MODx encountered the following error while attempting to parse the requested resource: . PHP Parse Error . PHP error debug . Error: . mysql_connect() [ function.mysql-connect ]: Too many connections . Error type/ Nr.: ... home/biochem/biochem.bio.msu.ru/docs/manager/includes/extenders/dbapi.mysql.class.inc.php . Line: . ... Line 87 source: . ... mysql_pconnect($host, $uid, $pwd) : mysql_connect($host, $uid, $pwd, true))) { . Parser timing . ... PHP: . 0.0148 s . ...

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... The factors that play the key role in complex formation are as follows: the rate of protein diffusion to the docking site; long-range electrostatic interactions between protein surfaces, geometric and chemical complementarity of binding areas; molecular mobility at the protein­protein interphase, hydrogen bonds, Van der Waals interactions, hydrophobic interactions, and salt bridges. ... Three-dimensional protein molecules are constructed on the basis of data extracted from the Protein Data Bank. ...

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• МОДЕЛИРОВАНИЕ ВЗАИМОДЕЙСТВИЯ МАГНИТНОГО ПОЛЯ С ОБЪЕМНЫМИ ВЯЗАНЫМИ СТРУКТУРАМИ

Welcome to Fourmilab 's calendar converter! ... In the Julian calendar every fourth year is a leap year in which February has 29, not 28 days, but in the Gregorian, years divisible by 100 are not leap years unless they are also divisible by 400. ... The average length of a year is 365.2468 days compared to the actual solar tropical year (time from equinox to equinox) of 365.24219 days, so the calendar accumulates one day of error with respect to the solar year every 216 years. ... Excel serial day: . ...

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... 4, 2014 DOI: 10.1007/s11664-014-3031-7 г 2014 TMS Calculation of the Thermoelectric Properties of n- and p-Type Lead Telluride Using a Three-Band Model of the Electron Energy Spectrum A.V. DMITRIEV 1,2 and E.S. TKACHEVA 1 1.- ... This expression is valid for any band. ... The averaged overlap integral Calculation of the Thermoelectric Properties of n- and p-Type Lead Telluride Using a Three-Band Model of the Electron Energy Spectrum 1283 I ?k; k0 о М 2 1X hk; ijk0 ; ji 4 iМ 1 ; 2 jМ1;2 2 w DA ?k; i ...

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• http://lizard.phys.msu.su/home/science/rec-GaN.pdf
• http://lizard.phys.msu.su/home/science/rec-GaN.ps.gz
• http://lizard.phys.msu.su/home/science/sust-2003-17-443.pdf

... SUPER RATIO . ... On this page I will present the most important (on my opinion) idea on Intellegence Life in the Universe . ... On the problem of the Super Ratio in astrophysics" . ... As a matter of fact, this is the main problem of the modern natural science. ... Here I shall try to speak about the most important problem of the modern natural science, the problem which is undoubtedly, of more importance than discovery of Blacks Holes, creation of Grand Unification Theory or Artificial...

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A full system of equilibrium differential equations for the finite number of suspension lines (n = 28) of square parachute is derived. ... One can determine the shapes of inflated canopy radial cross-sections, stress distribution of radial ribbons on the canopy surface and fabric stress between them, drag coefficients for various line lengths and air-permeability by means of computer simulation. ... Initially, this problem was solved assuming D p = const over total canopy of square parachute. ...

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• A Little History

MATSYM - symbolic matrix processor . ... To use the program you will need a MAT file (liked CIR file: "User manual for CIRSYM program") of your system. ... In first string of MAT file enter any text you want to be the title of your system. ... Starting from string 2 (if is not comments - "*") enter the system element name, incident row and column and, optionally, its value. ... To generate a solution, run MATSYM.exe and enter "system_file_name.CIR" or click on the "ENTER" (in "MAT" case). ...

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• Symbolic circuit processor

... Surface disturbance and deformat ion are shown in the same scale. Displac the free surface is much smoother as compared bottom deformations: init ial elevat ion has amplitude and spreads over a rather wide area. bottom theory, bottom ement of with the smaller F ­ velocity potential, H ­ depth, ­ vector of bottom deformation, 0 ­ initial elevation a . ... The init ial elevation assumed to be equal to the vertical bottom deformat ion (a); calculated with use of the Laplace smoothing algorithm (b). ...

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• http://ocean.phys.msu.ru/science/nosov/EGU2010_pumping.pdf
• http://ocean.phys.msu.ru/science/nosov/EGU2011_tsunami%20vs%20eq.pdf