We consider the chaotic behavior of the sediment movement with the obs
erved data of the Yangtze River in China and the method of the reconst
ructed phase space and we find that in the sediment movement there is
an attractor. As far as the real example mentioned in this paper is co
ncerned, the correlation dimension and the largest Lyapunov exponent a
re around 6.6 and 0.013 respectively. These results are crucially refe
rential for estimating the mode of the sediment movement, designing th
e scheme of the sediment observation, and studying the predictability
problem of the sediment.