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1.
It has been found that in general the volatility of dichlorides is much enhanced in the presence of gaseous A1C13 and FeCl3, and the existence of the complexes MA12C18, MAl3Cl11, and MFe2Cl8 is postulated. ΔH T, ΔS T, andT for MCl2(s) + 2AlCl3(g) = MAl2Cl8(g) are CaCl2: −17.8 kcal, −25.7 cal K−1 at 900 °K; CoCl2: −15.2, −19.4 at 750°K; MgCl2: −13.8, −17.9 at 800°K; MnCl2: −15.8, −20.9 at 750°K; NiCl2: −16.3, −24.2 at 750°K. For MCl2(s) + 3AlCl3(g) = MAl3Cl11(g) − CaCl2: −30.0, −40.5 at 900°K; CoCl2: −36.6, −47.4 at 700°K; MgCl2: −42.6, −55.4 at 750°K; MnCl2: −33.3, −42.0 at 750°K. For MCl2(s) + 2FeCl3(g) = MFe2Cl8(g) − CdCl2: −19.4, −20.9 at 700°K: CoCl2: −16.5, −17.2 at 800°K, MnCl2: −19.1, −21.2 at 750°K; NiCl2: −19.7, −24.4 at 800°K. Enhanced volatility was also found for ZnCl2, PbCl2, and CuCl, but since the condensed phase was liquid of unknown composition no calculations could be made. Owing to the interplay of the above equilibria with the dimerization equilibria for A1C13 and FeCl3 the effective vapor pressures of the dichlorides in the presence of the trichlorides pass through maxima in the region 600° to 700°C.  相似文献   

2.
Measurements have been made on the thermal capacity of γ-Gd2Se3 at 58.88–298.34 K. Values have been obtained for the thermal capacity, entropy, reduced Gibbs energy, and enthalpy under standard conditions: C°p = 125.87 ± 0.5 J· mole−1 · K−1; S°(298.15 K) = 196.5 · 1.6 J · mole−1 · K−1; Φ°(298.15 K) = 103.6 ± 1.6 J · mole−1 · K−1; H°(298.15 K)-H°(0) = 27681 ± 138 J · mole−1. The enthalpy of Gd2Se3 has been measured and the major thermodynamic functions have been calculated for the solid and liquid states over the temperature range 450–2300 K. The temperature dependence of the enthalpy in the ranges 300–1800 K and 2000–2300 K are represented: H°(T)-H°(298.15 K) = = 1.1949 · 10−2 · T2 + 122.38 · T + 347402 · T−1 − 38716 and H°(T)-H°(298.15 K) = 262.81 · T-− 196047, respectively. The calculated temperature, enthalpy, and entropy of melting for Gd2Se3 are: Tm = 1925 ± 40 K, ΔmH° (Gd2Se3) = 68.5 kJ · mole-1, ΔmS°(Gd2Se3) = 35.6 J · mole−1 · K−1. __________ Translated from Poroshkovaya Metallurgiya, Nos. 3–4(448), pp. 56–61, March–April, 2006.  相似文献   

3.
The nonideal activity of a metal oxide in a molten binary silicate system is described by treating the liquid as an ideal solution and by considering the formation of a few complexes. Application of this approach to the binary system PbO-SiO2 shows that the experimentally determined activity of PbO(l) can be modeled by considering the lead silicate melt as an ideal solution of Pb2+ and O2−,SiO 4 4− , Si2O 7 6− , Si12O 37 26− , and Si4O 10 4− . The calculated Gibbs free energy values for the formation of the anionic complexes from O2− and SiO 4 4− are: ΔGℴ(Si2O 7 6− )/J · mol−1 = 38977 − 30.909(T/K); ΔGℴ(Si12O 37 26− )/J · mol−1 = 200158 − 121.813(T/K); Δℴ(Si4O 10 4− )/J · mol−1 = 104627 − 28.094(T/K). Values of Gibbs free energy of formation of the solid phases PbO, Pb4Si06, Pb2SiO4, PbSiO3, and SiO2 which, together with the melt model data, give the best fit to experimental phase relations in the system PbO-SiO2 were calculated. These values are all in good agreement with literature data.  相似文献   

4.
The thermodynamic properties of dilute solutions of sulfur in pure liquid nickel were investigated at 1500, 1550, and 1575°C for sulfur concentrations up to 0.7 wt pct. Based on the infinitely dilute, wt pct standard state, the equilibrium data obtained for the reaction: H2(g) + S = H2S(g) were fitted by the equations: logK = − 1489/T − 1.772, and ΔG° = 6812 + 8.11T, cal/mole. For the solution ofS 2(g) in pure Ni according to the reaction: 1/2S 2(g) = S (in Ni), the standard free energy of solution is found to be: ΔG° = - 28,342 + 3.62T, cal/mole. For the very dilute solutions of sulfur normally encountered in nickel-base melting, the activity coefficient of sulfur in pure Ni at 1575°C is given by: log fS= -0.035 (pct S). The effects of alloying elements normally used in nickel-base alloys on the activity coefficient of sulfur in molten nickel were investigated. The activity coefficient of sulfur is increased by all of the alloying elements studied, as evidenced by the interaction parameters: eS fe = +0.005, eS Cr = +0.030, eS Mo = +0.053, eS Ti = +0.160, and eS A1 = +0.133. Measured values of the activity coefficient of sulfur in the quaternary system Ni-S-Cr-Fe agreed reasonably well with those predicted from binary and ternary data. This work constitutes a portion of the work performed by W. F. VENAL for the Ph.D. degree from the University of Illinois at Chicago Circle. Formerly Professor of Metallurgical Engineering at UICC.  相似文献   

5.
Gibbs energy change for the reactionxFe(s) + 1/2O2(g) = Fe x O(s) has been redetermined using the galvanic cell (−) Fe(s), Fe x O(s)∥ZrO2 − CaO∥NiO(s), Ni(s)(+) in the temperature range 866 to 1340 K. The results are at variance with earlier works in that they reflect the transformations occurring in the iron phase. The Gibbs energy function is represented by two nonlinear equations,viz., ΔG° (866 to 1184 K) = −251480 − 18.100T + 10.187T lnT ± 210 J/mol and ΔG° (1184 to 1340 K) = −286248 + 181.419T - 13.858T lnT ± 210 J/mol. Formerly Research Assistant at the Department of Theoretical Metallurgy, The Royal Institute of Technology, Stockholm  相似文献   

6.
The vapor pressure of sulfur over Ni-S melts of various compositions was calculated from the equilibrium weight of the melt in gas streams of known H2S-H2 composition. The Gibbs-Duhem equation was used to calculate the activity of nickel and other thermodynamic properties. For the reaction: 3Ni(S) + S2(g) ⇌ Ni3S2(l) the suggested free energy rslationship is: ΔG° = -57,910 + 15.89T (800° to 1100°C). The Calculations were extrapolated to predict that for the reaction: Ni(s) + 1/2S2(g) ⇌ NiS(l), ΔG° = -26.730 + 10.5T (1000° to 1100°C)  相似文献   

7.
Modified coulometric titrations on the galvanic cell: O in liquid Bi, Sn or Ge/ZrO2( + CaO)/Air, Pt, were performed to determine the oxygen activities in liquid bismuth and tin at 973, 1073 and 1173 and in liquid germanium at 1233 and 1373 K. The standard Gibbs energy of solution of oxygen in liquid bismuth, tin and germanium for 1/2 O2 (1 atm) →O (1 at. pct) were determined respectively to be ΔG° (in Bi) = −24450 + 3.42T (±200), cal· g-atom−1 = − 102310 + 14.29T (±900), J·g-atom−1, ΔG° (in Sn) = −42140 + 4.90T (±350), cal· g-aton−1 = −176300 + 20.52T (± 1500), J-g-atom−1, ΔG° (inGe) = −42310 + 5.31 7 (±300), cal·g-atom−1 = −177020 + 22.21T(± 1300), J· g-atom−1, where the reference state for dissolved oxygen was an infinitely dilute solution. It was reconfirmed that the modified coulometric titration method proposed previously by two of the present authors produced far more reliable results than those reported by other investigators. TOYOKAZU SANO, formerly a Graduate Student, Osaka University  相似文献   

8.
The rate of desulfurization of Fe-C-Si-S meltsin vacua (10 ώm pressure) has been investigated using 15 kg alloys melted by induction heating. For the sulfur contents from 0.008 to 0.1 pct investigated, the rate is a first-order type with respect to sulfur. Over this sulfur concentration range and in the presence of carbon up to saturation and silicon from 0 to 5 pct, the sulfur activity is sufficiently high that the fractional surface coverage by adsorbed sulfur is within 0.75 < θS < 1. The rate equation derived to satisfy the experimental findings for the limiting case of θS → 1 indicates that sulfur is evolved primarily via two activated reactions involving (SiS2)° and (S2)°. These complexes then produce SiS and S vapor species. At 1600°C the rates of formation of these volatile species are about one fourth of those for free vaporization of SiS and sulfur, respectively. The apparent heats of activation are ∼47 kcal for SiS and ∼37 kcal for sulfur vapor. Using an apparatus involving a Knudsen cell and the Bendix mass spectrometer, the enthalpy of reaction SiS2(s) + Si(s) = 2SiS(v) has been measured, giving 102.2 kcal. Combining this with other thermodynamic data, the free energy of formation of SiS vapor is evaluated as Si(s) + 1/2S2(v) = SiS(v) δF° = 15,500-19.5T from 1000° to 1686°K Si(l)+ 1/2S2(v)= SiS(v) δF°= 3500 -12.4T above 1686°K  相似文献   

9.
The possibility of using quantitative differential thermal analysis to investigate phase transformations is examined. The temperature, enthalpy, and entropy of polymorphic transformations in LaGe1.8 and SmSi2 are determined: Ttr = 724 K, ΔtrH = 1635 ± 79 J · mole−1, ΔtrS = 2.3 ± 0.1 J · mole−1 · K−1 (LaGe1.8); Ttr = 658 K, ΔtrH = 1384 ± 69 J · mole−1, ΔtrS = 2.1 ± 0.1 J · mole−1 · K−1 (SmSi2). __________ Translated from Poroshkovaya Metallurgiya, Vol. 46, No. 3–4 (454), pp. 72–78, 2007.  相似文献   

10.
The standard enthalpies of formation of TiSi2 and VSi2 have been measured by a new calorimetric method. The following results are reported: ΔH f ° (TiSi2) = −(170.9 ± 8.3) kJ mol−1 and ΔH {f °} (VSi2) = −(112.4 ± 6.0) kJ mol−1. These results are compared with experimental, assessed, and predicted values reported in the literature and with our own data for the corresponding borides. Estimates are given for the enthalpies of formation of the silicides of scandium and chromium.  相似文献   

11.
The theory of the solid-electrolyte cells is given, and it is shown that cryolite itself with Ca2+ in solid solution is a suitable Na+-ion conductor. Experimental electromotive forces for the ranges 570° to 725°C and 570° to 670°C, r − 18,960 cal with a standard deviation of ±36 cal (based on a third-law calculation). For 5NaF(s) + 3AlF3(s) = Na5Al3F14(s), ΔG° = −38,560 − 7.081T with a standard deviation of ±130 cal. Combination of these results with recent values for Al + 3/2 F2 = A1F3 and for 6NaF + Al = Na3AlF6 + 3Na gives ΔH°f298(Na3AlF6) = −792,400 cal and ΔH°f298(NaF) = −137,530 cal. The latter is in excellent agreement with the most recent critical assessment.  相似文献   

12.
The standard Gibbs energies of formation of platinum-rich intermetallic compounds in the systems Pt-Mg, Pt-Ca, and Pt-Ba have been measured in the temperature range of 950 to 1200 K using solid-state galvanic cells based on MgF2, CaF2, and BaF2 as solid electrolytes. The results are summarized by the following equations: ΔG° (MgPt7) = −256,100 + 16.5T (±2000) J/mol ΔG° (MgPt3) = −217,400 + 10.7T (±2000) J/mol ΔG° (CaPt5) = −297,500 + 13.0T (±5000) J/mol ΔG° (Ca2Pt7) = −551,800 + 22.3T (±5000) J/mol ΔG° (CaPt2) = −245,400 + 9.3T (±5000) J/mol ΔG° (BaPt5) = −238,700 + 8.1T (±4000) J/mol ΔG° (BaPt2) = −197,300 + 4.0T (±4000) J/mol where solid platinum and liquid alkaline earth metals are selected as the standard states. The relatively large error estimates reflect the uncertainties in the auxiliary thermodynamic data used in the calculation. Because of the strong interaction between platinum and alkaline earth metals, it is possible to reduce oxides of Group ILA metals by hydrogen at high temperature in the presence of platinum. The alkaline earth metals can be recovered from the resulting intermetallic compounds by distillation, regenerating platinum for recycling. The platinum-slag-gas equilibration technique for the study of the activities of FeO, MnO, or Cr2O3 in slags containing MgO, CaO, or BaO is feasible provided oxygen partial pressure in the gas is maintained above that corresponding to the coexistence of Fe and “FeO.” Formerly Professor and Chairman, Department of Metallurgy, Indian Institute of Science Formerly Visiting Scientist, Department of Metallurgy, Indian Institute of Science  相似文献   

13.
The enthalpies of formation of liquid (Ga + Pd) alloys were determined by direct reaction calorimetry in the temperature range 1322 <T/K < 1761 and the molar fraction range 0 <x Pd < 0.87. The enthalpies are very negative with a minimum Δmix H m = −70.4 ± 3.0 kJ mol-1 atx Pd = 0.6, independent of the temperature. Limiting partial molar enthalpies of palladium and gallium were calculated as Δh m (Ga liquid in ∞liquid Pd) = −265 ± 10 kJ mol−1 and Δh m (Pd liquid in ∞liquid Ga) = -144 ± 5 kJ mol−1. The integral molar enthalpy is given by Δmix H m =x(1-x) (-143.73 -232.47x + 985.77x 2-4457.8.x 3 + 6161.1x 4 + 2577.4x 5), wherex = x Pd. Moreover, values for the enthalpies of formation and fusion of PdGa, Pd2Ga, and the solid solution (withx Pd = 0.8571) have been proposed. These results have been discussed taking into account the equilibrium phase diagram. Formerly Ph.D. student, Université de Provence  相似文献   

14.
The standard enthalpy of formation of Sc5Si3 has been determined by solute-solvent drop calorimetry at (1473±2) K. The following value is reported: ΔH f o (mean)=−(719.1±34.0) kJ mol−1. This result is compared with corresponding published values for the enthalpies of formation of Me5Si3, with Me=Mn, Cr, V, Ti. This comparison shows regularly increasing negative enthalpies of formation from Mn5Si3 to Sc5Si3. LETTTIA TOPOR, formerly Senior Research Associate, The James Franck Institute, The University of Chicago,  相似文献   

15.
High temperature thermodynamic data for equilibria in the Ca-S-O, Mg-S-O, and La-S-0 systems were determined by a galvanic cell technique using calcia stabilized zirconia (CSZ) solid electrolytes. The measured emf data were used to calculate the standard free energy changes of the following reactions: [1] CaO(s) + 1/2S2(g) → CaS(s) + 1/2O2(g) 1000 to 1350 K ΔG° = 21906.9 − 0.8T(K)(±400 cal) = 91658 − 3.37 (±1700 J) [2] CaS(s) + 2O2(g) → CaSO4(s) 1050 to 1450 K ΔG° = -227530.7 + 80.632T(K) (±400 cal) = -951988.5 + 337.4T (±1700 J) [3] CaO(s) + 3/2O2(g) + 1/2S2(g) → CaSO4(s) 1050 to 1340 K ΔG° = -204892.7 + 79.83T(K)(±400 cal) = -857271.1 + 334.0T (±1700 J) [4] MgO(s) + 1/2S2(g) → MgS(s) + 5O2(g) 1000 to 1150 K ΔG° = 45708.6 − 2.897(K)(±500 cal) = 191244.8 − 12.1T (±2100 J) [5] La2O3(s) + 1/2S2(g) → La2O2S(s) + 1/2O2(g) 1080 to 1350 K ΔG° = 17507 − 2.32T(K)(±380 cal) = 73249.3 − 9.7T (±1600 J) [6] La2O3S(s) + S2(g) → La2S3(s) + O2(g) 950 to 1120 K ΔG° = 70940 + 2.25T(K)(±500 cal) = 296812.9 + 9.47 (±2100 J) The ΔG° values of reaction [5] were combined with the literature data for ΔG°f(La2O3) to obtain the standard free energy of formation of La2O2S at high temperatures. The values of ΔG°f thus calculated for La2O2S were combined with the ΔG° data for reaction [6] to obtain the standard free energy of formation of La2S3 at high temperatures.  相似文献   

16.
The decomposition equilibria of platinum dichloride have been found to consist of two decomposition steps, with chlorine molecules being the vapor species for both steps. An intermediate metastable PtCl solid is formed in the first step in addition to platinum metal and chlorine molecules. The platinum dichloride decomposes incongruently, the stepwise decomposition being PtCl2 → PtCl → Pt. The PtCl2 decomposition reactions consist of PtCl2(s) = PtCl (metastables) + 1/2 Cl2 (g) and PtCl2(s) = Pt(s) + Cl2 (g). The sum of the third lawΔH D, 298 K for the above two reactions is 214.637 ± 1.963 kJ/mole, in very good agreement with the second law ΔHD, 298 K = 215.107 ± 13.062 kJ/mole. The second decomposition step is given by the reaction 2PtCl (metastables) = 2Pt(s) + Cl2 (g) with a third law ΔHD, 298 K = 127.356 ± 0.791 kJ/mole, in excellent agreement with the second law ΔHD, 298 K = 127.509 ± 6.154 kJ/mole. The calculated heat of formation of PtCl2 is -139 ± 2 kJ/mole and that of PtCl is -63 ± 1 kJ/mole. Formerly Graduate Assistant. Formerly Undergraduate Research Helper,  相似文献   

17.
Standard molar enthalpies of formation of MeAl (Me = Ru,Rh, Os,Ir)   总被引:2,自引:0,他引:2  
The standard molar enthalpies of formation of RuAl, RhAl, and IrAl have been determined by the direct combination method using a high-temperature calorimeter operated at (1473 ±2) K. The following values are reported: ΔH f o (RuAl) = −(124.1 ± 3.3) kJ/mol; ΔH f o (RhAl) =-(212.6 ± 3.2) kJ/mol; and ΔH f o (IrAl) = -(185.5 ± 3.5) kJ/mol. For OsAl, an approximate value is −77 kJ/mol. The results are compared with available data for related alloys and with predicted values.  相似文献   

18.
The equilibrium 3/(1 −x)Fe1−x S(s) + (5 − 2x)/(1 −x)O2(g) Fe3O4(s) + 3/(1 −x)SO2(g) was studied in the temperature interval 850 to 1275 K by measuring oxygen potentials in a galvanic cell containing calcia stabilized zirconia as solid electrolyte. The SO2 activity was controlled by equilibrating the solid phases pyrrhotite and magnetite with a continuously flowing SO2-Ar gas mixture of known composition. Formation of S2 gas was taken into account and a recently published thermodynamic model for the pyrrhotite phase4 was used to derive the Gibbs energy change for the pyrrhotite-magnetite equilibrium and for the formation of Fe1−x S as a function of the variables temperature and pyrrhotite composition.  相似文献   

19.
The pressure of sodium existing over a mixture of aluminum and NaF has been measured by a gas-transference method over the range 635° to 816°C. The results (corrected for the presence of Na2) give for the reaction 6NaF(s) + A1(l) =Na3AlF6(s) + 3Na(g) ΔH°298 = +107,970 ± 220 cal (standard deviation) or ±60 cal (standard error). The corresponding activities of Na(l) may be expressed by log aNa = −2,854/T − 0.853 log T + 4.303 The sodium content of aluminum in equilibrium with NaF(s) and Na3AlF6(s) has been determined over the range 679° to 876°C. The activity coefficient of sodium in aluminum is given byRT In γNa/n 2 Al = 8290 + 3.73 T The present results are not consistent with the suggestion that Na2F is an important gaseous species in this system.  相似文献   

20.
The free energy of mixing in the Mn-P melts in the composition range ofX p = 0.0 to 0.333 was estimated by coupling the phase boundary information with reliable ΔG° formation for the Mn2P phase. This information was used to obtain the dilute solution properties of P in Mn. P(l,pure) = P(l,Henrian, Mn) ΔG °(Joules) = -203,611.39 + 41.003T The free energy is shown to be more negative than in the Fe system, reflecting a stronger interaction between Mn and P atoms than between Fe and P atoms. Presenting the activity coefficient of P with the expression used by Lupis and Elliott, the first and second interaction coefficients are obtained as follows: ε P P (Mn) = 10.538 + 9728.14/T ρ P P (Mn) = 28.148 + 9101.83/T The Gibbs free energy of formation for Mn3P was estimated in the temperature range of {dy1233} to {dy1378} K to be 3Mn l + P(l = Mn3P(s ΔG °(Joules) = -241,461.65 + 65.031T  相似文献   

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