Author:
Barkle G. F.,Stenger R.,Singleton P. L.,Painter D. J.
Abstract
Over recent years regulatory authorities in New Zealand have promoted
irrigation of dairy farm effluent (DFE) onto the land, to protect surface
water quality. The rate at which the resistant organic matter from DFE
accumulates in the soil and the effect of any accumulation on other soil
organic matter (SOM) related pools, such as microbial biomass, are, however,
unknown. This information is necessary to determine the long-term impact and
sustainability of land-applied DFE.
In this paper we report on changes over 4 years in organic carbon (C
org) and total nitrogen (N t )
from a soil receiving a high application rate of DFE. Soil microbial biomass
(C mic ) measurements were also included to test the hypothesis that C
mic or the C mic /C
org ratio can be used as an early indicator of changes
in SOM.
The regular irrigation with DFE at the high rates used in this study increased
the C mic , pH, C org , and N
t of the soil receiving the effluent. The time series of
C mic showed that this measurement is suitable as an
early indicator of changes in C org and N
t , whereas a single determination of the C
mic /C org ratio was not.
The sustainability of DFE application onto land in terms of N leaching can be
maintained only when the supply of inorganic N is continually matched by the
demand of the pasture. This means that inorganic N fertilisation has to be
reduced concurrently with the gradually increasing N mineralisation from the
accumulating organic matter.
Subject
Earth-Surface Processes,Soil Science,Environmental Science (miscellaneous)
Cited by
36 articles.
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