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Moores curve

A range of individual pore size PLgel packing materials is produced and their pore size distribution is conveniently represented by a SEC calibration curve as illustrated in Fig. 12.1. It should be pointed out that the descriptors used for the different pore sizes, 50 A, 100 A, and so on, are not the actual pore sizes of the beads but relate to the size of a polystyrene molecule just excluded from the packing material. This nomenclature comes from the original work carried out by Moore (3) and should only be viewed in the context of differentiating... [Pg.350]

The terrestrial biota seem unable to take up much of the excess CO2. In fact, a careful assessment of the impact of deforestation and land-use changes indicate that the terrestrial biota has been a considerable source of CO2 during the past century (Bolin, 1977 Woodwell et al, 1983). A complex effort to deduce mankind s impact on terrestrial biota using a bookkeeping model based on historical records on land use in all parts of the world (Moore et al, 1981 Houghton et al, 1983 Woodwell et al., 1983) gives the curves in Fig. 11-25. Woodwell et al. (1983)... [Pg.306]

Fig. 3.12. Simple (exponential) curve of growth for low-excitation Fe I lines with wavelengths between 4000 and 8700 A at the centre of the solar disk, with 6>ex = 1.00, b = lkms-1 (assuming Roo = 1), a = 0.02. Equivalent widths are from Moore, Minnaert and Houtgast (1966). gf -values are from furnace measurements by the Oxford group (Blackwell et al. 1986 and references therein). Fig. 3.12. Simple (exponential) curve of growth for low-excitation Fe I lines with wavelengths between 4000 and 8700 A at the centre of the solar disk, with 6>ex = 1.00, b = lkms-1 (assuming Roo = 1), a = 0.02. Equivalent widths are from Moore, Minnaert and Houtgast (1966). gf -values are from furnace measurements by the Oxford group (Blackwell et al. 1986 and references therein).
Moore JW, Flanner HH. Mathematical comparison of curves with an emphasis on in vitro dissolution profiles. Pharm Tech 1996 206 64-74. [Pg.96]

One of the most powerful techniques by which protein-protein neighborhoods within the ribosomal particles can be elucidated is neutron scattering. When using this method to determine the relative positions of proteins in the 30 S subunit, the pardcle is reconstituted with two specific proteins that are deuterated whereas all other ribosomal components are in the protonated form (Moore, 1980). The subunits containing the two deuterated proteins give additional contributions to the scattering curves which provide information on the lengths of the vectors between the two deuterated proteins. [Pg.34]

Curve Pond Zone, and Boomerang all hosted within felsic volcanic rocks and spatially associated with black, locally graphitic shale and chert. (McKenzie et al. 1993 Evans Kean 2002 Rogers van Staal 2002, Squires Moore 2004) however, the Boomerang deposit is spatially associated with significant volumes of volcaniclastic rocks of intermediate composition. [Pg.332]

Fig. 16.15 Phosphate adsorption curves of three low moor soils with different goethite content as a function of contact time (1 -238 h) (Schwertmann Schieck, 1980 with permission). Fig. 16.15 Phosphate adsorption curves of three low moor soils with different goethite content as a function of contact time (1 -238 h) (Schwertmann Schieck, 1980 with permission).
Here, / is in amu A2, M is in amu, d is in A, a is in A-1, and v is in cm-1. The second exponential term results from a correction for the change in velocity due to the increase in rotational energy. The steric factor, Z0, is introduced as in V-T theory to account for noncolinear collision orientations. Moore tested this equation, along with two other more approximate forms, on a series of molecules having one or more H (or D) atoms. He also examined V-R transfer for collisions of dissimilar molecules, such as C02-CH4, C12-HC1, and CH4-Ar. Twenty-five different molecules having small moments of inertia were fitted with a single curve represented by equation (71) using a = 2.94 A-1 and Z0 = 5.0, with at least qualitative success. [Pg.202]

Chen and Moore s investigation [220] of room-temperature relaxation in HC1 and in DC1 shows that the high-temperature shock-tube results [222,225] do not extrapolate smoothly according to a 7 1/s law. Figure 3.29, taken from their paper, shows that while log P versus r 1/s appears to be fairly linear above 1000°K, the room-temperature deactivation probability is 15 times larger than the value expected by linear extrapolation of the shock-tube data. The upper dashed curve represents a probable interpolation between the shock-tube data and the fluorescence data the lower dashed line is an interpolation based on SSH theory for V-T transfer. The datum represented by the square is for vibrational deactivation of DC1 by HC1. [Pg.248]

Figure 13. Chondtite-normalized REE patterns for soapstone from the central Labrador coast. Dashed curves (%--%) outline the range of three samples from the Moore s Island, Okak outcrops (M) and two artifacts made of this soavstone. The Eskimo Island (O) artifact is from a Labrador Eskimo site (historic period) in Hamilton Inlet and the Koliktakik (A) artifact is from a soapstone pot from a late Dorset Eskimo site in the Nain region. A sample of the soapstone outcrop near Vanse aux Meadows (L) is shown (0) along with the Viking spindle whorl (A) made from this material. Figure 13. Chondtite-normalized REE patterns for soapstone from the central Labrador coast. Dashed curves (%--%) outline the range of three samples from the Moore s Island, Okak outcrops (M) and two artifacts made of this soavstone. The Eskimo Island (O) artifact is from a Labrador Eskimo site (historic period) in Hamilton Inlet and the Koliktakik (A) artifact is from a soapstone pot from a late Dorset Eskimo site in the Nain region. A sample of the soapstone outcrop near Vanse aux Meadows (L) is shown (0) along with the Viking spindle whorl (A) made from this material.
Palytoxin is a white, amorphous, hydroscopic solid that has not yet been crystallized. It is insoluble in nonpolar solvents such as chlorophorm, ether, and acetone sparingly soluble in methanol and ethanol and soluble in pyridine, dimethyl sulfoxide, and water. The partition coefficient for the distribution of palytoxin between 1-butanol and water is 0.21 at 25°C based on comparison of the absorbance at 263 nm for the two layers. In aqueous solutions, palytoxin foams on agitation, like a steroidal saponin, probably because of its amphipathic nature. The toxin shows no definite melting point and is resistant to heat but chars at 300°C. It is an optically active compound, having a specific rotation of -i-26° 2° in water. The optical rotatory dispersion curve of palytoxin exhibits a positive Cotton effect with [a]25o being -i-700° and [a]2,j being +600° (Moore and Scheuer 1971 Tan and Lau 2000). [Pg.76]

Figure 3 Effect of Zn + binding on the CD spectrum of the hemopexin (Hx)-heme complex the Hx-heme complex (thick black curve), additions of 3-15 equiv of Zn + (thin black curve), and addition of 18 equiv of Zn + (red curve). The Hx-heme concentration is 8 xM, with 50 mM bisTris buffer and 50 mM sodium chloride (pH 7.0, 25 °C). (Reprinted with permission from Mauk, Rosell, Lelj-Garolla, Moore and Mauk. 2005 American Chemical Society)... Figure 3 Effect of Zn + binding on the CD spectrum of the hemopexin (Hx)-heme complex the Hx-heme complex (thick black curve), additions of 3-15 equiv of Zn + (thin black curve), and addition of 18 equiv of Zn + (red curve). The Hx-heme concentration is 8 xM, with 50 mM bisTris buffer and 50 mM sodium chloride (pH 7.0, 25 °C). (Reprinted with permission from Mauk, Rosell, Lelj-Garolla, Moore and Mauk. 2005 American Chemical Society)...
Ninhydrin Assay for Adsorbed Proteins. Measurements were made by a colorimetric procedure based on the reaction of ninhydrin with amino acids (25). The films were hydrolyzed in 5 ml of 2.5N NaOH for 2 hrs in capped plastic tubes in a boiling water bath. Then 1.5 ml of glacial acetic acid was added and mixed next I ml of ninhydrin reagent was added and mixed. [The reagent was three times more concentrated in ninhydrin, SnCb, and citrate than prescribed by Moore and Stein (25)]. The tubes were capped and boiled 20 mins more. The solution was clarified by centrifugation, and the absorbance read immediately at 570 nm on a Beckman DB spectrophotometer. If necessary, the sample was diluted with 50-50 2-propanol-water. Calibration curves (absorbance vs. fig of protein) were constructed in the 0-30 and 0-100 fig range with known amounts of each type of protein subjected to this same analysis procedure. [Pg.233]

Figure 4. Chondrite-normalized REE patterns for representative soapstone samples from outcrops in the Okak area. Curves 1 (O) and 2 (%) are the types of patterns found at the Cojfin Island outcrop curve 3 (x) is an outcrop at Moores Island curve 4 (Aj is typical of the Nutak outcrop. Figure 4. Chondrite-normalized REE patterns for representative soapstone samples from outcrops in the Okak area. Curves 1 (O) and 2 (%) are the types of patterns found at the Cojfin Island outcrop curve 3 (x) is an outcrop at Moores Island curve 4 (Aj is typical of the Nutak outcrop.
Comparison of data range on the variability of curve fitting. (Modified from Moore, D.R.J. and P.-Y. Caux. 1997. Estimating low toxic effects. Environ. Toxicol. Chem. 16 794—801. With permission.)... [Pg.58]

In 6 years there has been a number of papers written on the interpretation of the concentration (dose)-response curve. Results from the studies of D. Moore, R Caux, and M. Newman have demonstrated that curve-fitting is superior to the calculation of no-effect or low-effect values. G. Stephenson and colleagues have also published a flow diagram describing in detail the steps necessary to fit a curve to toxicity data. [Pg.494]

Drs. Moore and Stein of the Rockefeller Institute have studied the quantitative amino acid content of gramicidins A and B by starch chromatography. Figure 4 is an elution curve of gramicidin A. Here the concentration is estimated by the sensitive ninhydrm color test. 93% recovery of the nitrogen is accounted for. It has not proven possible... [Pg.317]

Figure 16.9. Calibration curve based on determinations of HCY standards. [Reprinted, with permission, from Mohammed T. Shipchandler, and Ewin G. Moore, Clinical Chem. 41 7, 1995, 991-994. Rapid, Fully Automated Measurement of Plasma Homocyst(e)ine with the Abbot Imx Analyzer . Amer. Assos. for Clinical Chemistry.]... Figure 16.9. Calibration curve based on determinations of HCY standards. [Reprinted, with permission, from Mohammed T. Shipchandler, and Ewin G. Moore, Clinical Chem. 41 7, 1995, 991-994. Rapid, Fully Automated Measurement of Plasma Homocyst(e)ine with the Abbot Imx Analyzer . Amer. Assos. for Clinical Chemistry.]...
A second-order transition would produce no obvious change in fluorescence image, so the close correspondence found by Moore et al. between the position of the abrupt change in slope in their isotherms and the start of the two-phase region in the fluorescence observations, rules out Dervichian s interpretation of the temperature dependence of the isotherms. If a second-order line intersects the coexistence curve, it does so at a temperature above 31 °C and an area smaller than 28 A. ... [Pg.426]

Fig. 7-28. Combined residence lifetimes of aerosol particles as a function of size. [Adapted from Jaenicke (1978c, 1980).] Important removal processes, active in various size ranges, are indicated. Coagulation and sedimentation time constants were calculated the time constant for wet removal is the residence time derived from 2,0Bi/210Pb and 222Rn/210Pb ratios (Martell and Moore, 1974). Curves 1 and 2 represent the background aerosol for rwel equal to 12 and 3 days, respectively. Curve 3 represents the continental aerosol with rwel = 6 days. The dashed line is calculated from a simple model for sedimentation equilibrium, as described in Section 7.6.3. Fig. 7-28. Combined residence lifetimes of aerosol particles as a function of size. [Adapted from Jaenicke (1978c, 1980).] Important removal processes, active in various size ranges, are indicated. Coagulation and sedimentation time constants were calculated the time constant for wet removal is the residence time derived from 2,0Bi/210Pb and 222Rn/210Pb ratios (Martell and Moore, 1974). Curves 1 and 2 represent the background aerosol for rwel equal to 12 and 3 days, respectively. Curve 3 represents the continental aerosol with rwel = 6 days. The dashed line is calculated from a simple model for sedimentation equilibrium, as described in Section 7.6.3.

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