Messages

Thank you very much for your prompt assistance. I sincerely appreciate it.
I'm conducting an isenthalpic calculation: adding a small amount of new magma (new_magma.melts) to a shallow magma chamber (Initial.melts).（A small amount of magma from the deep magma chamber has replenished the shallow magma chamber.）
Following your advice, I gave it a try:
env.txt
ALPHAMELTS_VERSION MELTS
ALPHAMELTS_MODE isenthalpic
ALPHAMELTS_CELSIUS_OUTPUT true
ALPHAMELTS_ASSIMILATE true
ALPHAMELTS_FRACTIONATE_SOLIDS true
ALPHAMELTS_DO_TRACE true
ALPHAMELTS_DO_TRACE H2O true
ALPHAMELTS_TRACE_INPUT_FILE new_trace_data.txt
ALPHAMELTS_SAVE_ALL true


Steps：
-f -----env.txt
1------Initial.melts
3-----1--Superliquidus
12----new_magma.melts-------1--Mix traces and majors
                       20----Mass ...... added     ###Is that correct?
          Tip:  Old reference Enthalpy (H0): not set yet
                   Old total Enthalpy: -1.18037e+006
4------1--Superliquidus
0------Number of assimilant MELTS files (or '0' for binary input file)
1------Mass of enriching agent to be added in grams per cycle1
           Assimilant filename        ###I don't understand here.

       ###Do I need files for many different minerals here? I saw the discussion on "isenthalpic AFC" in the forum(2012). I don't have these files. What should I do?
After completing the isenthalpic mixing, I want to continue by allowing the mixed magma to undergo fractional crystallization under isobaric conditions. Do you have any suggestions?  Unfortunately, I'm stuck at the stage of isenthalpic mixing.My idea is to use the output from the successful mixing as the initial composition for a fractional crystallization simulation under isobaric conditions.

I have two more questions:
(1) Can Alphamelts simulate magnetite crystallization? The results I obtained were rhm-oxide. Is this ilmenite? If Alphamelts can simulate magnetite, how should I set it up?

(2) Can only integer oxygen fugacities be simulated? For example, +1FMQ, +2FMQ, but not +0.5FMQ? When I used non-integer oxygen fugacities, only liquid_0 and olivine_0 appeared, and no other minerals.

Thank you so much for your time and effort. I extend my best wishes to you!

Hello, I want to simulate the enrichment process of a trace element in minerals after magma mixing using Alphamelts 1.9 on Windows. The scenario involves mixing a 1200°C magma with a 1180°C magma in a 0.3:0.7 ratio. Both magmas have identical compositions, including H2O and trace elements. However, during the mixing calculation, I consistently encounter errors related to the reference enthalpy settings. Even after adjusting the enthalpy values, the simulation fails. I've tried debugging parameters like temperature, pressure, and oxygen fugacity (fO2) but the problem persists. I'm at my wit's end and urgently need assistance. Below are the steps I followed:
env
ALPHAMELTS_VERSION MELTS
ALPHAMELTS_MODE isenthalpic
ALPHAMELTS_CELSIUS_OUTPUT true
ALPHAMELTS_FLUX_MELTING true
ALPHAMELTS ASSIMILATE=0.3
ALPHAMELTS_ASSIMILATE_FILE=Enrichment.melts
ALPHAMELTS_FRACTIONATE_SOLIDS true
ALPHAMELTS_DO_TRACE true
ALPHAMELTS_DO_TRACE H2O true
ALPHAMELTS_TRACE_INPUT_FILE new_trace_data.txt
ALPHAMELTS_SAVE_ALL true


Initial.melts：
Initial Composition: SiO2 45.4076
Initial Composition: TiO2 4.10505
Initial Composition: Al2O3 15.9333
Initial Composition: Cr2O3 0.00
Initial Composition: FeO 10.6709
Initial Composition: Fe2O3 2.14495
Initial Composition: MnO 0.2072
Initial Composition: MgO 5.5787
Initial Composition: CaO 9.62144
Initial Composition: Na2O 3.59729
Initial Composition: K2O 1.26834
Initial Composition: P2O5 0.918457
Initial Composition: H2O 0.5467
Initial Temperature: 1130.00
Initial Pressure: 1000.00
Initial Trace: Sc 26.6834
Initial Trace: Ni 1.72881
log fo2 Path: FMQ

Enrichment.melts
Initial Composition: SiO2 41.8471
Initial Composition: TiO2 5.23912
Initial Composition: Al2O3 14.5134
Initial Composition: Cr2O3 0.008769
Initial Composition: FeO 14.8942
Initial Composition: Fe2O3 2.1862
Initial Composition: MnO 0.172914
Initial Composition: MgO 6.81381
Initial Composition: CaO 9.53249
Initial Composition: Na2O 3.0196
Initial Composition: K2O 1.0099
Initial Composition: P2O5 0.762578
Initial Composition: H2O 0.0
Initial Temperature: 1200.00
Initial Pressure: 1000.0
Initial Trace: Sc 24.7462
Initial Trace: Ni 3.52352
log fo2 Path: FMQ

-f-----1------3-----1 Superliquidus ------12----1  Mix traces and majors----Mass proportion 0.3

Old reference Enthalpy (H0): not set yet
Old total Enthalpy: -1.18037e+006
and over
..............................

I have tried manually inputting the enthalpy values and other steps, but all attempts have failed，I really need your help.Looking forward to your suggestions!

Hi Paul,
The software you have developed is excellent and has greatly assisted me in understanding magmatic processes. However, I have encountered some issues during the operation that require your help.

I am a student who has recently been using alphaMELTS to simulate the mobility of the Sc (Scandium) element in layered mafic–ultramafic intrusions. That is, the process of Sc enrichment from a deep magma chamber (5kbar) to near the surface (1 kbar) and ultimately into different minerals (e.g., Cpx, Ilm, Amp).

I have already attempted simulation in the deep magma chamber under isobaric conditions, with an initial composition of Sc at 37.41 ppm. At the end of the simulation, only Cpx showed enrichment of Sc (26 ppm), and other minerals (e.g. Ilm, Amp) did not exhibit enrichment of Sc.

I also tried changing the partition coefficient of Sc in clinopyroxene (D=0.51 to 4), modifying it directly from the default_trace_data.txt file, but it did not work. The exported results show the partition coefficient fluctuating between 0.49xxxx and 0.51xxxx, which is not the value I set.

I would like to ask:
(1) Can the simulation of Sc enrichment in other minerals be performed? (e.g., Ilm, Amp) I saw a post on the forum mentioning that "the system cannot simulate Co and Ni because the partition coefficients of these elements in Ol/Cpx/Opx are unstable............" Is Sc subject to the same issue?
(2) If I want to simulate both major and trace elements, especially the enrichment trends of some key metallic elements, do you have any suggestions?
(3) There are some teaching videos on YouTube from a few years ago, which are basically for macOS and Linux OS. Since my computer operates on Windows, are there any teaching videos suitable for Windows users?


Best wishes,
Jimmy Young