- Nano Express
- Open Access
Novel Crystalline SiO2 Nanoparticles via Annelids Bioprocessing of Agro-Industrial Wastes
© The Author(s) 2010
Received: 20 April 2009
Accepted: 17 May 2010
Published: 15 June 2010
The synthesis of nanoparticles silica oxide from rice husk, sugar cane bagasse and coffee husk, by employing vermicompost with annelids (Eisenia foetida) is reported. The product (humus) is calcinated and extracted to recover the crystalline nanoparticles. X-ray diffraction (XRD), transmission electron microscopy (TEM), high-resolution transmission electron microscopy (HRTEM) and dynamic light scattering (DLS) show that the biotransformation allows creating specific crystalline phases, since equivalent particles synthesized without biotransformation are bigger and with different crystalline structure.
Agro-industrial wastes have recently attracted a great deal of attention as potential sources of novel green alternatives such as biotransformation for fuels and other materials. Many of these wastes contain amorphous silica that can be transformed into crystalline nanoparticles of industrial interest.
Silicon is the most common element of the Earth’s surface after oxygen; this element is released into the soil by chemical and biological processes . Industrially speaking, silicon is the basis of semiconductors, glasses, ceramics, plastics, elastomers, resins, mesoporous molecular sieves and catalysts, optical fibers and coatings, insulators, moisture shields, photoluminescent polymers, fillers, cosmetics and biomedical devices [2, 3], among many other applications. The manufacture of these materials typically requires high temperatures, high pressure and/or the use of caustic chemicals . In contrast, in nature, silica architectures with delicate morphologies are generated under ambient conditions . Unicellular organisms, such as diatoms, use structuring and templating biomolecules to produce silica shells that not only contain hierarchically ordered porous structures, with dimensions ranging from the nanometer to the micrometer domain, but also possess remarkable mechanical and structural properties [6–8]. Other approach involves the use Fosuarium oxysporum, a plant pathogenic fungus for the biotransformation of naturally occurring amorphous plant bio-silica into quasi-spherical crystalline silica nanoparticles and its extracellular leaching in the aqueous environment at room temperature . An analysis suggested that extreme thermophilic bacteria within the genera thermus and hydrogenobacter are predominant components among the indigenous microbial community in siliceous deposits. These bacteria seem to actively contribute to the rapid formation of huge siliceous deposits .
In general, the biosilification products are commonly composed of amorphous silica (opal-A, opal-CT and opal-C), and other crystal arrays such as cristobalite, trydimite and quartz. In particular, amorphous silica is a dominant component in marine surface sediment most of which is considered to be generated by the activity of living organism [3, 11]. Many scientists not only investigate the process underlying their formation, but also aim to mimic these processes in order to obtain better control over the structure and morphology of chemically produced silica [12–14]. The natural silica production receives increasing attention, since it holds the key to the formation of silica morphologies with a dedicated organization of hierarchically structure elements and the ability to synthesize such silica under ambient conditions . There exist many studies in silica bio-mineralization of simple aquatic life forms, including unicellular organisms like diatoms, radiolaria and sinurophytes as multicellular sponges [16–19]. In the soil, silica plays a major role in higher plants . Many plants sequester silica in biogenic phytoliths and soils can accumulate significant quantities of biogenic opal-A . The silica absorbed for terrestrial plants is around a fraction of 1% of the dry matter to several percent, and in some plants to 10% or even higher . It is observed that in some grammineae as rice (Oryza sativa), silica constitutes 20–22% of its total production in the rice husk form . Sugarcane bagasse contains around 5.08 to 7.08% of silica in dry matter basis , and coffee husk contains around 1 to 3% of silica in dry matter basis .
It is important to mention that the mechanical strength of plants resides greatly on the cell wall, enabling them to achieve and maintain erect habit conductive to light interception. There exist a relation in plants stress and the increased rigidity of cell walls of plants grown with ample available silica [26, 27]. When plants die, the silica is reincorporated into the soil where microorganisms play an important role in the degradation of organic matter and in the release of minerals nutrients [28, 29], other important source that raises mineralization rate is earthworms producing biohumus. Humus contains principally carbon, oxygen, hydrogen and minor proportion of other minerals. These elements vary within the humic material in order to define chemical characteristics of the original basis. There exists a symbiotic interaction between earthworms and microorganisms that breakdown and fragment the organic matter progressively, finally incorporating it into water-stable aggregates. The mineral nutrients in earthworm casts and lining earthworm burrows are in a form readily available to plants. There is evidence that interactions between earthworms and microorganisms not only provide these available nutrients, but stimulate plant growth indirectly in others ways . The digestive system of earthworms consists of a pharynx, esophagus and gizzard (zone reception) followed by an anterior intestine that secrets enzymes and a posterior intestine that absorb nutrients. During progress through this digestive system, there is a dramatic increase in numbers of microorganism of up to 1,000 times. The digestive systems of earthworms from different species, genera and families differ in detail, but their gusts have a common basic structure. In different species earthworms Eisenia foetida is peculiar for its degradation rate . Most studies of digestive enzymes in earthworms have been limited to the lumbricids. Protease, lipase, amylase, lichenase, cellulose and chitinase activities also have been described . A wide range of microorganisms, including bacteria, algae, protozoa, actinomycetes, fungi and even nematodes, are found commonly throughout the length of the earthworms gut. The species of microbes in the gut are usually very similar to those in the surrounding soil or organic matter upon which the earthworms feed [32–34]. Eisenia foetida is considered a machine to produce humus in conditions environmental control and the microorganism can live in it in anoxic effect raising productivity in the material expel. The biological mechanism to earthworms transforms organic matter and even so carries out biosilification even is uncertain. Understanding the mechanism of silica nanofabrication in other organisms is supported by a precursor namely biosilica monosilicic acid Si(OH)4[35, 36]. Proteins have been isolated from diatoms, sponges and grasses that are proposed to be responsible for biosilification and have been sequenced and some of the key amino acids identified. Other authors have studied the role of homopolymers of various amino acids that are key constituents of the proteins lysine, histidine, arginine, cysteine, proline and serine in the process biosilification . This biopolymer acts as gelating agents of silica oligomers in silicic acid and as flocculation agents in silica sols [38, 39]. Other researches have been focused toward the development of efficient and innovative fabrication methods to obtain inorganic materials using microorganisms from potential cheap agro-industrial waste materials and could lead to an energy-conserving and economically viable green approach toward the large-scale synthesis of oxide nanomaterials . Thus, we develop a novel process for synthesis of diverse nanometric materials with specific crystal arrays as precursors to agro-industrial wastes employing annelids, an approach not used before, that permit to rise natural sources dedicated to production particles’ mean biosilification.
Three sources derived from agro-industrial activity were used: rice husk, coffee husk and sugarcane bagasse. These by-products were added to vermicompost separately. The annelid specimen used was Eisenia foetida. The environmental conditions ideal to the reproduction and control of these specimens were set up: temperature at 20°C, moisture around 60–85%, aeration conditions and darkness. The stabilization time was around 1 month and the humus obtained was dried in a room at a temperature between 30 and 40°C. Then, the humus was sieved to size 0.5 mm approximately. Next, the sample was calcinated to eliminate the organic matter. Three temperature levels were used: 500, 600 and 700°C for each agro-industrial waste by 19 h. Calcinations were carried out in a muffle Lindberg/Eurotherm model 847 with energy consumption of 0.17 kcal/h cm3, considering that the average density of the nanoparticles is around 0.1380 g/cm3, the consumed energy in the calcinations is approximately 1.2318 kcal/h by each gram of recuperated SiO2 particles. This energy could be considered low in comparison with other conventional process where fumed silica is manufactured with a consumed energy of until 15.48 kcal/h by each gram of SiO2 particles . Thus, the samples were tried with nitric and hydrochloric acids (volume ratio 3:1). For each gram of calcinated sample, 4 ml of acid mix was added in order to eliminate impurities (calcium, potassium, magnesium, manganese, iron, boron and phosphorous). Acid treatment was achieved at 40°C by 4 h with constant stirring. Then, samples were filtrated and washed with distilled water to neutralize them. Solids obtained were dried at room temperature. All reagents employed were provided by Sigma–Aldrich.
Also, as a reference, SiO2 was obtained from the agro-industrial wastes without employing vermicompost bioprocess. The extraction process to recuperate SiO2 is the same as described previously using calcination and acid treatment. In addition, commercial synthetic SiO2 Aerosil® 130 provided by Degussa AG was employed to compare size and structure with SiO2 nanoparticles produced in this research. Aerosil® 130 particles are amorphous SiO2 nanoparticles produced by high-temperature hydrolysis of silicon tetrachloride in an oxygen gas flame . Also, this research compares the particle features based on biotransformation process with those synthesized using chemical process.
SiO2 powders were characterized by employing a Fourier transform infrared spectrophotometer (FTIR) Bruker Vector 33 using KBr powders. Transmission electron microscopy (TEM) was realized using a JEOL TEM-1010 transmission electron microscope, and high-resolution transmission electron microscopy (HRTEM) was realized in a Tecnai G2 T20 Microscope. Average particle size was determined for dynamic light scattering (DLS) using a Brookhaven model BI200SM with laser He–Ne of 35 mW model 9167 EB-1 Melles-Griot. Elemental analysis was carried out using energy dispersion spectroscopy (EDS) mean software Oxford Inca X–Sight. EDS is adapted in equipment JEOL JSM-6060 LV Scanning Electron Microscope. X-ray diffraction (XRD) was realized in a diffractometer Rigaku, model MiniFlex, with a wavelength from 1.54 Å corresponding kα cupper radiations. Crystalline structures present in the samples were analyzed with Materials Data Jade software of MDI Materials Data.
Results and Discussion
Diameter mean using DLS to particles SiO2 synthesized with bioprocess and without bioprocess
Diameter mean (nm)
Diameter mean (nm)
EDS to particles SiO2 synthesized with bioprocess and without bioprocess
Figure 4c and 4d show the diffractrograms corresponding to particles obtained from sugarcane bagasse. Crystalline phases are present in both procedures (with and without bioprocess). However, some diffraction planes are not the same in both processes. This allows to assume that the calcination temperature and earthworm metabolism play an important role to generate different crystalline phases that involve not only silicon and oxygen atoms, but other elements take part, as well. In Fig. 4c and 4d, by comparing the diffractrograms (samples obtained without bioprocess at 500 and 700°C), it is possible to observe that the same crystalline phases are found: quartz (different crystallographic planes) and trydimite. However, the diffractrograms corresponding to samples obtained via bioprocess show different crystalline phases, such as: zinc phosphate, aluminum phosphate at 500°C and albite in 700°C.
It is important to mention that silica shows several polyphorms depending on temperature and pressure. Thus, although bioprocess conditions employed to obtain SiO2 particles are favorable to inducing α hexagonal quartz (corroborated by X-ray diffraction), it is possible to find others metastable polyphorms such as tetragonal arrangement (268–1,470°C). This structure belongs to β crystobalite . Therefore, some SiO2 nanoparticles obtained from sugarcane bagasse can be found with transitions of hexagonal to tetragonal phase. Thus, tetragonal arrangement does not appear in X-ray diffraction; however, in some nanoparticles characterized by HRTEM (Fig. 3b) it is identified.
Diffractrograms corresponding to particles obtained from coffee husk are shown in Fig. 4e and 4f. Significant changes in both processes (using bioprocess and without employing bioprocess), which are produced by temperature and metabolism in earthworms, are observed. At 500°C, by employing bioprocess, the diffraction peaks detected are related to quartz, trydimite, sanidine and magnesium nickel hydride, meanwhile without bioprocesses diffraction peaks appear, corresponding to trydimite, gypsum and calcium aluminim oxide hydrate. At 700°C, by employing bioprocess, quartz, aluminim phosphate and caminite are found, meanwhile without bioprocess appears: calcium aluminim oxide hydrate, trikalsilite and quartz.
Percent crystallization in particles SiO2 synthesized with bioprocess and without bioprocess
The microbial population in annelids is very important to achieve the biotransformation of the amorphous silica naturally present in the analyzed agro-industrial wastes. Characteristics of the organic matter exposed to a broad variety of microorganisms, as well as the method employed for the fragmentation and minerals release, represent key factors to understand the biocrystallization. Our results reveal a novel synthesis method to obtain SiO2 crystalline nanoparticles using annelids’ biotransformation by employing agro-industrial wastes. The approach represents an inexpensive and relatively eco-friendly technology in comparison with standard chemical methods. By taking into account the biological aspects of the production of SiO2 nanoparticles with specific crystal arrangement using annelids allows to extend the number of living organism dedicate to biosilification, in addition to open an interesting field toward the knowledge of new annelid bioprocesses with a primitive metabolism, as potential alternative natural nanotechnology bioprocesses to synthesize nanoparticles and nanostructures, for the particles obtained through biotransformation by annelids show similar characteristics than synthetic SiO2 Aerosil®130 such as size, composition and polydispersity. While synthetic particles possess amorphous structure the particles synthesized using vermicompost present different disables characteristics such as crystalline (different polymorphism) and nanometric dimension.
The authors are grateful to Ms. Maria de Lourdes Palma for her assistance in TEM, to Dr. Genoveva Hernández-Padron for her assistance in IR analysis, to Dr. Eric Rivera for his assistance in XRD, to CINVESTAV Querétaro, particularly to Dr. S. Jimenez and Mr. F Rodriguez for their assistance in some measurements and to DGEST and Consejo Nacional de Ciencia y Tecnologia (CONACyT), Mexico, for the economical support through the projects P333-05 and JI-58232, respectively. Financial support from the National Council for Science and Technology of Mexico (CONACYT) (PhD Scholarship to A.E.-G.) is gratefully acknowledged.
This article is distributed under the terms of the Creative Commons Attribution Noncommercial License which permits any noncommercial use, distribution, and reproduction in any medium, provided the original author(s) and source are credited.
- Alexandre A, Meunier J-D, Colin F, Koud J-M: Plant impact on the biogeochemical cycle of silicon and related weathering processes. Geochim. Cosmochim. Acta 1997, 61: 677–682. COI number [1:CAS:528:DyaK2sXhsFaltbw%3D]; Bibcode number [1997GeCoA..61..677A] COI number [1:CAS:528:DyaK2sXhsFaltbw%3D]; Bibcode number [1997GeCoA..61..677A] 10.1016/S0016-7037(97)00001-XView ArticleGoogle Scholar
- Morse ED: Silicon biotechnology: harnessing biological silica production to construct new materials. Els. Sci. Trends Biotech. 1999, 17: 230–232. COI number [1:CAS:528:DyaK1MXltFaisL8%3D] COI number [1:CAS:528:DyaK1MXltFaisL8%3D] 10.1016/S0167-7799(99)01309-8View ArticleGoogle Scholar
- Iler RK: The Chemistry of Silica. John Wiley & Sons, New York; 1979.Google Scholar
- Ball P: Made to Measure: New Materials for the 21st Century. Princenton University Press, Princenton, NJ. USA; 1999.Google Scholar
- Bauerlein E: Biomineralization of unicellular organism: an unusual membrane biochemistry for the production of inorganic nano- and microstructures. Angew Chem. Int. Edn 2003, 42: 614–641. COI number [1:CAS:528:DC%2BD3sXhs1Sitbw%3D] COI number [1:CAS:528:DC%2BD3sXhs1Sitbw%3D] 10.1002/anie.200390176View ArticleGoogle Scholar
- Hamm CE, et al.: Architecture and material properties of diatoms shells provide effective mechanical protection. Nature 2003, 421: 841–843. COI number [1:CAS:528:DC%2BD3sXht1Kqt7Y%3D]; Bibcode number [2003Natur.421..841H] COI number [1:CAS:528:DC%2BD3sXht1Kqt7Y%3D]; Bibcode number [2003Natur.421..841H] 10.1038/nature01416View ArticleGoogle Scholar
- Asada R, Okuno M, Tazaki K: Structural anisotropy of biogenic silica in pennate diatoms under Fourier transform polarized infrared spectroscopy. J. Mineral Petrol. Sci. 2002, 97: 219–226. COI number [1:CAS:528:DC%2BD3sXlsVOitQ%3D%3D] COI number [1:CAS:528:DC%2BD3sXlsVOitQ%3D%3D]View ArticleGoogle Scholar
- Almqvist N, et al.: Micromechanical and structural properties of pennate diatom investigated by atomic force microscopy. J. Microsc. 2001, 202: 518–532. COI number [1:CAS:528:DC%2BD3MXlt1SrsLc%3D] COI number [1:CAS:528:DC%2BD3MXlt1SrsLc%3D] 10.1046/j.1365-2818.2001.00887.xView ArticleGoogle Scholar
- Bansal V, Ahmad A, Sastry M: Fungus-mediated biotransformation of amorphous silica in rice husk to nanocrystalline silica. J. Am. Chem. Soc. 2006, 128: 14059–14066. COI number [1:CAS:528:DC%2BD28XhtVKitbzN] COI number [1:CAS:528:DC%2BD28XhtVKitbzN] 10.1021/ja062113+View ArticleGoogle Scholar
- Inagaki F, Motomura Y, Ogata S: Microbial silica deposition in geothermal hot waters. Appl. Microbiol. Biotechnol. 2003, 60: 605–611. COI number [1:CAS:528:DC%2BD3sXitlOqsbg%3D] COI number [1:CAS:528:DC%2BD3sXitlOqsbg%3D]View ArticleGoogle Scholar
- Kastner M: The Oceanic Lithosphere. Wiley, New York; 1981.Google Scholar
- Dujardin E, Mann S: Bio-inspired materials chemistry. Adv. Mater. 2002, 14: 775. COI number [1:CAS:528:DC%2BD38XkvVOiurw%3D] COI number [1:CAS:528:DC%2BD38XkvVOiurw%3D] 10.1002/1521-4095(20020605)14:11<775::AID-ADMA775>3.0.CO;2-0View ArticleGoogle Scholar
- Vrieling EG, Beelen TPM, van Santen RA, Gieskes WWC: Nanoscale uniformity of pores in diatomaceous silica: a combined small and wide angle X-ray scattering study. J. Phycol. 2003, 35: 1044–1053.Google Scholar
- Vrieling EG, Beelen TPM, van Santen RA, Gieskes WWC: Diatoms silicon biomineralization as an inspirational source of new approaches to silica production. J. Biotechnol. 1999, 70: 41–53. 10.1016/S0168-1656(99)00056-5View ArticleGoogle Scholar
- Sun Q, Vrieling EG, van Santen RA, Sommerdijk NAJM: Bioinspired synthesis of mesoporous silicas. Solid State Mater. Sci. 2004, 8: 111–120. COI number [1:CAS:528:DC%2BD2cXlvVWru70%3D] COI number [1:CAS:528:DC%2BD2cXlvVWru70%3D] 10.1016/j.cossms.2004.01.005View ArticleGoogle Scholar
- Dugdale RC, Wilkerson FP: Silicate regulation of new production in the equatorial Pacific upwelling. Nature 1998, 391: 270–273. COI number [1:CAS:528:DyaK1cXnsVyruw%3D%3D]; Bibcode number [1998Natur.391..270D] COI number [1:CAS:528:DyaK1cXnsVyruw%3D%3D]; Bibcode number [1998Natur.391..270D] 10.1038/34630View ArticleGoogle Scholar
- Hecky RE, Mopper K, Kilham P, Degens ET: The amino acid and sugar composition of diatom cell-walls. Marine Biol. 1973, 19: 323. COI number [1:CAS:528:DyaE3sXlt1art7w%3D] COI number [1:CAS:528:DyaE3sXlt1art7w%3D] 10.1007/BF00348902View ArticleGoogle Scholar
- Kroger N, Lorenz S, Brunner E, Sumper M: Self-assembly of highly phosphorylated silaffins and their function in biosilica morphogenesis. Science 2002, 298: 548. 10.1126/science.1076221View ArticleGoogle Scholar
- Shimizu K, Cha J, Stucky GD, Morse DE: Silicatein α: cathepsin L-like protein in sponge biosilica. Proc. Natl. Acad. Sci. 1998, 95: 6234. COI number [1:STN:280:DyaK1c3mtleguw%3D%3D]; Bibcode number [1998PNAS...95.6234S] COI number [1:STN:280:DyaK1c3mtleguw%3D%3D]; Bibcode number [1998PNAS...95.6234S] 10.1073/pnas.95.11.6234View ArticleGoogle Scholar
- Perry CC, Keeling-Tucker T: Model studies of colloidal silica precipitation using biosilica extracts from Equisetum telmateia. Colloid Polym. Sci. 2003, 281: 652. COI number [1:CAS:528:DC%2BD3sXkvFent74%3D] COI number [1:CAS:528:DC%2BD3sXkvFent74%3D] 10.1007/s00396-002-0816-7View ArticleGoogle Scholar
- Derry AL, Kurtz CA, Ziegler K, Chadwick AO: Biological control of terrestrial silica cycling and export fluxes to watersheds. Nature 2005, 433: 728–730. COI number [1:CAS:528:DC%2BD2MXhtleqsLo%3D]; Bibcode number [2005Natur.433..728D] COI number [1:CAS:528:DC%2BD2MXhtleqsLo%3D]; Bibcode number [2005Natur.433..728D] 10.1038/nature03299View ArticleGoogle Scholar
- Eipstein E: The anomaly of silicon in plant biology. Proc. Natl. Acad. Sci. USA 1994, 91: 11–17. Bibcode number [1994PNAS...91...11E] Bibcode number [1994PNAS...91...11E] 10.1073/pnas.91.1.11View ArticleGoogle Scholar
- Ding TP, Ma GR, Shui MX, Wan DF, Li RH: Silicon isotope study on rice plants from the Zhejiang province. China. Chin. Chem. Geol 2005, 218: 41. COI number [1:CAS:528:DC%2BD2MXktVahsLw%3D] COI number [1:CAS:528:DC%2BD2MXktVahsLw%3D]View ArticleGoogle Scholar
- Suryawanshi BG, Patil SS, Patil BN: Studies on the chemical composition of sugarcane tops. J. Maharashtra Agric. Univ. 2003, 28: 50–51.Google Scholar
- Pandey A, et al.: Biotechnological potential of coffee pulp and coffee husk for bioprocesses. J. Biochem. Eng. 2000, 6: 153–162. COI number [1:CAS:528:DC%2BD3cXntFShsLo%3D] COI number [1:CAS:528:DC%2BD3cXntFShsLo%3D] 10.1016/S1369-703X(00)00084-XView ArticleGoogle Scholar
- Raven JA: The transport and function of Silicon in plants. Biol. Rev. 1983, 58: 179–207. COI number [1:CAS:528:DyaL3sXlslakt7s%3D] COI number [1:CAS:528:DyaL3sXlslakt7s%3D] 10.1111/j.1469-185X.1983.tb00385.xView ArticleGoogle Scholar
- Jones LHP, Handreck KA: Silica in soils, plants and animals. Adv. Agron. 1967, 19: 107–149. COI number [1:CAS:528:DyaF1cXitFWrsA%3D%3D] COI number [1:CAS:528:DyaF1cXitFWrsA%3D%3D] 10.1016/S0065-2113(08)60734-8View ArticleGoogle Scholar
- Edwards CA, Lofty Jr: Biology Earthworms. Chapman and Hall, London; 1977.View ArticleGoogle Scholar
- Lee KE: Earthworms. Their Ecology and Relationships with Soils and Land Use. Academic Press, Australia; 1985.Google Scholar
- Edwards AC, Fletcher EK: Interactions between earthworms and microorganisms in organic-matter breakdown. Agric. Ecosystems Env. 1988, 24: 235–247. 10.1016/0167-8809(88)90069-2View ArticleGoogle Scholar
- Laverack : The physiology of earthworms. Int. Ser. Monogr. Pure Appl. Biol., Zool 1963, 15: 206.Google Scholar
- Went JC: Influence if earthworms on the number of bacteria in the soil. In Soil Organisms. Edited by: Koeksen J, Drift J. North Holland Publishing Company, Amsterdam; 1963.Google Scholar
- Parle JN: Microorganisms in the intestines of earthworms. J. Gen. MIcrobiol. 1963, 31: 1–11.View ArticleGoogle Scholar
- Atlavinyte O, Daciulyte J, Lugauskas A: Correlation between the numbers earthworms microorganisms and vitamin B12 in soils fertilized with straw. Liet. TSRA Mokslu Akad. Darb. Ser. B 1971, 3: 43–56.Google Scholar
- Treguer P, et al.: The silica balance in the World Ocean: a reestimate. Science 1995, 268: 375–379. COI number [1:CAS:528:DyaK2MXltFKkt7k%3D]; Bibcode number [1995Sci...268..375T] COI number [1:CAS:528:DyaK2MXltFKkt7k%3D]; Bibcode number [1995Sci...268..375T] 10.1126/science.268.5209.375View ArticleGoogle Scholar
- Del Amo YB: The chemical form of dissolved Si taken up by marine diatoms. A.M. J. Phycol. 1999, 35: 1162–1170. COI number [1:CAS:528:DC%2BD3cXnsFCqsA%3D%3D] COI number [1:CAS:528:DC%2BD3cXnsFCqsA%3D%3D]View ArticleGoogle Scholar
- Patwardhan VS, Clarson JS: Silicification and biosilicification part 6. Poly-l- histidine mediated synthesis of silica at neutral pH. J. Inorg. Organomet. Poly. 2003,13(1):50–53.Google Scholar
- Coradin T, Durupthy O, Livage J: Interaction of amino-containing peptides with sodium silicate and colloidal silica: a biomimetic approach of silification. Langmuir 2002, 18: 2331–2336. COI number [1:CAS:528:DC%2BD38Xhtlyjt7o%3D] COI number [1:CAS:528:DC%2BD38Xhtlyjt7o%3D] 10.1021/la011106qView ArticleGoogle Scholar
- Coradin T, Roux C, Livage J: Biomimetic self activated formation of multiscale porous silica in the presence of arginine-based surfactants. J. Mater. Chem. 2002,12(5):1242–1244. COI number [1:CAS:528:DC%2BD38XivF2rtrk%3D] COI number [1:CAS:528:DC%2BD38XivF2rtrk%3D] 10.1039/b201616hView ArticleGoogle Scholar
- Baluais G, Caratini Y: Medium purity metallurgical silicon and method for preparing same. Patent US7404941 assigned to Ferropem 2005.Google Scholar
- Aerosil R-Manufacture, properties and applications, Technical Bullettin Pigments. N. 11, Degussa-Huls AG, Germany; 2002.Google Scholar
- Sales AAJ, Petrucelli CG, Oliveira EVJF, Airoldi C: Some features associated with organosilane groups grafted by the sol–gel process onto synthetic talc-like phyllosilicate. J. Collod. Inter. Sci. 2006, 297: 95–103. COI number [1:CAS:528:DC%2BD28Xisl2qt7o%3D] COI number [1:CAS:528:DC%2BD28Xisl2qt7o%3D] 10.1016/j.jcis.2005.10.019View ArticleGoogle Scholar
- Lim HM, Blanford FC, Stein A: Synthesis and characterization of a reactive vinyl-functionalized mcm-41: probing the internal pore structure by a Bromination reaction. J. Am. Chem. Soc. 1997, 119: 4090–4091. COI number [1:CAS:528:DyaK2sXisVyjsbk%3D] COI number [1:CAS:528:DyaK2sXisVyjsbk%3D] 10.1021/ja9638824View ArticleGoogle Scholar
- Melde JB, Johnson JB, Charles TP: Mesoporous silicate materials in Sensing. Sensors 2008, 8: 5202–5228. COI number [1:CAS:528:DC%2BD1cXhsVekt7zK] COI number [1:CAS:528:DC%2BD1cXhsVekt7zK] 10.3390/s8085202View ArticleGoogle Scholar
- Gao X, Jensen ER, Li W, Deitzel J, Mcknight H, Gillespie WJ Jr.: Effect of fiber surface texture created from silane blends on the strength and energy absorption of the glass fiber/epoxy interphase. J. Compos. Mater 2008, 42: 513. COI number [1:CAS:528:DC%2BD1cXltFyns70%3D] COI number [1:CAS:528:DC%2BD1cXltFyns70%3D]Google Scholar
- Sumper M, Kroger N: Silica formation in diatoms: the function of long-chain polyamines and silaffins. J. Mater. Chem. 2004, 14: 2059–2065. COI number [1:CAS:528:DC%2BD2cXls1egsrs%3D] COI number [1:CAS:528:DC%2BD2cXls1egsrs%3D] 10.1039/b401028kView ArticleGoogle Scholar