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Rapid miner

Rapid Miner is an open-source tool and has a collection of various ML and data mining tools with plug and play operators [41], This demonstration can be prototyped for mnning Rapid Miner from within a Java project with an objective to use source code to work with Rapid Miner. [Pg.160]

File file = new File( rapidminer output file ) if(file.mkdir())  [Pg.160]

RapidMiner.setExecutionMode(RapidMiner.ExecutionMode.COMMANDLINE) RapidMiner.initO  [Pg.160]

Operator bayesClassifier = OperatorService.createOperator(NaiveBayes.class)  [Pg.160]

Operator raodelWriter = OperatorService.createOperator(ModelWriter.class)  [Pg.160]


Jhanson R, Ackerman CE, Scow KM (1999) Biodegradation of methyl ter/-butyl ether by abacterial pure culture. Appl Environ Microbiol 65 4788-4792 Kanaly RA, Bartha R, Watanabe K, Harayama S (2000) Rapid mineralization of benzo[a]pyrcnc by a microbial consortium growing on diesel fuel. Appl Environ Microbiol 66 4205-4211... [Pg.194]

Dodecyltrimethylammonium chloride is rapidly mineralized in fresh water after an acclimation period, and the rate is faster following the second rather than the first addition of the quaternary ammonium compound. [Pg.341]

In a cranberry soil pretreated with 4-nitrophenol, parathion was rapidly mineralized to carbon dioxide by indigenous microorganisms (Ferris and Lichtenstein, 1980). The half-lives of parathion (10 ppm) in a nonsterile sandy loam and a nonsterile organic soil were <1 and 1.5 wk, respectively (Miles et al, 1979). Walker (1976b) reported that 16 to 23% of parathion added to both sterile and nonsterile estuarine water was degraded after incubation in the dark for 40 d. [Pg.890]

The use of other isolated pure (Table 22.1) and mixed microbial cultures (Grigg et al., 1997) that rapidly mineralize. v-triazines may further improve the prospects for bioremediation. Moreover, novel approaches to enhance the... [Pg.320]

Barriuso, E. and S. Houot (1996). Rapid mineralization of the y-triazine ring of atrazine in soils in relation to soil management. Soil Biol. Biochem., 28 1341-1348. [Pg.321]

Iwamoto M, Shapiro IM, Yagami K, Boskey AL, Leboy PS, Adams SL, Pacifici M. Retinoic acid induces rapid mineralization and expression of mineralization-related genes in chondrocytes. Exp Cell Res. 1993 207 413-420. [Pg.254]

Plants. The a.i. is extensively metabolised Soil. Readily biodegradable. Soil DTJ0 0.6-2 days (lab., aerobic conditions, 20°C) rapidly mineralized... [Pg.1907]

Katraly, R. A., Bartha, R., Watarrabe, K. Harayama, S. (2000). Rapid mineralization of betrzo[a]pyretre by a microbial consortium growing on diesel fuel. Applied and Environmental Microbiology, 66, 4205-11. [Pg.205]

Nutrient recycling and supply is tightly regulated by largely biotic processes, such as retranslocation or resorption prior to leaf abscission (Medina and Cuevas 1989, Cuevas and Medina 1990). Nutrients are also reutilized from decomposing residues through rapid mineralization and uptake by a dense... [Pg.54]

Commonly, the forest-derived C declines sharply in the first years of pasture installation, due to rapid mineralization of a very... [Pg.170]

A9.4.3.3.2 These criteria are proposed in order to ensure that rapid mineralization did occur, although the test was ended before 28 days and before the pass level was attained. Interpretation of test data that do not comply with the prescribed pass levels must be made with great caution. It is mandatory to consider whether a biodegradability below the pass level was due to a partial degradation of the substance and not a complete mineralization. If partial degradation is the probable explanation for the observed biodegradability, the substance should be considered not readily biodegradable. [Pg.466]

Nucleation of calcium phosphate precipitation within the matrix vesicles is mediated by phosphatidylserine, which comprises about 8% of the phospholipids of the inner cytosolic membrane surface (Fig. 9.5a). Calbindin in the vesicle (Fig. 9.5b) may also contribute. Rapid mineral growth within the vesicle keeps the concentration of dissolved calcium and inorganic phosphate ions so low that additional Ca2+ and Pi ions spontaneously enter from the extracellular fluid via their respective transporters. Attached type II and type X collagens from cartilage in the growth plate enhance calcium ion transport and calcification during endochondral ossification (Fig. 9.5b). [Pg.138]

Figure 9.8 outlines how matrix vesicles increase and decrease the concentration of pyrophosphate. NTP-PPi hydrolase synthesizes pyrophosphate from stromal fluid nucleotides, mostly ATP (ATP —> AMP + PPi). Many cells secrete ATP into the extracellular fluid and it passes into the blood plasma where it affects a variety of cells independently of its function in intracellular energy metabolism. In mice, a nonfunctional ANK protein or a deletion of NTP-PPi hydrolase decreases the extracellular pyrophosphate concentration and the phenotype exhibits extensive mineralization. Thus, the hydrolysis of pyrophosphate appears to be a major function of alkaline phosphatase (TNAP) after the calcium phosphate precipitate has raptured the matrix vesicles. Rapid mineralization of collagen and the rest of the osteoid matrix ensue without a need to transport any more Ca2+ or Pi to the region. [Pg.140]

Thermal expansion induced by insolation may be of importance in desert areas where rocky outcrops and soil surfaces are barren. In a desert, daily temperature excursions are wide and rocks are heated and cooled rapidly. Minerals have different coefficients of thermal expansion. Consequently, when a rock is heated or cooled, its minerals differentially expand and contract inducing stresses... [Pg.134]

All soils from fields previously treated with carbofuran exhibited a much higher mineralization rate than soils from non-history fields. Previous reports have confirmed the enhanced degradation of carbofuran, and its rapid mineralization In each carbofuran-hlstory soil is Indicative of Its great susceptibility to enhanced degradation. Even the fencerow soils surrounding carbofuran-history fields exhibited increased carbofuran mineralization rates, and had apparently been contaminated by carbofuran or carbofuran-treated soli. Up to 5 years had elapsed since the last carbofuran soil application to history soils. [Pg.71]

In summary, preservation of a seawater redox signal is favored by rapid mineralization and stabilization at the sediment/water interface and uptake of REE from pore waters (rather than from seawater) is likely to reduce or eliminate any inherited cerium anomaly. Negative cerium anomalies in ancient marine biogenic apatite therefore suggest oxic conditions in the water column and possibly in the upper pore waters, but the lack of a negative cerium anomaly in biogenic apatite does not necessarily indicate sub-oxic or anoxic conditions in the water column (Kemp and Trueman in press). [Pg.508]

BIOLOGICAL PROPERTIES ThOD 2.06 ring distribution by Pseudomonas at 200 mg/L parent 100% in 58 hr, mutant 100% in 14 hr onee released, it will decrease in concentration due to dilution and photooxidation release to water and soil will dissipate due to vaporization and slow biodegradation in the soil or water rapid mineralization (20%/week) is reported ... [Pg.265]

Less than 3% of soil organic phosphorus is present as nucleic acids and derivatives derived from the decomposition of living organisms (Dalai, 1977). The four bases of DNA have been identified in humic acids (Anderson, 1961). The presence of nucleic acids and derivatives in the soil was confirmed by the isolation of two pyrimidine nucleoside diphosphates (Anderson, 1970). Nucleic acids are rapidly mineralized, re-synthesized and combined with other soil constituents, or incorporated into microbial biomass (Anderson and Malcolm, 1974). Nevertheless, the interaction of nucleases with soil constituents can inhibit DNA hydrolysis, with important environmental consequences related to extracellular gene uptake by bacteria (Demanfeche et al., 2001). [Pg.90]

The broad band of the dashed Fe+++ spectrum at 300 nm is attributed to Fe(III)OH2+,9 while the top spectrum with a shoulder at 260 nm is assigned to Fe(lII)(C204)33-. The spectra in the lower left hand corner are of samples taken at various times from the O2 purged solution during uv radiation. The t=5 minute sample (4 minutes after turning on the lamp) already shows the absorbance at 210 reduced by more than 80% relative to what it was in the 1(X) ppm OA solution by t=10 it is reduced about 90%. Rapid mineralization is confirmed by the NPOC measurements seen in curve OA 4 in Figure 6. [Pg.67]


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Rapid miner classification

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