{"id":"3c7bf048-1e78-4fc3-82c3-7c59cad8b971","arxiv_id":"2505.18567","paper_version":1,"verdict":"CONDITIONAL","confidence":"MODERATE","novelty_score":6.0,"correctness_risk":"medium","formal_verification":"none","parameter_count":0,"one_line_summary":"Partial exterior measurements stably determine the fractional conductivity, with logarithmic (resp. log-log) stability when conductivities agree in the exterior (resp. when their difference has compact support).","lead":"This mathematics paper proves the first partial-data stability estimates for a nonlocal version of the electrical impedance tomography problem, the fractional conductivity inverse problem. It shows that small differences in exterior measurements imply small differences in the reconstructed conductivity, with error growing only logarithmically (or log-log) in the measurement noise.","discovery_kind":"extension","skeptic_critique":{"model":"deepseek-v4-flash","headline":"Theorem 1.2 invokes CRTZ24 Prop. 4.1 under a regularity hypothesis that is not implied by the stated assumption m_i in H^{2s+epsilon,n/s}; a scaling argument shows the relevant Sobolev spaces are not nested.","rationale":"The paper's central contribution is a partial-data stability theory for the inverse fractional conductivity problem. For Theorem 1.1 the route is coherent: Lemma 3.3 and Lemma 3.6 reduce conductivity measurements to Schrodinger measurements, Theorem 3.1 (RS20) gives logarithmic stability from partial data for the reduced potentials, and Lemma 3.8 converts the potential difference back to the conductivity difference. I found no fatal objection in that chain. The product estimate in Lemma 3.4 is misstated as written, but it is easily repaired because the cut-off is C_c^infty, so multiplication by psi is bounded on H^s. The missing verification that zero is not a Dirichlet eigenvalue for the reduced operators also follows from the coercivity of the conductivity form together with the Liouville identity, so it is a fixable omission rather than a fatal flaw.\n\nThe load-bearing concern is in Theorem 1.2. The proof's key step is the estimate ||Lambda_{q1}-Lambda_{q2}|| <= omega(||Lambda_{gamma1}-Lambda_{gamma2}||_W), obtained by combining Theorem 3.1 and CRTZ24 Prop. 4.1. Proposition 4.1 has a regularity hypothesis involving the Besov-style space H^{(2s+epsilon)/theta0, theta0 n/s}, whereas the theorem only assumes H^{2s+epsilon,n/s}. These are not nested: the target space asks for more smoothness and weaker integrability simultaneously, and a scaling computation shows that no embedding H^{2s+epsilon,n/s}(R^n) -> H^{(2s+epsilon)/theta0, theta0 n/s}(R^n) exists for theta0<1. The proof does not acknowledge this mismatch or provide a replacement argument. This affects the log-log claim in Theorem 1.2, one of the two advertised main results.\n\nI want to be clear that this is a proof gap, not evidence that the theorem is false. The stability result may well hold under the stronger CRTZ24 regularity condition, or Prop. 4.1 may admit a proof under the weaker H^{2s+epsilon,n/s} assumption using the same ideas as Lemma 3.2. The omission is of the kind that can be corrected by adding condition (iii') to Theorem 1.2 and rerunning the same argument. Therefore the reader's CONDITIONAL verdict remains the right editorial position; my analysis does not move the verdict. I agree with the reader that the regularity mismatch is a central weak assumption, and I have isolated it as the single most load-bearing gap.","tokens_in":14260,"tokens_out":21375,"duration_ms":176626,"concrete_test":"Fix concrete parameters, e.g. n=3, s=1/4, epsilon=1/4, so Theorem 1.2 assumes m_i in H^{0.75,12}(R^3) while Prop. 4.1 with theta0=1/2 requires m_i in H^{1.5,6}(R^3). To settle the gap, test the embedding claim directly: for any nonzero m in the source space, consider m_lambda(x)=m(lambda x) and compare the homogeneous H^{a,p} and H^{b,q} norms as lambda varies. The ratio scales as lambda^{-(s+epsilon)(1/theta0-1)}, which is unbounded, so the claimed embedding fails. The authors would therefore need either to exhibit a different argument proving Prop. 4.1 with only H^{2s+epsilon,n/s} regularity, or to strengthen assumption (iii) of Theorem 1.2 to the CRTZ24 hypothesis and restate the theorem accordingly.","verdict_should_be":"UNCHANGED","load_bearing_attack":"The proof of Theorem 1.2 depends on the comparison estimate [CRTZ24, Prop. 5.1], restated as Prop. 4.1, which transfers the measured conductivity DN-map difference to the reduced Schrodinger DN-map difference. Prop. 4.1 requires, for some s/n < theta0 < 1 and some epsilon > 0, that the background deviations satisfy m_i in H^{(2s+epsilon)/theta0, theta0 n/s}(R^n). Theorem 1.2 only assumes m_i in H^{2s+epsilon,n/s}(R^n). These spaces are not comparable in the needed direction: writing a = 2s+epsilon and p = n/s, the target has smoothness b = a/theta0 > a and integrability q = theta0 n/s < p. On the level of homogeneous norms, H^{a,p} scales like lambda^{-n/p+a}, while H^{b,q} scales like lambda^{-n/q+b}, and here b - n/q = (s+epsilon)/theta0 > s+epsilon = a - n/p. Hence no embedding H^{a,p}(R^n) -> H^{b,q}(R^n) exists; the CRTZ24 hypothesis is strictly stronger. The paper does not supply a substitute argument: the sentence 'Repeating the argument in the proof of Proposition 3.7' only yields the H^{delta,n/(2s)}(Omega) bound on q_j, not the required H^{(2s+epsilon)/theta0, theta0 n/s} regularity of m_i. Since Prop. 4.1 is the only bridge from conductivity data to Schrodinger-potential data in Theorem 1.2, the log-log estimate is not established under the stated hypotheses. The omission is probably repairable by strengthening assumption (iii) or by proving Prop. 4.1 under the weaker H^{2s+epsilon,n/s} condition, but as written the proof has a real gap.","agreement_with_reader":"agree"},"referee_report":{"model":"deepseek-v4-flash","summary":"The paper studies the inverse fractional conductivity problem with partial exterior measurements. The authors prove two stability estimates: a logarithmic bound for conductivities that agree a priori in the whole exterior, and a log-log bound when the difference has compact support and measurements are taken on a single exterior set. The proofs use the fractional Liouville reduction to relate the conductivity DN map to the fractional Schrödinger DN map, then invoke known stability results of Rüland–Salo and of Covi–Railo–Tyni–Zimmermann. The paper also contains a self-contained proof that multiplication by gamma^{1/2} and gamma^{-1/2} preserves the space tilde H^s(U).","tokens_in":14583,"tokens_out":6477,"duration_ms":50402,"significance":"If the stated estimates hold, these are the first partial-data stability results for the fractional conductivity problem with the expected logarithmic and log-log rates, extending the full-data result of CRTZ24. The reduction strategy is elegant and Lemma 3.3 is a useful independent technical contribution. However, the proof of Theorem 1.2 relies on a regularity hypothesis in a quoted proposition that is not implied by the theorem's assumptions, and the non-eigenvalue condition required by the main Schrödinger stability theorem is never checked. Both issues are repairable, but as written the main claims are not fully established.","major_comments":[{"comment":"The proof of Theorem 1.2 invokes Proposition 4.1, quoted from CRTZ24 Proposition 5.1, to bound the Schrödinger DN-map difference in terms of the conductivity DN-map difference. Proposition 4.1 requires the background deviations to satisfy m_i in H^{(2s+epsilon)/theta_0, theta_0 n/s}(R^n) for some s/n < theta_0 < 1, whereas Theorem 1.2 assumes only m_i in H^{2s+epsilon, n/s}(R^n). These spaces are not nested in the needed direction: on the level of homogeneous norms, H^{a,p} scales as lambda^{-n/p+a} and H^{b,q} as lambda^{-n/q+b}, and here b - n/q = (s+epsilon)/theta_0 is larger than a - n/p = s+epsilon, so no embedding H^{2s+epsilon,n/s} into H^{(2s+epsilon)/theta_0, theta_0 n/s} exists. The sentence 'Repeating the argument in the proof of Proposition 3.7' only yields the H^{delta, n/(2s)} bound on q_j, not the required Sobolev regularity of the background deviations m_i. Since Proposition 4.1 is the only bridge from the conductivity data to the Schrödinger-potential data in this proof, the log-log stability estimate is not established under the stated hypotheses. This gap is repairable by either strengthening assumption (iii) of Theorem 1.2 to the CRTZ24 condition or by proving the comparison estimate under the weaker H^{2s+epsilon,n/s} regularity.","section":"Section 3, Proposition 3.7 and Theorem 3.1"},{"comment":"Theorem 3.1, which is the key input for Proposition 3.7, requires that zero is not a Dirichlet eigenvalue of the exterior value problem (-Delta)^s u + q_j u = 0 in Omega with u = 0 in Omega^e, for j = 1, 2. Proposition 3.7 states that 'It suffices to show that the conditions of Theorem 3.1 are met' and then verifies only the H^{delta,n/(2s)} bound on q_j. The non-eigenvalue condition is never stated, checked, or referenced for the reduced potentials q_j = -((-Delta)^s m_j)/gamma_j^{1/2}. Without this condition the DN maps Lambda_{q_j} are not known to be well-defined, and the stability estimate of Theorem 3.1 does not apply. Since the paper aims to use Theorem 3.1 as a black box, the missing verification is a load-bearing gap, though it may be filled by a perturbation argument or by imposing a smallness condition on the potentials.","section":"Section 3, Proposition 3.7"}],"minor_comments":[{"comment":"In the abstract, 'shaper' should be 'sharper'.","section":"Abstract"},{"comment":"The word 'furhter' should be 'further'.","section":"Introduction, page 1"},{"comment":"The typo 'non-emtpy' should be 'non-empty'.","section":"Section 2, Theorem 3.1 statement (page 7)"},{"comment":"The typo 'becuse' should be 'because'.","section":"Section 4, proof of Theorem 1.2 (page 13)"},{"comment":"The estimate ||phi_k^pm psi - gamma^{pm 1/2} psi||_{H^s} <= ||phi_k^pm - gamma^{pm 1/2} chi||_{H^s} ||psi||_{H^s} is not a direct consequence of the H^s multiplication because H^s is not an algebra. Since psi is fixed, smooth, and compactly supported, multiplication by psi is a bounded operator on H^s, so the argument survives with a constant depending on psi. The authors should state this to avoid giving the impression that the displayed inequality holds as written.","section":"Section 3, proof of Lemma 3.4, equation (5)"},{"comment":"The assumption supp(gamma_1 - gamma_2) = Sigma is an equality; if the authors intend only that the support is contained in Sigma, the condition should be stated as supp(...) subset Sigma to avoid measure-theoretic pedantry.","section":"Section 4, Theorem 1.2 condition (i)"},{"comment":"The proof works with p = 2n/(n-2s') for s' < s; the connection to an arbitrary p in the range stated in the theorem should be made explicit by choosing s' such that p < 2n/(n-2s') and then adjusting the constants.","section":"Section 4, proof of Theorem 1.2 (parameter p)"}],"recommendation":"major_revision","confidential_remarks":"The paper is a solid contribution to the inverse fractional conductivity literature. The main concerns are the regularity mismatch in the proof of Theorem 1.2 and the unchecked non-eigenvalue condition in the application of Theorem 3.1. Both are repairable within the manuscript's scope, so I recommend major revision rather than rejection. The paper is within the journal's scope and the references are appropriate."},"author_rebuttal":null,"desk_editor":{"model":"deepseek-v4-flash","letter":"First thing to know: this is a genuine step forward. It proves the first partial-data stability estimates for the fractional conductivity equation, with a logarithmic modulus under exterior agreement and log-log under compact support. The Liouville reduction chain is standard and mostly clearly written. The new Lemma 3.3 on multiplication preserving \\tilde H^s is useful, and the reliance on RS20 and CRTZ24 is legitimate — those are independent published results. I agree with the reader's overall assessment: the main ideas are right, and the gaps are repairable.\n\nNow the soft spots. In Proposition 3.7, the proof applies Theorem 3.1 (RS20) but never checks the condition that zero is not a Dirichlet eigenvalue for (−Δ)^s+q_j. That is a genuine hypothesis of the theorem, and the paper just asserts the reduced potentials satisfy the bounds. For a fixed conductivity this may be generic, but the theorem as stated covers all gamma in the class, so the proof is incomplete. This should be fixable by adding the non-eigenvalue assumption to the hypotheses or by an approximation argument.\n\nThe larger problem is in Theorem 1.2. The proof uses CRTZ24, Prop. 5.1 (restated as Prop. 4.1), which requires m_i ∈ H^{(2s+ε)/θ_0, θ_0 n/s} for some s/n<θ_0<1. The theorem only assumes m_i ∈ H^{2s+ε, n/s}. The stress-test note is right: the scaling exponents give (s+ε)/θ_0 > s+ε, so H^{2s+ε,n/s} is strictly larger than the needed space; there is no embedding in the right direction. The sentence “Repeating the argument in the proof of Proposition 3.7” only controls q_j, not m_i in the stronger space. Since this proposition is the only bridge from conductivity data to Schrödinger data in that theorem, the log-log estimate is not established under the stated hypotheses. The likely fix is to strengthen assumption (iii) or prove a variant of the comparison estimate under the weaker condition, but as written the proof has a real hole.\n\nMinor: Lemma 3.4 uses an inequality ‖φψ‖ ≤ ‖φ‖ ‖ψ‖ in H^s, which fails for s<n/2. The argument can be repaired by using continuity of multiplication by a fixed smooth compactly supported function, so this is not a serious issue.\n\nWho is this for? Researchers in fractional inverse problems, especially stability. It deserves a serious referee — the claims are new and plausible, and the gaps are identifiable and likely fixable. I recommend engaging with it, but the revision needs to address the non-eigenvalue condition and, more importantly, the regularity mismatch in Theorem 1.2.","headline":"First partial-data stability estimates for the fractional conductivity problem, but the proof of the log-log theorem uses a regularity hypothesis the stated assumptions don't imply.","tokens_in":15182,"tokens_out":5630,"would_cite":true,"duration_ms":42945,"reading_group":"yes","serious_thinker":"yes","would_accept_peer_review":true},"rs_alignment":null,"lean_confirmation":null,"pith_extraction":{"msc":["35R30","26A33","42B37"],"pacs":[],"model":"deepseek-v4-flash","headline":"Partial exterior measurements for the fractional conductivity problem determine the interior conductivity with logarithmic stability, and with log-log stability when the conductivities are not known outside the domain.","keywords":["fractional Laplacian","inverse conductivity problem","partial data","logarithmic stability","Liouville reduction","nonlocal inverse problem","stability estimates","Dirichlet-to-Neumann map"],"falsifier":"Verify whether the assumed $H^{2s+\\epsilon,n/s}(\\mathbb{R}^n)$ condition implies the weighted-space hypothesis $H^{(2s+\\epsilon)/\\theta_0,\\theta_0 n/s}$ used in the cited comparison proposition for every allowed $\\theta_0$; a counterexample for small $\\epsilon$ would expose a gap in the proof of Theorem 1.2, and a pair of conductivities achieving a slower-than-logarithmic rate would refute Theorem 1.1.","tokens_in":13981,"feed_emoji":"⚡","tokens_out":7081,"duration_ms":54357,"temperature":0.7,"pith_summary":"This paper proves that for the fractional, nonlocal analogue of the classical conductivity inverse problem, measurements taken only on bounded pieces of the exterior domain still control the conductivity inside the domain, with at most logarithmic loss of accuracy. If the two conductivities are known to agree in the whole exterior, the interior $H^s(\\Omega)$ difference is bounded by a power of the logarithm of the measurement error (Theorem 1.1). If their difference merely has compact support and they agree on the measurement set, the same conclusion holds in $L^p$ with a log-log modulus (Theorem 1.2). This matters because inverse imaging problems are typically unstable, and quantitative stability rates tell users how small measurement errors must be to resolve features at a given precision.","feed_headline":"Outside measurements recover interior conductivity at log rate","feed_subtitle":"New theorems show partial exterior voltage-current data control interior conductivity with log or log-log error.","key_machinery":"The fractional Liouville reduction: multiplying a solution of the conductivity equation by $\\gamma^{1/2}$ turns it into a solution of $(-\\Delta)^s v + q v = 0$ with $q = -(-\\Delta)^s(\\gamma^{1/2}-1)/\\gamma^{1/2}$, and conjugates the conductivity Dirichlet-to-Neumann map into the Schr\\\"odinger one through multiplication by $\\gamma^{\\pm 1/2}$. The argument also relies on a regularity lemma showing that $\\gamma^{\\pm 1/2}$ maps $\\widetilde H^s$ spaces homeomorphically, on a known logarithmic stability theorem for fractional Schr\\\"odinger equations with partial exterior data, and, for the log-log case, on a proposition that bounds a compactly supported function in terms of its fractional Laplacian outside the set.","core_discovery":"The central discovery is that partial exterior data suffice for quantitative stability in the fractional conductivity problem, not just uniqueness. After applying the fractional Liouville reduction, which rewrites the conductivity equation as a fractional Schr\\\"odinger equation with reduced potential $q = -(-\\Delta)^s(\\gamma^{1/2}-1)/\\gamma^{1/2}$, the paper proves that the operator-norm difference of the conductivity Dirichlet-to-Neumann maps dominates the difference of the reduced potentials. An elliptic estimate then converts the potential difference into the $H^s(\\Omega)$ difference of the conductivities themselves. The resulting moduli of continuity are explicit, and all constants depend only on the geometry, the measurement sets, the ellipticity bound, and the a priori smoothness bound, not on the individual conductivities.","pith_inferences":["The log-log rate in Theorem 1.2 likely reflects the additional uncertainty from not knowing the conductivities outside $\\Omega$; an analogous rate is known to be optimal in the local inverse conductivity problem, and one may conjecture a similar optimality here.","A direct check of whether the assumed $H^{2s+\\epsilon,n/s}(\\mathbb{R}^n)$ condition implies the weighted-space hypothesis used in the cited comparison proposition is a natural next step; the paper does not spell out that implication, despite relying on it.","The same reduction should yield partial-data stability for other nonlocal inverse problems, such as fractional magnetic Schr\\\"odinger equations, whenever a comparable comparison lemma for the relevant Dirichlet-to-Neumann maps is available.","Numerical experiments on simple conductivity families could test whether the logarithmic modulus is qualitatively sharp or merely an artifact of the proof technique."],"forward_implications":["Partial exterior measurements are enough: when the conductivities agree a priori in the whole exterior, the interior $H^s(\\Omega)$ conductivity error is bounded by $C|\\log \\delta|^{-\\sigma}$, where $\\delta$ is the operator-norm measurement error.","Without exterior agreement, compact support of the conductivity difference still gives control in $L^p(\\mathbb{R}^n)$ for $1 \\le p < 2n/(n-2s)$, at a log-log rate.","The constants in both estimates depend only on $s,n,\\Omega$, the measurement sets, the ellipticity lower bound, and the a priori smoothness bound, so the stability is uniform over the admissible class.","This improves the earlier complete-data stability result by allowing the measurements to be taken only on bounded open subsets of the exterior, rather than on the whole exterior.","The nonlocal nature of the operator is used essentially: the proof controls the difference in a larger set by the fractional Laplacian of the difference in an exterior set, a step with no local analogue."],"supporting_citations":[{"why":"Supplies the core logarithmic stability theorem for the fractional Schr\\\"odinger equation with partial exterior data, which the paper feeds after the Liouville reduction.","marker":"[RS20]"},{"why":"Provides the comparison between conductivity and Schr\\\"odinger Dirichlet-to-Neumann maps and the elliptic estimate used to pass from potential differences to conductivity differences.","marker":"[CRTZ24]"},{"why":"Its Proposition 6.1 bounds a compactly supported function by its fractional Laplacian outside the set, producing the log-log rate in Theorem 1.2.","marker":"[GRSU20]"},{"why":"Gives the low-regularity fractional Liouville reduction and the multiplication estimates for $\\gamma^{\\pm 1/2}$ on Sobolev spaces.","marker":"[RZ24]"},{"why":"Ensures existence and boundedness of the exterior Dirichlet-to-Neumann map for the fractional conductivity equation under the stated regularity.","marker":"[RZ23b]"},{"why":"Establishes the basic exterior Dirichlet-to-Neumann map formalism for the fractional Schr\\\"odinger equation and its boundedness.","marker":"[GSU20]"},{"why":"Supplies the Kato-Ponce commutator estimate used to place the reduced potentials in the required Sobolev space.","marker":"[KP88]"}],"fun_headline_variants":["Partial data yields log stability in fractional conductivity","Fractional conductivity recovery with log-log error bounds","Stable partial-data inversion for fractional conductivity","Logarithmic stability from exterior measurements only","Partial data: log-stable fractional conductivity imaging"],"cache_read_input_tokens":3200,"weakest_assumption_plain":"The proof requires the background deviations $m_i = \\gamma_i^{1/2}-1$ to lie in the mixed-norm Sobolev space $H^{2s+\\epsilon,n/s}(\\mathbb{R}^n)$ with a uniform bound, and the reduced Schr\\\"odinger operators to avoid a zero Dirichlet eigenvalue; if either fails, the chain of estimates is not established.","fun_headline_variants_meta":{"raw":{"variants":["Partial data yields log stability in fractional conductivity","Fractional conductivity recovery with log-log error bounds","Stable partial-data inversion for fractional conductivity","Logarithmic stability from exterior measurements only","Partial data: log-stable fractional conductivity imaging"]},"model":"deepseek-v4-flash","effort":"low","cost_usd":0.00012,"raw_usage":{"total_tokens":1002,"prompt_tokens":774,"completion_tokens":228,"prompt_tokens_details":{"cached_tokens":384},"prompt_cache_hit_tokens":384,"prompt_cache_miss_tokens":390,"completion_tokens_details":{"reasoning_tokens":160}},"tokens_in":390,"tokens_out":228,"duration_ms":2706,"temperature":1.0,"reasoning_tokens":160,"cache_read_input_tokens":384,"cache_creation_input_tokens":0},"cache_creation_input_tokens":0},"created_at":"2026-08-07T14:30:26.180010+00:00","model_set":{"reader":"deepseek-v4-flash"},"falsifier":"Verify whether the assumed $H^{2s+\\epsilon,n/s}(\\mathbb{R}^n)$ condition implies the weighted-space hypothesis $H^{(2s+\\epsilon)/\\theta_0,\\theta_0 n/s}$ used in the cited comparison proposition for every allowed $\\theta_0$; a counterexample for small $\\epsilon$ would expose a gap in the proof of Theorem 1.2, and a pair of conductivities achieving a slower-than-logarithmic rate would refute Theorem 1.1.","supporting_citations":[],"review_version":1}