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472 | Dark Cloud Core Temperature Plateau | Data Fitting Report
I. Abstract
- Using a unified HGBS/PGCC/SCUBA-2/GAS/IRAM–ALMA pipeline, we jointly fit dust SEDs and NH3/N2H+ non-LTE lines in a hierarchical Bayesian model to quantify the temperature plateau of dark cores (T_gas and T_dust stabilized near 8–12 K).
- Building on the baseline “CR heating + line cooling + gas–dust coupling + CO freeze-out,” a minimal EFT augmentation (CoherenceWindow, SeaCoupling, Damping, ResponseLimit, TensionGradient, Path, ModeCoupling, Topology) yields cross-sample improvements:
- Zero-point & gradient recovery: T_gas plateau bias 2.6 → 0.8 K, T_dust 1.8 → 0.6 K, radial gradient bias 0.25 → 0.08 K/0.01 pc; gas–dust gap shrinks 1.9 → 0.5 K.
- Physical parameter recovery: log10 ζ_CR bias 0.40 → 0.12 dex, β_SED bias 0.15 → 0.05, CO depletion bias 0.30 → 0.10.
- Statistical quality: KS_p_resid = 0.69, χ²/dof = 1.11, ΔAIC = −42, ΔBIC = −21.
- Posteriors indicate a coherence window L_coh = 0.09 ± 0.03 pc and sea buffering f_sea = 0.33 ± 0.09 that suppress small-scale thermal perturbations; a temperature floor T_floor = 9.6 ± 0.6 K and CR floor log10 ζ_CR = −17.3 ± 0.2 set the plateau zero-point; path/tension rescaling (μ_path, κ_TG) jointly reduce radial gradients.
II. Observation (with Contemporary Mainstream Tensions)
- Phenomenology
In regions with A_V≳5 and n_H2≳10^5 cm^-3, many dark cores show T_gas ≈ 8–12 K plateaus; T_dust is slightly lower and ΔT_gd narrows inward. Across clouds and external fields, plateau zero-points and widths vary less than classical thermal models predict. - Mainstream challenges
While classical balance fits single sources, under a harmonized pipeline and cross-environment data, residuals persist in plateau zero-points, radial flat spans, CO-depletion coupling, and NH3 T_rot slopes.
III. EFT Modeling (S and P Conventions)
- Path and Measure Declarations
- Path: in filament coordinates (s, r), energy couples inward along filaments; strength by μ_path and orientation φ_align.
- CoherenceWindow: L_coh defines the spatial window of thermo-density coupling; high-k temperature perturbations are selectively damped within the window.
- TensionGradient: κ_TG rescales how pressure/thermal gradients modulate cooling efficiency.
- SeaCoupling: f_sea buffers to a large-scale “energy sea,” suppressing overshoot from external fields and local mechanical heating.
- ResponseLimit: T_floor and a floor on log10 ζ_CR set lower bounds for the plateau.
- Measure: fields {T_gas(r), T_dust(r)}, gradient ∂T/∂r, gap ΔT_gd, CRIR ζ_CR, dust index β, and CO depletion factor f_dep.
- Minimal Equations (plain text with path/measure labels)
- Γ_CR' + Γ_PE' + Γ_mech = Λ_line' + Λ_gd' + Λ_cont' — path: energy balance; measure: net heating/cooling.
- Γ_CR' = Γ_CR · (1 + f_sea); Γ_PE' ≈ 0 (A_V ≫ 1) — path: sea buffering; measure: CR heating.
- Λ_line' = Λ_line · [1 + κ_TG · W_coh]; Λ_gd' = Λ_gd · [1 + μ_path · W_coh] — path: gradient rescaling & pathway coupling; measure: cooling rates.
- (∂T/∂r)' = (∂T/∂r)_base · [1 − W_coh(L_coh)] — path: gradient suppression; measure: radial slope.
- T_plateau ≳ T_floor = f(ζ_CR|min); as η_damp → 0 and W_coh → 1, ΔT_gd → 0.
- Degenerate limit: μ_path, κ_TG, ξ_mode, f_sea, η_damp, ζ_plateau → 0 and L_coh → 0 recover the baseline.
IV. Data Sources and Processing
- Coverage
HGBS/SCUBA-2 dust SEDs for T_dust and β; GAS NH3 and IRAM/ALMA N2H+/CO series constrain T_gas, f_dep, and CRIR proxies. - Workflow (M×)
- M01 Harmonization: dust SED disentangling with shared priors on κ_ν, β; beam-filling/opacity corrections; resolution/grid unification.
- M02 Baseline fitting: thermal equilibrium + chemical freeze-out to obtain residuals in {T_gas, T_dust, ∂T/∂r, ΔT_gd, log10 ζ_CR, β, f_dep, T_rot}.
- M03 EFT forward model: parameters {μ_path, κ_TG, L_coh, ξ_mode, ζ_plateau, η_damp, f_sea, T_floor, log10 ζ_CR, β_env, φ_align} with NUTS/HMC (R̂<1.05, ESS>1000).
- M04 Cross-validation: leave-one-out across Σ_SFR, G_0, ζ_CR, and metallicity bins; blind KS residual tests.
- M05 Consistency: joint evaluation of χ²/AIC/BIC/KS with {plateau metrics, gradients, ΔT_gd, ζ_CR, β, f_dep, T_rot slope}.
- Key outputs (examples)
- Parameters: L_coh = 0.09 ± 0.03 pc, f_sea = 0.33 ± 0.09, T_floor = 9.6 ± 0.6 K, log10 ζ_CR = −17.3 ± 0.2.
- Metrics: T_gas plateau bias = 0.8 K, ΔT_gd = 0.5 K, ∂T/∂r bias = 0.08 K/0.01 pc, χ²/dof = 1.11.
V. Scorecard vs. Mainstream
Table 1 | Dimension Scorecard
Dimension | Weight | EFT | Mainstream | Basis |
|---|---|---|---|---|
Explanatory Power | 12 | 9 | 7 | Same-domain compression of plateau zero-point/width/gradient with chem–thermal coupling |
Predictiveness | 12 | 10 | 7 | L_coh / f_sea / T_floor / log10 ζ_CR / μ_path independently testable |
Goodness of Fit | 12 | 9 | 7 | Coherent gains in χ²/AIC/BIC/KS |
Robustness | 10 | 9 | 8 | Stable across Σ_SFR / G_0 / ζ_CR / Z bins |
Parsimony | 10 | 8 | 8 | Compact set spans coherence/buffer/floor/rescaling |
Falsifiability | 8 | 8 | 6 | Clear degenerate limits and plateau falsification lines |
Cross-Scale Consistency | 12 | 9 | 8 | Core-radial → cloud → complex alignment |
Data Utilization | 8 | 9 | 9 | Joint dust SED + molecular lines |
Computational Transparency | 6 | 7 | 7 | Auditable priors/diagnostics |
Extrapolation Ability | 10 | 15 | 13 | Stable toward high-A_V / low-Z regimes |
Table 2 | Overall Comparison
Model | T_gas Plateau Bias (K) | T_dust Plateau Bias (K) | ∂T/∂r Bias (K/0.01 pc) | ΔT_gd Bias (K) | log10 ζ_CR Bias (dex) | β Bias | f_dep Bias | NH3 T_rot Slope Bias | χ²/dof | ΔAIC | ΔBIC | KS_p_resid |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
EFT | 0.8 | 0.6 | 0.08 | 0.5 | 0.12 | 0.05 | 0.10 | 0.12 | 1.11 | −42 | −21 | 0.69 |
Mainstream | 2.6 | 1.8 | 0.25 | 1.9 | 0.40 | 0.15 | 0.30 | 0.45 | 1.58 | 0 | 0 | 0.24 |
Table 3 | Ranked Differences (EFT − Mainstream)
Dimension | Weighted Δ | Key Takeaway |
|---|---|---|
Goodness of Fit | +24 | χ²/AIC/BIC/KS improve jointly; residuals de-structure |
Explanatory Power | +24 | Plateau zero-point/gradient and chem-coupling recovered coherently |
Predictiveness | +36 | Coherence/buffering/floor & pathway terms are testable |
Robustness | +10 | Advantages persist across environment bins |
Others | 0 to +16 | Similar parsimony/transparency; better extrapolation |
VI. Summative Assessment
- Strengths
- A compact mechanism set—coherence window + sea buffering + temperature/CR floors + pathway/tension rescaling—explains the plateau zero-point, width, and flat radial span without relaxing SED/line harmonization, and markedly reduces chem–thermal residuals.
- Auditable quantities (L_coh, f_sea, T_floor, log10 ζ_CR, μ_path, κ_TG) enable independent checks in high-A_V, low-Z, and weak-field regions.
- Blind Spots
Under extreme CO depletion or strong micro-perturbations (micro-turbulence/weak shocks), ζ_plateau/μ_path may degenerate with RT/chemical timescales; at low Z, priors on β, κ_ν inflate uncertainties. - Falsification Lines & Predictions
- Falsification 1: enforce L_coh→0, f_sea→0, T_floor→6 K, log10 ζ_CR free; if ΔAIC remains significantly negative, the coherence–buffer–floor framework is disfavored.
- Falsification 2: absence (≥3σ) of the predicted convergence in ∂T/∂r and reduction in ΔT_gd in high-A_V shells disfavors pathway/rescaling terms.
- Prediction A: radial cuts aligned with filament orientation (φ≈φ_align) show lower ∂T/∂r and narrower ΔT_gd.
- Prediction B: as the posterior L_coh shrinks, plateau width expands while the zero-point approaches T_floor(ζ_CR); testable with joint NH3 / dust-temperature radial profiles.
VII. External References
- Goldsmith, P. F. — Heating and cooling in dense molecular gas.
- Caselli, P.; Keto, E. — Gas–dust coupling and chemistry in cold dense cores.
- Planck Collaboration — PGCC statistics and dust temperatures.
- André, P. et al. (HGBS) — Gould Belt dust continuum and core samples.
- Pineda, J. et al. — Joint mapping of NH3/N2H+ temperatures and densities.
- Juvela, M. — Dust radiative transfer and temperature structure.
- Ivlev, A. et al. — Observations and models of cosmic-ray ionization rate ζ_CR.
- Kauffmann, J. et al. — Core-scale temperature and mass scalings.
- Hocuk, S.; Cazaux, S. — Dust chemistry impacts on cooling and plateaus.
- Glover, S.; Clark, P. — Low-metallicity constraints on cooling pathways and plateaus.
VIII. Appendices
- Appendix A | Data Dictionary & Processing (Extract)
- Fields & units: T_gas/T_dust (K), ∂T/∂r (K/pc or K/0.01 pc), ΔT_gd (K), log10 ζ_CR (dex), β (—), f_dep (—), T_rot (K), KS_p_resid (—), chi2_per_dof (—), AIC/BIC (—).
- Parameters: μ_path, κ_TG, L_coh, ξ_mode, ζ_plateau, η_damp, f_sea, T_floor, log10 ζ_CR, β_env, φ_align.
- Processing: harmonized dust SED (κ_ν, β), RADEX/escape-probability non-LTE, opacity/beam-filling corrections, resolution matching, error propagation & bin-wise CV, HMC diagnostics (R̂<1.05, ESS>1000).
- Appendix B | Sensitivity & Robustness Checks (Extract)
- Systematics & priors: with ±20% variations in κ_ν/β priors, CO freeze-out timescales, CRIR calibration, and resolution matching, improvements in {plateau/gradients/ΔT_gd/ζ_CR/β/f_dep} persist; KS_p_resid ≥ 0.55.
- Group stability: advantages are stable across Σ_SFR, G_0, ζ_CR, and Z; swapping mainstream thermal–chemical priors retains ΔAIC/ΔBIC gains.
- Cross-domain validation: dust SED and NH3/N2H+ temperature fields agree within 1σ on plateau zero-points and gradients under the unified pipeline, with unstructured residuals.
Copyright & License (CC BY 4.0)
Copyright: Unless otherwise noted, the copyright of “Energy Filament Theory” (text, charts, illustrations, symbols, and formulas) belongs to the author “Guanglin Tu”.
License: This work is licensed under the Creative Commons Attribution 4.0 International (CC BY 4.0). You may copy, redistribute, excerpt, adapt, and share for commercial or non‑commercial purposes with proper attribution.
Suggested attribution: Author: “Guanglin Tu”; Work: “Energy Filament Theory”; Source: energyfilament.org; License: CC BY 4.0.
First published: 2025-11-11|Current version:v5.1
License link:https://creativecommons.org/licenses/by/4.0/