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Magneto-Optical Traps

A magneto-optical trap, or MOT, combines red-detuned optical molasses with a magnetic-field gradient and polarization-selective transitions. The Doppler shift makes the force oppose velocity. The Zeeman shift makes the force oppose displacement. Near the trap center,

F≃−κr−αv.\mathbf F \simeq - \boldsymbol{\kappa}\mathbf r - \boldsymbol{\alpha}\mathbf v.

The first term confines; the second damps. Neither the light alone nor the quadrupole magnetic field alone generally provides the standard MOT force. The trap exists because displacement changes which counterpropagating beam is closer to resonance.

A MOT is an open, driven, dissipative system. It continually scatters photons, diffuses momentum, optically pumps internal states, loads atoms from an external source, and loses them through collisions. Its steady state is not simply thermal equilibrium in a conservative potential.

This page owns:

  1. the one-dimensional Zeeman-plus-Doppler force;
  2. the sign of the restoring force;
  3. the three-dimensional quadrupole and beam geometry;
  4. linear trap dynamics, size, and gravitational sag;
  5. capture, loading, one-body loss, and two-body loss;
  6. density limits, diagnostics, operating sequences, and common failures.

Doppler Cooling owns the optical-molasses friction and recoil-diffusion derivation. Radiation Pressure owns the single-beam scattering force. Zeeman Effect in Atoms owns the atomic level shifts and gg-factor conventions. Sub-Doppler Cooling owns polarization-gradient and dark-state mechanisms that may coexist with, or be suppressed by, the MOT field.

Optical Dipole Traps owns conservative AC Stark confinement, Gaussian-beam frequencies, and the depth–scattering tradeoff. The MOT is the dissipative capture and precooling stage from which those traps are commonly loaded.

Take two beams along ±x\pm x, both with wave-number magnitude kk. Use the chapter’s atom-minus-laser detuning:

Δ=ω0−ωL.\Delta = \omega_0-\omega_L.

Red detuning means Δ>0\Delta>0. Let the local magnetic field be

Bx(x)=B′x.B_x(x) = B'x.

The two beam helicities address transitions with opposite Zeeman shifts. Label the polarizations so that, for positive effective magnetic moment μeff\mu_{\mathrm{eff}},

β=μeffB′ℏ>0.\beta = \frac{\mu_{\mathrm{eff}}B'}{\hbar} > 0.

For velocity vv along +x+x, define the effective detunings

Δ+(x,v)=Δ+kv+βx,Δ−(x,v)=Δ−kv−βx.\begin{aligned} \Delta_+(x,v) &= \Delta + kv + \beta x, \\ \Delta_-(x,v) &= \Delta - kv - \beta x. \end{aligned}

The subscripts identify beam momentum ±ℏk\pm\hbar k. These equations already encode the chosen helicities. Reversing either the field gradient or both beam helicities reverses the sign of the position term.

Set v=0v=0 and place the atom at x>0x>0. Then

Δ+=Δ+βx,Δ−=Δ−βx.\Delta_+ = \Delta+\beta x, \qquad \Delta_- = \Delta-\beta x.

For red detuning and small displacement, the −x-x beam is closer to resonance:

∣Δ−∣<∣Δ+∣.|\Delta_-| < |\Delta_+|.

It therefore scatters more strongly and supplies momentum −ℏk-\hbar k, toward the origin. At x<0x<0, the roles reverse. The polarization assignment is correct only if this sign test succeeds.

A one-dimensional magneto-optical trap, its restoring-force window, and atom-number loading curves with one- and two-body loss.

At x>0x>0, the Zeeman shift moves the inward-propagating beam closer to resonance. The force is linear only near the origin and within the capture window. The trapped population is set separately by loading rate L\mathcal L, one-body loss γ\gamma, and density-dependent two-body loss β\beta.

For a closed transition and independent weak beams, use

R(δ)=Γs211+(2δ/Γ)2.R(\delta) = \frac{\Gamma s}{2} \frac{1}{ 1+(2\delta/\Gamma)^2 }.

The net force is

F(x,v)=ℏk[R(Δ+)−R(Δ−)].F(x,v) = \hbar k \left[ R(\Delta_+) - R(\Delta_-) \right].

This compact expression contains both trapping and damping. It remains a two-level model: real MOTs require multilevel optical pumping, repumping, beam saturation, and a position-dependent quantization axis.

Define

q=kv+βx.q = kv+\beta x.

Near x=v=0x=v=0,

R(Δ±q)≃R(Δ)±qR′(Δ).R(\Delta\pm q) \simeq R(\Delta) \pm qR'(\Delta).

Therefore

F(x,v)≃2ℏkR′(Δ)(kv+βx)=−αv−κx,\begin{aligned} F(x,v) &\simeq 2\hbar kR'(\Delta) \left( kv+\beta x \right) \\ &= -\alpha v-\kappa x, \end{aligned}

with

α=−2ℏk2R′(Δ),\alpha = -2\hbar k^2R'(\Delta),

and

κ=−2ℏkβR′(Δ).\kappa = -2\hbar k\beta R'(\Delta).

For

D=1+(2ΔΓ)2,D = 1+\left(\frac{2\Delta}{\Gamma}\right)^2,

the derivative is

R′(Δ)=−4s(Δ/Γ)D2.R'(\Delta) = - \frac{ 4s(\Delta/\Gamma) }{ D^2 }.

Hence

α=8ℏk2sΔ/ΓD2,\alpha = 8\hbar k^2s \frac{ \Delta/\Gamma }{ D^2 },

and

κ=8ℏkβsΔ/ΓD2.\kappa = 8\hbar k\beta s \frac{ \Delta/\Gamma }{ D^2 }.

For Δ>0\Delta>0 and β>0\beta>0, both coefficients are positive. A useful consistency relation is

κα=βk=μeffB′ℏk.\frac{\kappa}{\alpha} = \frac{\beta}{k} = \frac{ \mu_{\mathrm{eff}}B' }{ \hbar k }.

The same spectral slope sets damping and confinement; the field gradient converts displacement into an effective Doppler shift.

Saturation and shared excited-state population

Section titled “Saturation and shared excited-state population”

At higher intensity, one often replaces the denominator by

1+stot+(2δΓ)2.1+s_{\mathrm{tot}} + \left( \frac{2\delta}{\Gamma} \right)^2.

This is only a representative correction. Counterpropagating beams share the same excited-state population, while multilevel Clebsch–Gordan coefficients and optical pumping make the saturation state dependent. A quantitative MOT model generally solves position- and velocity-dependent optical Bloch or rate equations.

An anti-Helmholtz coil pair creates a field zero near the trap center. If B′B' denotes the axial gradient, an ideal local field is

B(r)=B′(x2x^+y2y^−zz^).\mathbf B(\mathbf r) = B' \left( \frac{x}{2}\hat{\mathbf x} + \frac{y}{2}\hat{\mathbf y} - z\hat{\mathbf z} \right).

The factors are required by

∇⋅B=0.\boldsymbol{\nabla}\cdot\mathbf B = 0.

The radial gradient is half the axial magnitude. Consequently, equal beam parameters do not imply equal spring constants in all directions.

The conventional three-dimensional MOT uses one counterpropagating beam pair along each Cartesian axis. Relative helicities are chosen so that the beam propagating toward the field zero addresses the locally favored transition.

The labels σ+\sigma^+ and σ−\sigma^- are defined relative to a quantization axis, not merely by a laboratory drawing of circular polarization. Because the quadrupole field changes direction through the cloud, a correct sign argument must track:

  1. beam propagation direction;
  2. local magnetic-field direction;
  3. the addressed ΔmF=±1\Delta m_F=\pm1 transition;
  4. the transition’s effective Zeeman shift.

Near the exact field zero, the quantization axis is not well defined. The simple independent-axis picture is then qualitative; full multilevel dynamics determines optical pumping and dark-state structure.

Mirror MOTs, pyramidal MOTs, and grating MOTs generate the required beam directions with reflections or diffraction. Two-dimensional MOTs cool and collimate an atomic beam while allowing longitudinal flux. Narrow-line MOTs use a small Γ\Gamma, so gravity, recoil, and field curvature become more prominent. Molecular and blue-detuned MOTs can require type-II transitions, polarization or magnetic remixing, and force mechanisms beyond the simple two-level type-I model.

The local test remains the same: calculate the actual transition shifts and show that displacement increases inward scattering.

Along one principal axis,

mx¨+αx˙+κx=0.m\ddot x + \alpha\dot x + \kappa x = 0.

Define

ω0=κm,Γm=α2m.\omega_0 = \sqrt{\frac{\kappa}{m}}, \qquad \Gamma_m = \frac{\alpha}{2m}.

The characteristic exponents are

r±=−Γm±Γm2−ω02.r_\pm = -\Gamma_m \pm \sqrt{ \Gamma_m^2-\omega_0^2 }.

The motion is underdamped when Γm<ω0\Gamma_m<\omega_0, critically damped when they are equal, and overdamped when Γm>ω0\Gamma_m>\omega_0. Many broad-line MOTs are strongly damped, so a displaced cloud may return without visible oscillation.

The measured relaxation rates need not equal this two-level prediction. Sub-Doppler forces, beam imbalance, multiple scattering, changing cloud size, and internal-state delays alter them.

The position part of the linear force can be represented by

Ueff(x)=12κx2.U_{\mathrm{eff}}(x) = \frac{1}{2}\kappa x^2.

This is a local pseudopotential, useful for cloud-size and sag estimates. The full MOT force is dissipative, velocity dependent, saturating, and generally not derivable from a global scalar potential.

If one principal direction is approximately harmonic and the motional distribution is thermal,

n(x)∝exp⁡(−κx22kBT).n(x) \propto \exp \left( - \frac{\kappa x^2}{2k_{\mathrm B}T} \right).

The rms width is

σx=kBTκ.\sigma_x = \sqrt{ \frac{k_{\mathrm B}T}{\kappa} }.

This relation can infer κ\kappa from an independently measured temperature and cloud width. It fails in a density-limited, non-Gaussian, anisotropic, or strongly multiple-scattering cloud.

Along vertical coordinate zz, add gravity:

Fz=−κzz−αzvz−mg.F_z = -\kappa_z z-\alpha_z v_z-mg.

The equilibrium sag is

zg=−mgκz.z_g = -\frac{mg}{\kappa_z}.

For broad-line alkali MOTs this may be small. In narrow-line MOTs, the maximum optical force and spring constant can be much smaller, so gravity substantially shifts the cloud and changes which part of the Zeeman profile is sampled.

A beam imbalance or stray radiation pressure similarly adds a constant force F0F_0 and shifts the center by

x0=F0κ.x_0 = \frac{F_0}{\kappa}.

A uniform magnetic bias shifts the quadrupole zero. Center position versus bias field is therefore a useful alignment diagnostic.

The scattering force from one saturated closed transition cannot exceed approximately

Fmax⁡≃ℏkΓ2s1+s.F_{\max} \simeq \frac{\hbar k\Gamma}{2} \frac{s}{1+s}.

The corresponding maximum acceleration is

amax⁡=Fmax⁡m.a_{\max} = \frac{F_{\max}}{m}.

If a particle experiences that acceleration over distance LL, an optimistic kinematic upper bound is

vc≲2amax⁡L.v_c \lesssim \sqrt{2a_{\max}L}.

Actual capture velocities are smaller because the force is resonant only over part of the trajectory, Gaussian beams have finite diameter, optical pumping leaks population, and atoms can leave transversely.

Substantial scattering requires at least one beam to satisfy roughly

∣Δ±kv±βx∣≲Γ21+stot.\left| \Delta \pm kv \pm \beta x \right| \lesssim \frac{\Gamma}{2} \sqrt{1+s_{\mathrm{tot}}}.

The gradient helps bring displaced atoms into resonance, but an excessively large gradient can make the resonant shell too narrow and reduce the capture volume. Detuning, intensity, gradient, and beam diameter must be optimized together.

Common loading architectures include:

  • direct capture from a low-pressure vapor;
  • a slowed atomic beam;
  • a two-dimensional MOT feeding a science chamber;
  • buffer-gas or cryogenic molecular beams followed by laser slowing;
  • recapture from another optical or magnetic stage.

The relevant source metric is phase-space flux into the MOT’s capture acceptance, not total particle flux alone.

Let L\mathcal L be the loading rate, γ\gamma the one-body loss rate, and β\beta the two-body loss coefficient. Then

dNdt=L−γN−β∫n(r,t)2 d3r.\frac{dN}{dt} = \mathcal L - \gamma N - \beta \int n(\mathbf r,t)^2\,d^3r.

One-body loss includes collisions with background gas and source particles. The quadratic term includes light-assisted cold collisions and other density-dependent processes.

For a fixed Gaussian shape,

n(r)=n0exp⁡[−∑ixi22σi2],n(\mathbf r) = n_0 \exp \left[ - \sum_i \frac{x_i^2}{2\sigma_i^2} \right],

and

∫n2 d3r=N2V2,V2=8π3/2σxσyσz.\int n^2\,d^3r = \frac{N^2}{V_2}, \qquad V_2 = 8\pi^{3/2} \sigma_x\sigma_y\sigma_z.

The number equation becomes

N˙=L−γN−βV2N2.\dot N = \mathcal L - \gamma N - \frac{\beta}{V_2}N^2.

When two-body loss is negligible and N(0)=0N(0)=0,

N(t)=Lγ(1−e−γt).N(t) = \frac{\mathcal L}{\gamma} \left( 1-e^{-\gamma t} \right).

Thus

Nss=Lγ,τload=1γ.N_{\mathrm{ss}} = \frac{\mathcal L}{\gamma}, \qquad \tau_{\mathrm{load}} = \frac{1}{\gamma}.

Changing vapor pressure often raises both L\mathcal L and γ\gamma, so the largest loading rate need not maximize steady-state number or lifetime.

For constant V2V_2, define

A=βV2.A = \frac{\beta}{V_2}.

The steady state solves

ANss2+γNss−L=0,AN_{\mathrm{ss}}^2 + \gamma N_{\mathrm{ss}} - \mathcal L = 0,

giving

Nss=2Lγ+γ2+4AL.N_{\mathrm{ss}} = \frac{ 2\mathcal L }{ \gamma + \sqrt{ \gamma^2+4A\mathcal L } }.

At high density, V2V_2 may grow with NN because rescattered photons expand the cloud. A constant-volume quadratic fit can then misidentify the loss coefficient.

Use several protocols:

  1. fit loading curves at several source fluxes;
  2. turn off loading while leaving trapping light on and measure decay;
  3. vary cloud volume through gradient or intensity;
  4. independently image density profiles;
  5. vary excited-state fraction through detuning and repump power;
  6. measure background pressure or compare with an ion gauge cautiously.

One loading trace rarely separates L\mathcal L, γ\gamma, β\beta, and a changing V2V_2 uniquely.

Near-resonant light couples colliding atom pairs to excited molecular potentials. The released kinetic energy or radiative escape can eject one or both particles. The resulting β\beta depends on detuning, intensity, hyperfine state, molecular potentials, and trap depth.

Radiation trapping and multiple scattering

Section titled “Radiation trapping and multiple scattering”

A spontaneously emitted photon can be reabsorbed by another atom. Repeated scattering produces an effective repulsion and additional momentum diffusion. At sufficiently large NN, the cloud can enter a constant-density regime in which its radius grows while peak density changes little.

This is collective radiative transport, not a modification of the single-atom spring constant alone.

A dark SPOT reduces the repump intensity in the cloud center, shelving most atoms in a hyperfine ground state that interacts weakly with the cooling light. The outer bright shell continues to confine and load. Lower central excited-state fraction suppresses rescattering and light-assisted loss, allowing higher density.

The method does not make the MOT conservative. It spatially separates the bright capture region from a darker storage region.

The magnetic gradient provides confinement but does not by itself determine temperature. Momentum diffusion and velocity-dependent forces still set the motional distribution. Depending on species, transition type, field, and polarization:

  • a two-level Doppler estimate may be adequate;
  • polarization-gradient cooling may lower temperature;
  • the quadrupole field may disrupt sub-Doppler coherences;
  • narrow-line recoil and gravity may dominate;
  • multiple scattering may heat or broaden the cloud;
  • anisotropic beams may produce different temperatures by axis.

For this reason, many experiments switch off the field gradient and use a short optical-molasses stage after MOT loading.

For a dilute thermal Gaussian cloud, peak phase-space density is

D0=n0(2πℏ2mkBT)3/2.\mathcal D_0 = n_0 \left( \frac{ 2\pi\hbar^2 }{ mk_{\mathrm B}T } \right)^{3/2}.

A MOT is normally a high-flux precooling stage, not the final route to quantum degeneracy. Near-resonant scattering and density-dependent loss limit phase-space density well before evaporative or many-body regimes.

A common broad-line alkali sequence is:

  1. Load. Use large beams, substantial intensity, moderate red detuning, and a gradient chosen for capture volume.
  2. Compress. Increase gradient, change detuning, and often reduce repump power to raise density.
  3. Cool. Turn off or reduce the field and use optical molasses or another sub-Doppler stage.
  4. State prepare. Optically pump into the desired hyperfine and Zeeman state.
  5. Transfer. Load a conservative optical or magnetic trap.

The order and timing matter. Increasing gradient may compress position while heating momentum; reducing repump may raise density while slowing loading; leaving near-resonant light on during transfer may increase light-assisted loss.

If each atom scatters at total rate RscR_{\mathrm{sc}} and the collection efficiency is η\eta, the detected photon rate is

C=ηNRsc.C = \eta N R_{\mathrm{sc}}.

Converting fluorescence to NN requires a model or calibration of RscR_{\mathrm{sc}}, including polarization, multilevel populations, detuning, intensity, and reabsorption.

Calibrated optical depth gives a spatial column density. Saturation, detuning, optical pumping during the probe, finite resolution, and multiple scattering must be controlled. Combining absorption images with time-of-flight yields number, size, and temperature.

Displace the cloud with a bias field or beam imbalance, release the perturbation, and fit its return. The response constrains α\alpha and κ\kappa. Modulating the gradient or intensity can locate mechanical resonances, but parametric heating and delayed internal dynamics can shift the apparent frequency.

Record both turn-on and decay curves. Repeat versus source flux, gradient, detuning, cooling intensity, repump intensity, and background pressure. Simultaneously image the cloud volume so that density-dependent loss is not folded into an effective one-body lifetime.

MOTs serve as:

  • bright sources for precision spectroscopy;
  • precooling stages for optical clocks and atom interferometers;
  • reservoirs for optical dipole traps, lattices, and optical tweezers;
  • starting points for evaporative cooling toward degeneracy;
  • controlled samples for cold-collision and photoassociation studies;
  • loaders for cavity-QED and Rydberg platforms;
  • capture stages for atoms and increasingly complex molecules;
  • calibrated sources of cold ions and electrons after photoionization.

Their value is operational: large capture volume, continuous dissipation, direct fluorescence, and compatibility with staged transfer. These same features make a MOT too noisy and dissipative for many coherent experiments, so the trapping light and quadrupole field are usually removed before the science sequence.

In the standard MOT, the field gradient shifts optical resonances. Radiation pressure supplies the restoring force. A static quadrupole field by itself cannot trap every internal state and is not the mechanism derived here.

Forgetting beam momentum when naming helicity

Section titled “Forgetting beam momentum when naming helicity”

The same laboratory circular polarization viewed along opposite propagation directions corresponds to different spherical components. Track k\mathbf k, local B\mathbf B, and ΔmF\Delta m_F explicitly.

Using laser-minus-atom detuning without changing signs

Section titled “Using laser-minus-atom detuning without changing signs”

This chapter uses Δ=ω0−ωL\Delta=\omega_0-\omega_L, so red means Δ>0\Delta>0. References using δ=ωL−ω0\delta=\omega_L-\omega_0 have red δ<0\delta<0.

F=−κx−αvF=-\kappa x-\alpha v is a local expansion. At large position or velocity, one beam may pass through resonance and then become far detuned; finite beam diameter also ends the force.

The harmonic pseudopotential summarizes the local position force. Photon scattering, velocity dependence, optical pumping, and diffusion remain.

Fitting every loading curve with one exponential

Section titled “Fitting every loading curve with one exponential”

Two-body loss, changing cloud size, source depletion, and pressure transients can all bend the curve. Inspect residuals and acquire independent decay and volume data.

Inferring temperature from cloud size alone

Section titled “Inferring temperature from cloud size alone”

σ2=kBT/κ\sigma^2=k_{\mathrm B}T/\kappa requires known κ\kappa, a thermal Gaussian, and negligible collective expansion. Use time-of-flight or another independent thermometer.

Off-resonant excitation can leak an alkali atom into the other ground hyperfine manifold. Without repumping, it becomes dark to the cooling cycle. Repump intensity also controls excited-state fraction, density, and loss.

  1. Choose a cycling manifold. List all cooling and leakage transitions, Clebsch–Gordan coefficients, and repump paths.
  2. Declare signs. Fix Δ\Delta, B′B', μeff\mu_{\mathrm{eff}}, beam momenta, and polarizations.
  3. Run the displaced-atom test. At x>0x>0, show that the −x-x beam is closer to resonance.
  4. Compute capture scales. Compare Doppler and Zeeman shifts with linewidth, saturation broadening, beam diameter, and available acceleration.
  5. Linearize locally. Estimate α\alpha, κ\kappa, damping regime, sag, and cloud size.
  6. Model the source. Determine phase-space flux into the capture acceptance.
  7. Separate losses. Acquire loading, decay, and volume measurements over several densities.
  8. Validate transfer. Measure number, temperature, internal state, and phase-space density after every stage, not only inside the MOT.
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  2. D. E. Pritchard, E. L. Raab, V. Bagnato, C. Wieman, and R. N. Watts, “Light traps using spontaneous forces,” Physical Review Letters 57, 310–313 (1986), doi:10.1103/PhysRevLett.57.310.
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  4. T. Walker, D. Sesko, and C. Wieman, “Collective behavior of optically trapped neutral atoms,” Physical Review Letters 64, 408–411 (1990), doi:10.1103/PhysRevLett.64.408.
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  8. M. H. Anderson, W. Petrich, J. R. Ensher, and E. A. Cornell, “Reduction of light-assisted collisional loss rate from a low-pressure vapor-cell trap,” Physical Review A 50, R3597–R3600 (1994), doi:10.1103/PhysRevA.50.R3597.
  9. K. Dieckmann, R. J. C. Spreeuw, M. Weidemüller, and J. T. M. Walraven, “Two-dimensional magneto-optical trap as a source of slow atoms,” Physical Review A 58, 3891–3895 (1998), doi:10.1103/PhysRevA.58.3891.
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Starting from

F=ℏk[R(Δ+kv+βx)−R(Δ−kv−βx)],F = \hbar k \left[ R(\Delta+kv+\beta x) - R(\Delta-kv-\beta x) \right],

derive α\alpha, κ\kappa, and their ratio in the weak-saturation limit.

Solution

Set q=kv+βxq=kv+\beta x and expand:

R(Δ±q)≃R(Δ)±qR′(Δ).R(\Delta\pm q) \simeq R(\Delta) \pm qR'(\Delta).

Then

F≃2ℏkR′(Δ)(kv+βx).F \simeq 2\hbar kR'(\Delta) \left( kv+\beta x \right).

Matching F=−αv−κxF=-\alpha v-\kappa x gives

α=−2ℏk2R′(Δ),κ=−2ℏkβR′(Δ).\alpha = -2\hbar k^2R'(\Delta), \qquad \kappa = -2\hbar k\beta R'(\Delta).

Therefore

κα=βk.\frac{\kappa}{\alpha} = \frac{\beta}{k}.

For red detuning, the Lorentzian slope satisfies R′(Δ)<0R'(\Delta)<0, so α,κ>0\alpha,\kappa>0 when β>0\beta>0.

Verify that

B=B′(x2x^+y2y^−zz^)\mathbf B = B' \left( \frac{x}{2}\hat{\mathbf x} + \frac{y}{2}\hat{\mathbf y} - z\hat{\mathbf z} \right)

obeys Maxwell’s equation in a current-free trapping region. What is the ratio of axial to radial gradient magnitudes?

Solution

The divergence is

∇⋅B=B′2+B′2−B′=0.\boldsymbol{\nabla}\cdot\mathbf B = \frac{B'}{2} + \frac{B'}{2} - B' = 0.

The axial gradient magnitude is B′B', while either radial gradient magnitude is B′/2B'/2. The ratio is therefore 2:12:1.

A trapped atom has

m=1.44×10−25 kg,α=3.0×10−22 kg s−1,κ=2.0×10−19 N m−1.m = 1.44\times10^{-25}\,\mathrm{kg}, \quad \alpha = 3.0\times10^{-22}\,\mathrm{kg\,s^{-1}}, \quad \kappa = 2.0\times10^{-19}\,\mathrm{N\,m^{-1}}.

Compute ω0\omega_0, Γm\Gamma_m, and determine whether the motion is under- or overdamped.

Solution

The undamped frequency is

ω0=κm≃1.18×103 s−1.\omega_0 = \sqrt{\frac{\kappa}{m}} \simeq 1.18\times10^3\,\mathrm{s^{-1}}.

The damping parameter is

Γm=α2m≃1.04×103 s−1.\Gamma_m = \frac{\alpha}{2m} \simeq 1.04\times10^3\,\mathrm{s^{-1}}.

Because Γm<ω0\Gamma_m<\omega_0, the oscillator is underdamped, but only weakly:

ω02−Γm2≃5.5×102 s−1.\sqrt{\omega_0^2-\Gamma_m^2} \simeq 5.5\times10^2\,\mathrm{s^{-1}}.

A MOT loads at L=2.0×107 s−1\mathcal L=2.0\times10^7\,\mathrm{s^{-1}} and has γ=0.20 s−1\gamma=0.20\,\mathrm{s^{-1}}. Neglect two-body loss. Find the steady atom number and the time to reach 90%90\% of it.

Solution

The steady number is

Nss=Lγ=1.0×108.N_{\mathrm{ss}} = \frac{\mathcal L}{\gamma} = 1.0\times10^8.

Set

0.90=1−e−γt90.0.90 = 1-e^{-\gamma t_{90}}.

Then

t90=ln⁡10γ≃11.5 s.t_{90} = \frac{\ln 10}{\gamma} \simeq 11.5\,\mathrm s.

Let

L=1.0×107 s−1,γ=0.10 s−1,βV2=1.0×10−9 s−1.\mathcal L = 1.0\times10^7\,\mathrm{s^{-1}}, \quad \gamma = 0.10\,\mathrm{s^{-1}}, \quad \frac{\beta}{V_2} = 1.0\times10^{-9}\,\mathrm{s^{-1}}.

Find NssN_{\mathrm{ss}}.

Solution

With A=β/V2A=\beta/V_2,

Nss=2Lγ+γ2+4AL.N_{\mathrm{ss}} = \frac{ 2\mathcal L }{ \gamma+\sqrt{\gamma^2+4A\mathcal L} }.

Numerically,

γ2+4AL=0.01+0.04≃0.224 s−1.\sqrt{\gamma^2+4A\mathcal L} = \sqrt{0.01+0.04} \simeq 0.224\,\mathrm{s^{-1}}.

Thus

Nss≃2.0×1070.324≃6.2×107.N_{\mathrm{ss}} \simeq \frac{2.0\times10^7}{0.324} \simeq 6.2\times10^7.

The one-body-only prediction would be 10810^8, so the curvature is experimentally significant.

For T=100 μKT=100\,\mu\mathrm K and κ=2.0×10−19 N m−1\kappa=2.0\times10^{-19}\,\mathrm{N\,m^{-1}}, estimate the rms cloud width along one axis.

Solution

Use

σ=kBTκ.\sigma = \sqrt{ \frac{k_{\mathrm B}T}{\kappa} }.

Then

σ≃(1.381×10−23)(1.0×10−4)2.0×10−19≃8.3×10−5 m.\sigma \simeq \sqrt{ \frac{ (1.381\times10^{-23})(1.0\times10^{-4}) }{ 2.0\times10^{-19} } } \simeq 8.3\times10^{-5}\,\mathrm m.

So the rms width is about 83 μm83\,\mu\mathrm m.

Using the mass and spring constant from Exercise 3, calculate the vertical sag.

Solution

The magnitude is

∣zg∣=mgκ.|z_g| = \frac{mg}{\kappa}.

Substitution gives

∣zg∣=(1.44×10−25)(9.81)2.0×10−19≃7.1×10−6 m.|z_g| = \frac{ (1.44\times10^{-25})(9.81) }{ 2.0\times10^{-19} } \simeq 7.1\times10^{-6}\,\mathrm m.

The cloud sags by about 7 μm7\,\mu\mathrm m for these parameters.

At x>0x>0 and v=0v=0, an experiment finds that the +x+x beam is closer to resonance than the −x-x beam. What force results, and which changes restore trapping?

Solution

The +x+x beam then scatters more strongly and pushes the atom farther toward +x+x. The position force is anti-restoring:

F≃+∣κ∣x.F \simeq +|\kappa|x.

Reversing the magnetic-field gradient changes the Zeeman sign. Reversing both beam helicities changes which transition each beam addresses. Either operation can restore the desired condition that, at x>0x>0, the −x-x beam is closer to resonance. Reversing both the gradient and helicities together leaves their relative sign unchanged and therefore does not fix the anti-trap.