『Abstract
The selection and breeding of crop genotypes with root traits
that improve soil resource extraction is a promising avenue to
improved nutrient and water use efficiency in low-input farming
systems. Such genotypes may accelerate nutrient extraction (“nutrient
mining”), but may also reduce nutrient loss via soil erosion by
producing greater shoot biomass and by direct effects of root
traits on aggregate formation and water infiltration. Little is
known about the effects of root architecture on phosphorus (P)
runoff and soil erosion, and the relative importance of root and
shoot traits on runoff P loss has not been determined. Four genotypes
of common bean (Phaseolus vulgaris L.) and two genotypes
of soybean (Glycine max) selected for contrasting root
architecture were grown in a low P soil (Aquic Fragiudult, <20
mg kg-1 Mehlich-3 P, 3% slope) and subjected to rainfall-runoff
experiments with and without shoot removal. Plots with intact
shoots had significantly lower runoff volumes (1.3-7.6 mm) and
total P loads in runoff (0.005-0.32 kg ha-1) than plots
with shoots removed (7.0-16.8 mm; 0.025-1.95 kg ha-1).
Dissolved reactive P leached from plant material did not contribute
significantly to P loss in runoff. Total root length acquired
from soil cores differed significantly among genotypes. Root length
densities in the upper 15 cm of soil mid-way between rows were
less than 4.0 cm cm-3 and variation in root length
density was not correlated with runoff or P loss. Root length
density also did not affect rainfall infiltration or surface runoff
volume. We conclude that for annual dicotyledonous crops such
as bean and soybean with relatively low root length densities,
root traits have little direct effect on soil erosion.
Keywords: Phosphorus; Runoff; Erosion; Root architecture; Common
bean』
Introduction
Materials and methods
Experiment location and plant material
Rainfall simulations
Soil and root sampling
Sample analyses
Soils
Plants (shoots and roots)
Runoff water
Statistical analyses
Results
Plant growth
Runoff
Erosion and particulate P in runoff
Total dissolved P in runoff
Root length density and runoff
Discussion
Conclusions
Acknowledgments
References