We examine the apparent disorder which seems to characterize the spati
al structure of soil moisture by analyzing large-scale experimental da
ta. Specifically, we address the statistical structure of soil moistur
e fields under different scales of observation and find unexpected res
ults. The variance of Soil moisture follows a power law decay as funct
ion of the area at which the process is observed. The spatial correlat
ion remains unchanged with the scale of observation and follows a powe
r law decay typical of scaling processes. Soil moisture also shows cle
ar scaling properties on:its spatial clustering patterns. A well-defin
ed organization of statistical character is found to exist in sail moi
sture patterns linking a large range of scales through which the proce
ss manifests itself and impacts other processes. We suggest that such
scaling properties are crucial to our current understanding and modeli
ng of the dynamics of soil moisture in space and time.