Seismic noise includes the information that comes from crust of earth and hypocenter. The study of seismic noise is an essential topic for earthquake predictability and investigation of crustal structure. In this paper we analyze the seismic noise from 46 stations in all around Japan of Full Range Seismograph Network of Japan (F-net). To investigate the influence from earthquake we analyze two types of seismic noise data, one is the data after earthquake shake, which from 2,000 seconds after the max shake of an earthquake, and others are without any earthquake effects. We find that (i) the magnitude of seismic noise values follows a log-normal distribution and (ii) the conditional mean growth rate and the standard deviation of the growth rate of the magnitude value both obey power-law with the magnitude value. Furthermore we also find that the Hurst exponent depends on the max amplitude of earthquake, and shows a linear correlation with logarithmic max amplitude. §1. Introduction Many physical, physiological, biological, and social systems are characterized by complex interactions between a large number of individual components, which manifest in power-law correlations. 1)-14) For example, in financial field, several stylized facts have been found for the equity price data in temporal field, such as 1, the distribution of the stock price changes (return) has a power-law tail. 2, the absolute value of stock price change (volatility) is long-term power-law correlated. 3, The spectral density of stock price is well described by power-law function. 15) In seismology temporal and spatial clustering are considered to be important properties of seismic occurrences and, together with the Omori law (dictating aftershock timing) and the Gutenberg-Richter law (specifying the distribution of earthquake size), comprise the main starting requirements to construct reasonable seismic probabilistic models. Analyzing the timing of individual earthquakes, Ref. 5) introduces the scaling concept to statistical seismology. The recurrence times are defined as the time intervals between consecutive events, τ i = t i − t i−1 . In the case of stationary seismicity, the probability density P (τ ) of the occurrence times was found to follow a universal scaling lawwhere f is a scaling function and R is the rate of seismic occurrence, defined as the mean number of events with M ≥ M c . 16) References 17) and 18) have demonstrated * )