Plants, in addition to their role as primary synthesizers of organic
com- pounds, have evolved as selective accumulators of inorganic
nutrients from the earth's crust. This ability to mine the physical
environment is restricted to green plants and some microorganisms, other
life forms being direct1y or indirect1y dependent on this process for
their supply of mineral nutrients. The initial accumulation of ions by
plants is of ten spatially separated from the photosynthetic parts,
necessitating the transport to these parts of the inorganic solutes thus
acquired. The requirement for energy-rich materials by the accumulation
process is provided by a transport in the opposite direction of organic
solutes from the photosynthetic areas. These transport phenomena in
plants have been studied at the cellular level, the tissue level, and
the whole plant level. The basic problems of analysing the driving
forces and the supply of energy for solute transport remain the same for
alI systems, but the method of approach and the type of results obtained
vary widely with the experimental material employed, reflecting the
variation of the solute transporting properties which have se1ectively
evolved in response to both internal and external environmental
pressures.