“…Ways have also been sought to gather data on, and wherever possible to monitor continuously, physical processes without the need for detailed, laborious or repetitive measurements, particularly in the fields of hydrology and meteorology. A recognition that such environmental monitoring can only represent a finite sample from the infinite population of spatial and temporal variations possible has encouraged thorough investigation of sampling procedures in such geographical work (Walling, 1975;Walling and Webb, 1975). Methods by which environmental data may be gathered by less skilled operators have also been sought, for example by soil surveys, to reduce the expense of data collection by highly trained scientists, and it has been shown (Beckett and Burrough, 1971) that grid survey is likely to give better value than free soil survey at map scales greater than i : 50 00o in most landscapes.…”