REACTOR THEORY The basic principles are simple but detailed calculations are difficult Use very simplified models to understand principles of calculations.

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REACTOR THEORY The basic principles are simple but detailed calculations are difficult Use very simplified models to understand principles of calculations Hence assume a HOMOGENEOUS reactor Uniform mixture of UO2SO4 (fuel) and D2O (moderator) N.B. A normal reactor is HETEROGENEOUS with fuel and moderator separated The overall aim is to develop a reactor equation which will allow us to Estimate the minimum size of a thermal fission reactor Provide an estimate of how quickly the neutron flux will change when control rods are moved Lecture 20

Average over thermal neutron energies  The Reactor Equation PLAN Consider how neutrons diffuse in a reactor and define a partial flux density Apply the continuity equation for neutrons in a small volume allowing for diffusion, capture plus a source of neutrons Average over thermal neutron energies  The Reactor Equation Then look at steady state solutions for finite size reactors Look at time dependence for an infinite reactor NEUTRON DIFFUSION THEORY Assume all the neutrons have one velocity v  ONE GROUP MODEL (assumes all the neutrons have slowed down) Neutron Flux F = n v assuming n neutrons per unit volume Lecture 20

A vector with same dimensions as F Introduce PARTIAL CURRENT DENSITY J where J is the NET no. of neutrons s-1 crossing an area of 1 m2 perpendicular to the direction of J A vector with same dimensions as F i.e Jz+ is the number of Neutrons passing upwards through the area from the lower hemisphere Let Jz+ be the current density in + z direction Let Jz- be the current density in - z direction Net flow Jz = Jz+ - Jz- Similarly for Jx and Jy so J = Jx i + Jy j + Jz k Lecture 20

Homogeneous and isotropic medium ASSUME:- Homogeneous and isotropic medium Scattering in Lab. System is isotropic This happens as vC0 i.e. M >> m . e.g. OK for Carbon (but not H) 3. sS >> sA 4. Neutron flux is a slowly varying function of position Consider an infinite system in which neutrons are diffusing and we wish to determine Jz According to assumption 2. the scattering will be isotropic  Fraction scattered from volume dV in particular direction The number of interactions per second in a volume dV is FN sS dV (assuming 3. above) (N is the number of nuclei per unit volume) Lecture 20

In the above dV = r2 sinq dr dq df Probability that neutrons from dV will pass through dA is dA cosq / (4pr2) (i.e. the solid angle subtended by A at dV divided by 4p) If sS >> sA then the probability that neutrons will travel a distance r without interacting is exp(- sS Nr) Putting all these factors together and defining SS = sS N we obtain:- Lecture 20

The number of neutrons which pass through dA per second after scattering in dV is The current density at dA due to scattering in dV is The Flux F is not constant but varies throughout the reactor i,e. F = F(r) Evaluate F in terms of F0, the flux at the point at which J is being determined Make a Taylor expansion to 1st Order (See (4)) (F(r) is the flux at dV and F0 is flux at dA) Lecture 20

The terms involving cos(f) and sin(f) vanish when integrating f Now substitute in equation for Jz- and integrate to find the number of neutrons passing from the upper hemisphere to the lower hemisphere The terms involving cos(f) and sin(f) vanish when integrating f from 0 to 2p Lecture 20

Similarly for Jz+ we have :- for Jx and Jy Similarly we obtain Lecture 20

Introduce the DIFFUSION COEFFICIENT D Where lS is the MEAN FREE PATH for scattering Note the difference between J and F. One is a vector representing the net number of neutrons crossing an area and the latter is a scalar specifying the neutron flux at a point but with the neutrons travelling in all directions due to scattering as in a gas. N.B. Modern text books have a different definition of D as they start from Fick’s Law (which we have essentially just derived) This extra factor of v occurs in the ensuing derivations in Lilley for example but leads to the same final formulae. Lecture 20

Graphite; NC = 1600 / ( 12 * 1.66 10-27) = 8.03 1028 m-3 Example:- Calculate the Diffusion Coefficient in a) H20 and b) Graphite. [Densities are:- a) 1000 kg m-3 and b) 1600 kg m-3and the scattering cross sections are sS(H20) = 50 b and sS(Graphite) = 50 b ] H2O; NH2O = 1000 / ( 18 * 1.66 10-27) = 4.78 1028 m-3 lS = 1 / (Ns) = 1 / (4.78 1028 x 50 10-28) = 4.2 10-3 m  D = 4.2 10-3 / 3 = 1.4 10-3 m for H2O Graphite; NC = 1600 / ( 12 * 1.66 10-27) = 8.03 1028 m-3 lS = 1 / (Ns) = 1 / (8.03 1028 x 4.7 10-28) = 26.4 10-3 m  D = 26.4 10-3 / 3 = 8.8 10-3 m for H2O Lecture 20

EXAMPLE:- A source emitting S neutrons s-1 is situated at the origin in a moderator with Diffusion Coefficient D and Diffusion Length L= (D/SA)1/2(L allows for absorption of neutrons). The flux as a function of radius r is given by F(r)= (S / 4pDr) exp(-r/L) . Evaluate the total radial flux passing through a sphere at radius r. J = - D  F where   /  r for spherical symmetry so J  Jr(r) i.e.radial Jr(r) = - D  F /  r = - D (S/4pD)[ (- 1 / r2) exp(-r/L) – (1 /r L) exp(-r/L) ] Jr(r) = D (S/4pD) exp(-r/L) [ 1 / r2 + 1 / rL) ] Total Radial Flux = 4 p r2 Jr(r) = S exp(-r/L) [ 1 + r / L) ] N.B. In the limit r  0 Total flux is just S. Lecture 20