple-hypothesis correction (options are Bonferroni, Benjamini-Hochberg or Benjamini-Yekutieli corrections, with no correction being the default) may be applied. The enrichment p-value is then converted to an enrichment score, −log(P-value).
Experimental designs that the Dashboard should be appropriate for include time-course experiments, dose-response experiments, and experiments that vary growth conditions. The Dashboard performs well up to 20 columns of data, but the display becomes cramped; that effect will be lessened on larger monitors.
This paper uses the analysis of two datasets to illustrate the application of the Dashboard toolset: a genome-wide transcriptome analysis of Thalassiosira pseudonana, and an E. coli gene-expression analysis of a 10 min time course following a shift from anaerobic to aerobic growth conditions.
Mock et al. performed a genome-wide transcriptome analysis on T. pseudonana strain CCMP 1335 under five different environmental conditions: low nitrate (low N), low silicic acid (low Si), low iron (Low Fe), low temperature (4°C) and high pH (9.4), with nutrient-replete cultures serving as reference conditions (11 (link)). Cultures were maintained in natural seawater that had been autoclaved and supplemented with 2 × f/2 nutrients minus one of the limited nutrient (Si, Fe or N) at 20°C and 100 μmol of photons m−2s−1. F/2 provides the major nutrients including N, Si and P, as well as trace metals and vitamins (12 (link)). Alkaline pH condition was obtained by increasing the pH of 2 × f/2 seawater to 9.4 by adding 1M NaOH. Temperature limitation was achieved by transferring a culture maintained in nutrient-replete 2 ×f/2 seawater at 20°C to 4°C for 24 h (11 (link)). All limitation experiments were conducted in parallel with nutrient-replete cultures. Cells were harvested for RNA when the growth rate began to decrease significantly relative to the control cultures. Differentially expressed genes include those that have a Bayesian t-test P-value ≤ 0.05, and a ≥2-fold difference in mRNA levels with respect to the control samples. Data are available under GEO accession GSE9697.
Methods from von Wulffen et al. (13 ): Escherichia coli K–12 strain W3110 was used in this study. Cells were grown anaerobically in defined medium at pH7 and 37°C in a stirred 3-l bio-reactor until the culture reached an OD (600 nm) of 3. At that point, the first three replicate samples were drawn and aeration was started subsequently at 1 l/min. At 0.5, 1, 2, 5 and 10 min after the onset of aeration additional samples were drawn from the three replicates.
Analysis of von Wulffen et al. data performed for this publication: raw gene counts were obtained from the GEO database (accession GSE71562). Replicates were averaged and were next normalized using the TPM (Transcripts per Kilobase Million) approach (14 (link)). Genes that had zero counts in more than 15% of the samples were removed from further analysis; in addition, two genes (ssrA and rnpB) with high expression values that compressed the scales of two panels were removed; see Supplementary File S1. Differentially expressed genes in the samples at 0.5, 1, 2, 5 and 10 minutes were identified with respect to zero time samples by applying a paired T.TEST analysis (computed with Excel). Samples with statistically significant changes (P-value ≤ 0.05) and at least a 2-fold increase or decrease in gene expression (for any time point relative to time zero) were retained; see Supplementary File S2. At 0.5 min, 33 genes were found to be differentially expressed versus 487 at 10 min in aerobic growth. Over the 10-min period 639 genes were identified as significantly differentially expressed; their read counts summed to 12% of the total normalized read counts.
Publication 2017
Bacteria, Aerobic Cells Child Cold Temperature DNA Replication Enzymes Escherichia coli Gene Expression Gene Expression Profiling Genes Genes, vif Genome Growth Disorders Iron Metals Nitrates Nutrients Operon Parent RNA, Messenger Silicic acid Strains tmRNA Transcription, Genetic Vitamins
We use the global coupled physical‐biogeochemical model NEMO/PISCES (Aumont et al., 2015 (link)), which represents nitrate, ammonium, phosphate, silicic acid and dissolved iron cycling, the full carbon and oxygen systems, two phytoplankton groups (nanophytoplankton and diatoms) and two zooplankton size classes (microzooplankton and mesozooplankton) and has been extensively used to study regional and global ocean biogeochemistry (e.g. Aumont et al., 2017 (link); Gorgues et al., 2019 (link); Kwiatkowski, Aumont, Bopp, & Ciais, 2018 (link); Richon et al., 2017 (link); Tagliabue & Resing, 2016 (link)). Recent developments of the PISCES model have included micronutrient cycling such as Cu (Richon & Tagliabue, 2019 (link)), Zn, Co (Tagliabue et al., 2018 (link)) and Mn to build a new version of the model called PISCES‐BYONIC. The model is fully described and evaluated in supplement (Text S1). We present here the key information on the model.
In the standard version of PISCES‐BYONIC, the phytoplankton macronutrient stoichiometry (C:N:P) is fixed, but it is variable for micronutrients (Fe, Co, Cu, Mn and Zn), chlorophyll and silica. The maximum micronutrient:C molar quotas are 80E‐6 for Fe, 40 and 123 for Zn in nanophytoplankton and diatoms, respectively, 16E‐6 for Cu, 1.2E‐6 for Co and 8E‐6 for Mn, which broadly reflects available observational constraints (e.g. Twining & Baines, 2013 (link); Twining et al., 2015 (link)). The zooplankton molar micronutrient to carbon stoichiometry is fixed to 10E‐6 for Fe, Zn and Cu, and to 0.16E‐6 and 1E‐6 for Co and Mn, respectively, following the more limited observational understanding (see Baines et al., 2016 (link); Ratnarajah et al., 2014 (link); Twining & Baines, 2013 (link)).
The impacts of climate change on micronutrient recycling and recycling stoichiometry were simulated using offline physical fields from the IPSL‐CM5A climate model, as in previous work (Kwiatkowski, Aumont, Bopp, & Ciais, 2018 (link); Tagliabue et al., 2020 (link)). We performed two simulations: a preindustrial control (PICONTROL) from 1801 to 2100 with atmospheric CO2 concentrations fixed to the preindustrial value. Then, from 1851 to 2100, we performed a second simulation initialized from year 1851 of the PICONTROL, with CO2 concentrations varying according to the historical pathway until 2005 and switching to the high emissions RCP8.5 scenario (Riahi et al., 2011 (link)) from 2006 to 2100. Previous studies using NEMO/PISCES under the RCP8.5 scenario showed a global increase in stratification, increased SST and decrease in surface macronutrients leading to changes in plankton distribution and stoichiometry (Kwiatkowski, Aumont, & Bopp, 2018 (link); Kwiatkowski, Aumont, Bopp, & Ciais, 2018 (link)).
For our simulations, we use constant external nutrient sources (hydrothermal vents, rivers and aerosols). Sedimentary sources of Co and Mn are O2 dependent (Tagliabue et al., 2018 (link)). To assess our results, we define two periods of time: PRESENT (model results averaged over 1991–2000) and FUTURE (model results averaged over 2091–2100). Previous work with this model has shown that microzooplankton recycling accounts for most of micronutrient recycling fluxes (see Richon et al., 2020 (link)); therefore, we focus here on microzooplankton.
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Publication 2021
3-(2-iodoacetamido)-2,2,5,5-tetramethyl-1-pyrrolidinyloxyl Aerosols Ammonium Carbon Chlorophyll Climate Change Diatoms Dietary Supplements Fishes Hydrothermal Vents Iron Macronutrient Micronutrients Molar Nitrates Nutrients Phosphates Physical Examination Phytoplankton Plankton Rivers Silicic acid Silicon Dioxide Trace Elements Zooplankton
Prior
to deployment, PUF were cleaned (24 h, Soxhlet apparatus) with a 1:1
(v/v) hexane/acetone mixture and wrapped in aluminum foil within ZipLok
bags for storage and transport. Those PUFs ready for deployment were
installed in PAS housing and subsequently retrieved by trained field
staff. Resulting PUF samples were spiked with surrogate standards
(50 ng each of PCB 14, deuterated-65, and 166), extracted with the
same hexane/acetone mixture (Accelerated Solvent Extractor, Dionex
ASE-300), cleaned through a column of silicic acid, and concentrated,
as described by Persoon and Hornbuckle.31 (link) Laboratory blanks and field blanks were included at a 10% rate and
treated the same as samples. Finally, after addition of internal standards
(20 ng each of deuterated-PCB 30 and 204), samples were analyzed by
gas chromatography with tandem mass spectrometry (GC-MS/MS, Agilent
6890N Quattro Micro GC, Waters Micromass MS Technologies) in multiple
reaction monitoring mode, using a method derived from EPA Method 1668c,
but substantially modified for analysis with the aforementioned instruments.33 Transition ions were selected for each homologue
group allowing greater separation of congeners from each other and
from background noise than possible using electron capture detection.
We used a 60m Supelco SPB-Octyl capillary column for chromatographic
separation to isolate most of the dioxin-like congeners. We were able
to quantify 201 congeners as a set of 156 individual or coeluting
chromatographic peaks. Further details of this method are described
elsewhere (Supporting Information (SI)).31 (link),33 Deuterated standards were obtained from CDN Isotopes (Quebec, Canada),
and nondeuterated standards from AccuStandard (New Haven, USA).
Publication 2014
Acetone Aluminum Capillaries Chromatography Electrons Ions Isotopes n-hexane Silicic acid Solvents Tandem Mass Spectrometry Tetrachlorodibenzodioxin
Autoclaving of natural seawater (collected off Santa Barbara 34° 23′ N 119° 50′ W) for media preparation was not an option since the carbonate chemistry of seawater is severely impacted by de-gassing. The pH of freshly collected natural seawater from the Santa Barbara Channel increased from 7.58 to 8.67 during autoclaving. Stirring the autoclaved seawater while leaving the beaker open to the atmosphere only reduced the pH to 7.89 (Table 2). The repeated filtration of natural seawater through 0.2 µm pore-sized filters (Millipore, MA, USA) did not satisfactorily remove all bacterial contaminants. We therefore opted for the use of artificial seawater (ASW) [32] for media preparation. Using ASW imparts the added benefit of easily and precisely manipulating DIC concentrations. ASW was prepared with a DIC concentration of 2,050 µmol kg−1 for ambient treatments and supplemented with vitamins and trace metal solutions as in F/2 medium [33] . Macronutrients were added to a final concentration of 59 µM nitrate, 3.6 µM phosphate and 53.5 µM silicic acid to create ASW-media. The carbonate chemistry of future treatments was adjusted as described below.
Diatom cells were counted in a Sedgwick-Rafter Cell S50 (SPI Supplies, West Chester, PA, USA) using an inverted Axiovert 200 microscope (Zeiss, Jena, Germany). The axenicity of the diatom culture was checked by epifluorescence microscopy [34] after staining with the dye 4′, 6-diamidino-2-phenylindol (DAPI) [35] .
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Publication 2014
Atmosphere Bacteria Carbonates Cells Diatoms Filtration Macronutrient Metals Microscopy Nitrates Phosphates Silicic acid Vitamins
The diatom strain Thalassiosira weissflogii (Grun.) Fryxell and Hasle was obtained from the Provasoli-Guillard National Center for Culture of Marine Phytoplankton (CCMP-1051). Axenic cells were cultured in batch at low cell density (from 2×104 to 3×105 cells mL−1) in an artificial sea water medium (for details about the medium preparation see [23] (link)), under a 12∶12 hr light-dark cycle with a light intensity of ca. 100 μEinstein m−2 s−1 (ca. 7,000 Lux), and at 19°C. After sterilization, the artificial sea water medium was completed by adding 175 µM silicic acid (a non-limiting concentration), dipotassium hydrogen orthophosphate and vitamins. The pH of the medium was adjusted to the expected value, using sterile 0.2 M HCl or 0.2 M NaOH, prior to and after sterilization. To measure the different parameters, including the kinetics of valve formation, T. weissflogii cells were first acclimated to the appropriate medium for 3 to 6 days, to ensure that the cells were in exponential growth phase. For each experiment, duplicated growth rate measurements were performed from independent cultures, and all conditions were cultured in parallel. Algal cell density was determined by flow cytometry counting.
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Publication 2012
Cells Diatoms Flow Cytometry Kinetics Phytoplankton potassium phosphate, dibasic Silicic acid Sterility, Reproductive Sterilization Strains T-Lymphocyte Vitamins

Most recents protocols related to «Silicic acid»

Example 10

    • 6 months oral administration of 10 mg of bioavailable silicic acid per day in the form of choline-stabilized orthosilicic acid (ch-OSA®), wherein silicic acid is stabilized with choline chloride; preferably in the form of two dosage units, such as tablets
    • Local application of an ethylene/vinyl acetate copolymer fiber that contains tetracycline (12.7 mg per 9 inches) in the affected periodontal pocket for 10 days.
    • mouth rinsing with chlorhexidine 1% solution twice daily during 4 weeks.

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Patent 2024
Acids Administration, Oral Aggressive Periodontitis Chlorhexidine Choline Choline Chloride Dosage Forms ethylenevinylacetate copolymer Fibrosis Oral Cavity Periodontal Pocket Silicic acid Tetracycline

Example 5

    • Daily oral administration of 5 mg of bioavailable silicic acid in the form of choline-stabilized orthosilicic acid (ch-OSA®), wherein silicic acid is stabilized with choline chloride, for instance in the form of a capsule.
    • Daily administration of a tablet containing 200 mg vitamin C, 150 microgram selenium, 10 mg zinc, 1 mg copper.

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Patent 2024
Acids Administration, Oral Ascorbic Acid Capsule Choline Choline Chloride Copper Periodontitis Selenium Silicic acid Tablet Zinc

Example 4

A female peri-implantitis patient, 66 years old and non-smoker, had severe bone loss at two implant sites (as shown in FIG. 4A). The patient took during one year 5 drops of BioSil® liquid twice daily. This formulation contains choline-stabilized orthosilicic acid (ch-OSA®), wherein silicic acid is stabilized with choline chloride. The formulation furthermore contains glycerol as a diluent. After one year the bone level was significantly increased at the implant site (see FIG. 4B).

A second peri-implantitis patient, 73 years and non-smoker, with severe bone loss at the implant sites and damaged gingiva (FIG. 5a) took during one year 5 drops of BioSil® liquid twice daily. After one year the bone level was also significantly increased at the implant site (FIG. 5b, after 6 months, FIG. 5c, after 12 months). FIG. 6 shows that the gingiva regained its normal appearance with good color indicating improved vascularization in the course of the 1 year treatment.

The following treatment examples can be used as an adjunct to good mouth hygiene, scaling and root planing:

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Patent 2024
Acids Biosil Bones Choline Choline Chloride Gingiva Glycerin Non-Smokers Osteopenia Pathologic Neovascularization Patients Peri-Implantitis Periodontitis Silicic acid Woman
Not available on PMC !

Example 7

    • Initial full mouth one-stage disinfection by rinsing for 2 minutes with a 0.12% chlorhexidine solution.
    • 6 months oral administration of 10 mg of bioavailable silicic acid in the form of choline-stabilized orthosilicic acid (ch-OSA®), wherein silicic acid is stabilized with choline chloride, suitably in the form of two dosage units each containing 5 mg bioavailable silicic acid;
    • Daily administration of two probiotic lozenges, each containing 2 viable strains of Lactobacillus reuteri (1 108 CFU), for instance DSM17938 and ATCC PTA5289, during 6 months.

It is herein preferable, that the administration of the bioavailable silicic acid and the administration of the probiotic lozenges start simultaneously. Alternatively, the administration of the bioavailable silicic acid may precede the administration of the probiotic lozenges during a preparatory period of for instance 3 days up to 14 days, for instance 1 week.

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Patent 2024
Acids Administration, Oral Chlorhexidine Choline Choline Chloride Disinfection Dosage Forms Lactobacillus reuteri Periodontitis Probiotics Silicic acid Strains

Example 9

    • 6 months oral administration of 10 mg of bioavailable silicic acid per day, in the form of choline-stabilized orthosilicic acid (ch-OSA®), wherein silicic acid is stabilized with choline chloride, for instance in the form of 2 dosage units
    • combined oral administration of amoxicillin (250 mg three times daily) with metronidazole (250 mg three times daily) during 1 week and
    • Subgingival placement of 2.5 mg chlorhexidine gluconate in a hydrolyzed gelatin matrix chip (PerioChip). The chip degrades within 7-10 days.

It is herein preferable, that the administration of the bioavailable silicic acid and the administration of the antibiotic start simultaneously and concur with the subgingival placement. However, alternative protocols are not excluded.

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Patent 2024
Acids Administration, Oral Aggressive Periodontitis Amoxicillin Antibiotics chlorhexidine gluconate Choline Choline Chloride DNA Chips Dosage Forms Gelatins Metronidazole Silicic acid

Top products related to «Silicic acid»

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Silicic acid is a chemical compound with the formula H4SiO4. It is a white, crystalline solid that is soluble in water and other polar solvents. Silicic acid is a key component in various laboratory equipment and materials, where it serves as a fundamental building block for various silica-based products.
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Acetone is a clear, colorless, and volatile liquid organic compound. It is a common laboratory solvent used for a variety of purposes, such as cleaning and degreasing. Acetone has a high evaporation rate and is miscible with water, making it useful for various applications in scientific and industrial settings.
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HPLC-grade hexane is a high-purity solvent used as a mobile phase component in high-performance liquid chromatography (HPLC) applications. It is a colorless, volatile, and flammable liquid with a low boiling point. HPLC-grade hexane meets strict specifications for low levels of impurities, ensuring reliable and consistent chromatographic performance.
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Chloroform is a colorless, volatile, and dense liquid chemical compound. It is commonly used in scientific research and laboratory settings as a solvent for various organic compounds.
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Bis-[trimethylsilyl]-trifluoroacetamide (BSTFA) + 1 % trimethylchlorosilane (TMCS) is a reagent used in analytical chemistry. It is a silylating agent that is commonly used to derivatize organic compounds, such as alcohols and carboxylic acids, prior to analysis by gas chromatography-mass spectrometry (GC-MS).
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More about "Silicic acid"

Silicic acid, also known as silicic acid or orthosilicic acid, is a crucial inorganic compound that plays a pivotal role in a wide range of biological and industrial processes.
This silicon-containing acid is involved in the formation of silica and silicate minerals, and is also found in various living organisms, including plants and some marine invertebrates.
Silicic acid has a complex chemistry, with multiple forms and the ability to polymerize, making it an important subject of study in fields such as materials science, geology, and biochemistry.
Researchers often utilize techniques like GF/F filters, methanol, acetone, ethyl acetate, HPLC-grade hexane, chloroform, Bis-[trimethylsilyl]-trifluoroacetamide (BSTFA) + 1% trimethylchlorosilane (TMCS), and Celite 545 to investigate the properties and applications of silicic acid.
The PubCompare.ai platform can help optimize these research efforts by providing intelligent comparisons and guiding users to the best available protocols from literature, preprints, and patents.
By leveraging this innovative software, scientists can enhance the reproducibility and efficiency of their silicic acid research, driving their work forward with greater confidence and impact.
Additionally, the use of calcium phosphate (CaHPO4.2H2O) can be helpful in certain silicic acid-related studies.
By understanding the key aspects of silicic acid and the tools and techniques used to study it, researchers can unlock new insights and push the boundaries of this fascinatign field of study.