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17-Phys-B1 Radiation Physics · December 2017

Question 7 of 7: Port Hope Legacy Waste, CANDU Fuel Chemistry, and Precise Reporting

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

Paper format. 98-Phys-B1 Radiation Physics, National Examination December 2017 — a three-hour open-book examination in which any non-communicating calculator is permitted (the candidate must record the calculator's make and model on the first sheet). The cover page states the exam has 7 questions worth a total of 74 points, of which only 60 points' worth need be answered for full marks; every question and sub-part is nonetheless answered in full below so the paper remains a complete study resource. The cover page also invites the candidate to submit a written statement of any assumptions made where a question is open to interpretation — this licence is used below in Question 1(a)–(b) (the historic DOE report's "roentgens per hour" reading is converted to absorbed dose using the standard air-kerma factor since no calibration medium is stated) and 1(e) (the Canadian nuclear-energy-worker annual effective-dose limit, 50 mSv/yr, is used to size the inspection-crew rotation since the source states no dose constraint of its own), and in Question 6(a) (counting-statistics uncertainty is taken as Poisson, $\sigma(C)=\sqrt{C}$, on the one-minute count reported in each row, since the source gives no separate counting-time datum). Question 6 also carries a genuine internal inconsistency between the table header's definition of $g(t)$ and the definition restated in part (c) — both readings and the resolution adopted are flagged where they occur.

Reference texts. K. S. Krane, Introductory Nuclear Physics (nuclear reaction kinematics, pair production, fission energetics); F. H. Attix, Introduction to Radiological Physics and Radiation Dosimetry (exposure–dose conversion, photon interactions, non-ionizing radiation); J. R. Cember and T. E. Johnson, Introduction to Health Physics, 5th ed. (radiation weighting factors, ALARA dose planning, decay-counting statistics); J. E. Turner, Atoms, Radiation, and Radiation Protection, 3rd ed. (neutron detectors, radioactive decay/in-growth kinetics, radiation protection principles).

Question 7: Port Hope Legacy Waste, CANDU Fuel Chemistry, and Precise Reporting (16 marks)

Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.

Given. Port Hope's Eldorado/Cameco refinery history (radium and uranium refining since the 1930s–40s); the low-level waste stored at Port Hope and Port Granby; a June 2017 untreated-water overflow event; the refinery's UO$_2$ and UF$_6$ products and their respective end uses.

Find. (a) a substantive response identifying the waste's likely radionuclide content and its health significance; (b) why CANDU uses natural (unenriched) uranium; (c) why CANDU uses the oxide, not the metal; (d) a scientifically precise rewrite of the UF$_6$/light-water-reactor claim.

Approach. Trace the waste's radiological character back to Port Hope's radium and uranium refining history (part a), then work from CANDU's heavy-water neutron economy (part b) and UO$_2$'s ceramic-fuel properties (part c) before untangling the fuel-cycle distinction between an enrichment feedstock gas (UF$_6$) and an actual reactor fuel form (part d).

  1. Part (a) — response to the Waterkeeper blog. Port Hope's contamination legacy is not primarily "spent fuel" waste — it dates from decades of radium and, later, uranium ore refining by Eldorado, predating today's environmental controls. The radioactive material most characteristic of this specific legacy is 226Ra (radium-226, $T_{1/2}=1{,}600$ y) and its decay-chain progeny, together with residual natural-uranium process residues (238U, 230Th, and their own daughters) left in historic tailings, slag, and contaminated soil/sediment that were subsequently consolidated into the engineered storage now managed by the Port Hope Area Initiative. Unlike fission-product waste from reactor operation, this legacy material is overwhelmingly an alpha-emitting hazard chain: radium and its daughters (including the gas 222Rn and its own short-lived alpha-emitting progeny) pose little external hazard through intact skin or at a distance — alpha particles cannot penetrate even the outer dead layer of skin, let alone a container wall or open water — but represent a serious hazard only if inhaled or ingested, where they irradiate lung, bone, or other tissue directly at short range over a long period (radium is a well-documented bone-seeker, chemically similar to calcium). This distinction matters directly for the June 2017 overflow: the water reaching Lake Ontario carries these long-lived, low specific-activity legacy residues, not a fresh, concentrated fission-product plume, and PHAI's statement that the effect was assessed against aquatic-life protection criteria and found negligible is consistent with what would be expected of a dilute release of this material class, provided the reported sampling and comparison against provincial/federal criteria were performed correctly and transparently — which is exactly what Lake Ontario Waterkeeper's request for the underlying sample data and methodology is reasonably asking to confirm. For Port Hope residents specifically, the CNSC's cited "40 studies" finding of low exposure levels is consistent with the primarily-alpha, largely-contained nature of this legacy material: the principal health-protective measures are proper containment of dust/soil and drinking-water source control, not concern over penetrating external radiation from the stored waste itself. The July 17 CNSC order — requiring CNL to strengthen emergency preparedness and water management/storage capacity — is the right corrective response to an overflow event of this kind: it targets the actual failure mode (inadequate containment capacity during a heavy rain event), rather than implying any new type of hazard was discovered, and it is a reasonable, proportionate regulatory response given the low but non-zero radiological/environmental significance of an uncontrolled release from any licensed nuclear waste site.
  2. Part (b) — why CANDU uses unenriched uranium. CANDU reactors use heavy water (D$_2$O) as both moderator and coolant. Heavy water has a far smaller neutron-absorption cross-section than ordinary (light) water, so far fewer neutrons are lost to parasitic capture in the moderator during slowing-down. That superior neutron economy is enough, on its own, to sustain a chain reaction using only the 0.72% natural abundance of fissile 235U — no enrichment plant, and its associated cost and proliferation sensitivity, is required.
  3. Part (c) — why CANDU uses UO$_2$, not metallic uranium. Ceramic UO$_2$ has a much higher melting point ($\approx2865^{\circ}$C, versus $\approx1132^{\circ}$C for metallic uranium), giving a large safety margin against fuel melting. It is also dimensionally and chemically far more stable under irradiation: metallic uranium undergoes disruptive phase changes and irradiation-induced swelling/distortion, and, being pyrophoric, reacts readily with water or air if a cladding failure occurs, whereas the UO$_2$ ceramic matrix is chemically inert in the coolant, resists corrosion, and retains fission products far better within its lattice even if the fuel sheath is breached.
  4. Part (d) — precise rewrite of the UF$_6$/light-water-reactor claim. The Toronto Star's phrasing implies UF$_6$ gas is itself loaded into a light-water reactor, which is incorrect: UF$_6$ is the volatile compound used as the feedstock gas for the isotope enrichment process (gas centrifuge or, historically, gaseous diffusion) that raises the 235U content above its natural 0.72% abundance for light-water-reactor use. Once enriched, the UF$_6$ is converted back into UO$_2$ ceramic pellets and fabricated into fuel bundles — it is that enriched UO$_2$, not UF$_6$ gas, that is actually loaded into a light-water reactor core. A precise rewrite: "The refinery also produces uranium hexafluoride (UF$_6$), the natural-uranium feedstock gas used in the isotope-enrichment process that raises the uranium's U-235 content for light-water-reactor fuel; after enrichment elsewhere, the UF$_6$ is converted back into UO$_2$ ceramic fuel pellets before being loaded into a light-water reactor."
Question 7 — results
PartResult
(a)Legacy waste is primarily Ra-226/U-238-chain (alpha) residue from historic radium/uranium refining, not fission-product waste; internal (inhalation/ingestion) hazard dominates, consistent with low reported exposure
(b)D$_2$O's low neutron absorption sustains criticality on natural (unenriched) uranium
(c)UO$_2$: higher melting point, irradiation-stable, chemically inert vs. pyrophoric metallic U
(d)UF$_6$ is an enrichment feedstock gas, later converted to UO$_2$ fuel – never loaded into a reactor as UF$_6$
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