Author:
Strong D. T.,Sale P. W. G.,Helyar K. R.
Abstract
Small undisturbed soil volumes (c. 1·7
cm3) were collected from the surface of a small field
plot. Soil volumes were treated with clover-derived substrate, dried and
rewetted, or retained continuously moist from the field. These soil volumes
were then incubated for 20 days at a matric water potential of either
–10 or –30 kPa. At the end of the incubation the soil was analysed
for volumetric water content (θv),
NO-3 -N,
NH+4 -N, total N (%N), and
percentages of sand, silt, and clay. The texture terms were included in linear
regression models, together with %N and θv as predictors of N
mineralisation and nitrification.
Clay and sand were often observed to have a significant influence on N
mineralisation and nitrification, but silt rarely appeared to influence these
processes. In soils retained continuously moist, %clay had a negative
relationship with N mineralisation and nitrification, but this relationship
was positive in soils that had been dried and rewetted. The results suggest
that during periods of relatively high moisture content, soils that are higher
in clay are able to protect organic N more effectively from microbial attack.
However, on drying and rewetting, the protective mechanisms of clay are
undermined, the relatively large protected reservoirs of organic N in high
clay soils become more vulnerable to microbial attack, and these soils
therefore experience a greater flush of N mineralisation than soils with lower
clay levels. The negative influence of clay in the continuously moist soils
was not as clearly observed in the soils incubated at –10 kPa as in
soils incubated at –30 kPa, suggesting that the decomposition of organic
N resident in larger pores (10–30 µm neck diameter) may not be as
strongly regulated by clay as that resident in smaller pores. When soils were
treated with clover-derived substrate, clay had a positive relationship with N
mineralisation and nitrification rates. This may have been because clay
limited the diffusion of partially decomposed organics away from the
decomposing microbial population, thereby helping to facilitate more complete
decomposition of the organic material. Texture had very little influence on
the nitrification of urea-derived ammonium.
Subject
Earth-Surface Processes,Soil Science,Environmental Science (miscellaneous)
Cited by
47 articles.
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