SUBROUTINE BHEZ(ID) C ================== C C The part of matrices A and B corresponding to the hydrostatic C equilibrium equation, C i.e. the (NFREQE+INHE)-th row; C C Input: ID - depth index C INCLUDE 'IMPLIC.FOR' INCLUDE 'BASICS.FOR' INCLUDE 'ATOMIC.FOR' INCLUDE 'MODELQ.FOR' INCLUDE 'ARRAY1.FOR' INCLUDE 'ALIPAR.FOR' COMMON/SURFEX/EXTJ(MFREQ),EXTH(MFREQ) C NHE=NFREQE+INHE NRE=NFREQE+INRE NPC=NFREQE+INPC NZD=NFREQE+INZD NSE=NFREQE+INSE-1 c if(inhe.le.0) return IJ1=1 C C *********** Linearized equation for the fictitious massive particle C density C IF(INMP.GT.0) THEN NMP=NFREQE+INMP B(NMP,NMP)=-UN B(NMP,NHE)=UN IF(INPC.GT.0) B(NMP,NPC)=-UN END IF C C *********** Linearized hydrostatic equilibrium C HEXT=0. HEXN=0. GRD=0. FLUXW=0. DO I=1,NLVEXP HEX(I)=0. END DO C IF(ID.GT.1) GO TO 50 C C *** Upper boundary condition (ID=1) C C 1. possibility - the same as in stellar atmospheres C Basically, linearized eq. (7-10) of Mihalas (1978) C IF(IBCHE.EQ.0) THEN X1=PCK/DENS(ID) IF(NFREQE.GT.0) THEN DO IJ=IJ1,NFREQE IJT=IJFR(IJ) IF(.NOT.LSKIP(ID,IJT)) THEN FLUXW=W(IJT)*(FH(IJT)*RAD0(IJ)-HEXTRD(IJT)) GRD=GRD+FLUXW*ABSO0(IJ) HEXN=HEXN+FLUXW*DABN0(IJ) HEXT=HEXT+FLUXW*DABT0(IJ) DO I=1,NLVEXP HEX(I)=HEX(I)+FLUXW*DRCH0(I,IJ) END DO C C Columns corresponding to mean intensities C B(NHE,IJ)=X1*WDEP0(IJ)*FH(IJT)*ABSO0(IJ) END IF END DO END IF C RTN=X1*WMM(ID)/DENS(ID)*(GRD+FPRD(ID)) VT0=HALF*VTURB(ID)*VTURB(ID)/DM(ID)*WMM(ID) C C columns corresponding to total particle density, fictitious C massive particle density, temperature, and electron density, C respectively C B(NHE,NHE)=BOLK*TEMP(ID)/DM(ID)-GN*(RTN-VT0) IF(INMP.GT.0) B(NHE,NFREQE+INMP)=GP*(VT0-RTN) IF(INRE.GT.0) THEN B(NHE,NRE)=BOLK*PSI0(NHE)/DM(1)+X1*(HEXT+HEIT(ID)) C(NHE,NRE)=X1*HEITP(ID) END IF IF(INPC.GT.0) THEN B(NHE,NPC)=X1*(HEXN+HEIN(ID))+GN*(RTN-VT0) C(NHE,NPC)=X1*HEINP(ID) END IF C C Columns corresponding to populations C DO II=1,NLVEXP B(NHE,NSE+II)=B(NHE,NSE+II)+X1*(HEX(II)+HEIP(II,ID)) C(NHE,NSE+II)=C(NHE,NSE+II)+X1*HEIPP(II,ID) END DO C C The rhs vector also accounts for the total radiation pressure in C the fixed-option transitions (array FPRD) C GRAV=QGRAV*ZD(1) VECL(NHE)=GRAV-BOLK*TEMP(ID)*PSI0(NHE)/DM(ID)- * X1*(GRD+FPRD(ID))-VT0/WMM(ID)*DENS(ID) C RETURN ELSE IF(IBCHE.EQ.1) THEN C C 2. possibility - specifically disk - Hubeny (1990), Eq. (4.19) C newer variant C IF(NFREQE.GT.0) THEN DO IJ=IJ1,NFREQE IJT=IJFR(IJ) IF(.NOT.LSKIP(ID,IJT)) THEN FLUXW=W(IJT)*(FH(IJT)*RAD0(IJ)-HEXTRD(IJT)) GRD=GRD+FLUXW*ABSO0(IJ) HEXN=HEXN+FLUXW*DABN0(IJ) HEXT=HEXT+FLUXW*DABT0(IJ) DO I=1,NLVEXP HEX(I)=HEX(I)+FLUXW*DRCH0(I,IJ) END DO END IF END DO END IF c CCC=PCK/QGRAV HR1=CCC*(GRD+FPRD(1))/DENS(1) PG1=BOLK*PSI0(NHE)*TEMP(1) HG1=SQRT(TWO*PG1/DENS(1)/QGRAV) X=(ZD(1)-HR1)/HG1 IF(X.LT.3.) THEN IF(X.LT.0.) X=0. F1=8.86226925D-1*EXP(X*X)*ERFCX(X) ELSE F1=HALF*(UN-HALF/X/X)/X END IF X1=X*1.01 F1D=0. IF(X1.LT.3.) THEN F1D=8.86226925D-1*EXP(X1*X1)*ERFCX(X1) ELSE F1D=HALF*(UN-HALF/X1/X1)/X1 END IF IF(X.GT.0.) F1D=(F1D-F1)*100./X GGG=DENS(1)*HG1*F1 RF1=DENS(1)*F1D CCD=CCC*F1D C DO IJ=1,NFREQE B(NHE,IJ)=-CCD*WDEP0(IJ)*FH(IJFR(IJ))*ABSO0(IJ) END DO C C columns corresponding to total particle density and temperature C B(NHE,NHE)=B(NHE,NHE)+(GGG+HR1*RF1)/PSI0(NHE) IF(INRE.GT.0) B(NHE,NRE)= * (GGG-RF1*ZD(1)+RF1*HR1)*HALF/TEMP(1)-CCD*(HEXT+HEIT(ID)) IF(INZD.GT.0) B(NHE,NZD)=RF1 IF(INPC.GT.0) B(NHE,NPC)=-CCD*(HEXN+HEIN(ID)) DO II=1,NLVEXP B(NHE,NSE+II)=-CCD*(HEX(II)+HEIP(II,ID)) END DO C C The rhs vector C VECL(NHE)=DM(1)-GGG RETURN ELSE IF(IBCHE.EQ.2) THEN C C 3. possibility - specifically disk - Hubeny (1990), Eq. (4.19) C older variant C IF(NFREQE.GT.0) THEN DO IJ=IJ1,NFREQE IJT=IJFR(IJ) IF(.NOT.LSKIP(ID,IJT)) THEN FLUXW=W(IJT)*(FH(IJT)*RAD0(IJ)-HEXTRD(IJT)) GRD=GRD+FLUXW*ABSO0(IJ) END IF END DO END IF CCC=PCK/QGRAV PR1=CCC*(GRD+FPRD(1))/DENS(1) PG1=BOLK*PSI0(NHE)*TEMP(1) HG1=SQRT(TWO*PG1/DENS(1)/QGRAV) X=(ZD(1)-PR1)/HG1 IF(X.LT.3.) THEN IF(X.LT.0.) X=0. F1=8.86226925D-1*EXP(X*X)*ERFCX(X) ELSE F1=HALF*(UN-HALF/X/X)/X END IF GGG=HG1*QGRAV*HALF/F1 C C columns corresponding to total particle density and temperature C B(NHE,NHE)=BOLK*TEMP(1) IF(INRE.GT.0) B(NHE,NFREQE+INRE)=PG1/TEMP(1) C C The rhs vector C VECL(NHE)=DM(1)*GGG-PG1 RETURN ELSE C C 4. a simple form of the bounary condition P_gas(ID=1)=PGAS0, C where PGAS0 is an input parameter C B(NHE,NHE)=BOLK*TEMP(1) IF(INRE.GT.0) B(NHE,NRE)=BOLK*PSI0(NHE) VECL(NHE)=PGAS0-BOLK*TEMP(1)*PSI0(NHE) RETURN END IF C C *** Normal depth point (ID > 1) C C Columns (for matrices A and B) corresponding to mean intensities C 50 CONTINUE GRAV=QGRAV*(ZD(ID)+ZD(ID-1))*HALF GRAVZ=GRAV*(ZD(ID)-ZD(ID-1)) DGRV=GRAVZ*HALF*WMM(ID) GRD=0. IF(NFREQE.GT.0) THEN DO IJ=IJ1,NFREQE IF(.NOT.LSKIP(ID,IJFR(IJ))) THEN GRD=GRD+(FK0(IJ)*RAD0(IJ)-FKM(IJ)*RADM(IJ))*W(IJFR(IJ)) A(NHE,IJ)=-PCK*W(IJFR(IJ))*FKM(IJ) B(NHE,IJ)=PCK*W(IJFR(IJ))*FK0(IJ) END IF END DO END IF C VT0=HALF*VTURB(ID)*VTURB(ID)*WMM(ID) VTM=HALF*VTURB(ID-1)*VTURB(ID-1)*WMM(ID) C C columns corresponding to total particle density C A(NHE,NHE)=-BOLK*TEMP(ID-1)-GN*(VTM+DGRV) B(NHE,NHE)=BOLK*TEMP(ID)+GN*(VT0+DGRV) C C columns corresponding to temperature C IF(INRE.GT.0) THEN A(NHE,NRE)=-BOLK*PSIM(NHE)+PCK*HEITM(ID) B(NHE,NRE)=BOLK*PSI0(NHE)+PCK*HEIT(ID) C(NHE,NRE)=PCK*HEITP(ID) END IF C C columns corresponding to electron density C IF(INPC.GT.0) THEN A(NHE,NPC)=GN*(VTM+DGRV)+PCK*HEINM(ID) B(NHE,NPC)=-GN*(VT0+DGRV)+PCK*HEIN(ID) C(NHE,NPC)=PCK*HEINP(ID) END IF C C columns corresponding to NMP C IF(INMP.GT.0) THEN A(NHE,NFREQE+INMP)=-GP*(VTM+DGRV) B(NHE,NFREQE+INMP)=GP*(VT0+DGRV) END IF C C columns corresponding to populations C DO II=1,NLVEXP A(NHE,NSE+II)=A(NHE,NSE+II)+PCK*HEIPM(II,ID) B(NHE,NSE+II)=B(NHE,NSE+II)+PCK*HEIP(II,ID) C(NHE,NSE+II)=C(NHE,NSE+II)+PCK*HEIPP(II,ID) END DO C C the rhs vector C VECL(NHE)=-GRAVZ*(DENS(ID)+DENS(ID-1))*HALF- * BOLK*(TEMP(ID)*PSI0(NHE)-TEMP(ID-1)*PSIM(NHE))- * PCK*(GRD+FPRD(ID))- * VT0/WMM(ID)*DENS(ID)+VTM/WMM(ID)*DENS(ID-1) C RETURN END