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function Quaternion = madgwickAHRS( Gyroscope, Accelerometer, Magnetometer, quaternion_l,Beta,SamplePeriod)
q = quaternion_l; % short name local variable for readability
% Normalise accelerometer measurement
if(norm(Accelerometer) == 0), return; end % handle NaN
Accelerometer = Accelerometer / norm(Accelerometer); % normalise magnitude
% Normalise magnetometer measurement
if(norm(Magnetometer) == 0), return; end % handle NaN
Magnetometer = Magnetometer / norm(Magnetometer); % normalise magnitude
% Reference direction of Earth's magnetic feild
h = quaternProd(q, quaternProd([0 Magnetometer], quaternConj(q)));
b = [0 norm([h(2) h(3)]) 0 h(4)];
% Gradient decent algorithm corrective step
F = [-2*(q(2)*q(4) - q(1)*q(3)) - Accelerometer(1)
-2*(q(1)*q(2) + q(3)*q(4)) - Accelerometer(2)
-2*(0.5 - q(2)^2 - q(3)^2) - Accelerometer(3)
((2*b(2)*(0.5 - q(3)^2 - q(4)^2) + 2*b(4)*(q(2)*q(4) - q(1)*q(3))) - Magnetometer(1))
((2*b(2)*(q(2)*q(3) - q(1)*q(4)) + 2*b(4)*(q(1)*q(2) + q(3)*q(4))) - Magnetometer(2))
((2*b(2)*(q(1)*q(3) + q(2)*q(4)) + 2*b(4)*(0.5 - q(2)^2 - q(3)^2)) - Magnetometer(3))];
J = [2*q(3), -2*q(4), 2*q(1), -2*q(2)
-2*q(2), -2*q(1), -2*q(4), -2*q(3)
0, 4*q(2), 4*q(3), 0
-2*b(4)*q(3), 2*b(4)*q(4), -4*b(2)*q(3)-2*b(4)*q(1), -4*b(2)*q(4)+2*b(4)*q(2)
-2*b(2)*q(4)+2*b(4)*q(2), 2*b(2)*q(3)+2*b(4)*q(1), 2*b(2)*q(2)+2*b(4)*q(4), -2*b(2)*q(1)+2*b(4)*q(3)
2*b(2)*q(3), 2*b(2)*q(4)-4*b(4)*q(2), 2*b(2)*q(1)-4*b(4)*q(3), 2*b(2)*q(2)];
step = (J'*F);
step = step / norm(step); % normalise step magnitude
% Compute rate of change of quaternion
qDot = 0.5 * quaternProd(q, [0 Gyroscope]) - Beta * step';
% Integrate to yield quaternion
q = q + qDot * SamplePeriod;
Quaternion = q / norm(q); % normalise quaternion
end
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