Abstract
Two-year legume fallows of Sesbania Sesban, Acacia angustissima and Cajanuscajan were evaluated for their residual N effects on two subsequent maize crops under minimum and conventional tillage management. The proportion of N 2 -fixed in litter was 56, 55, 84 and 58 % for Acacia, Sesbania , Cajanus, and cowpea, respectively, resulting in inputs of biologically fixed N of 122, 84, 97 and 28 kg N ha -1 . Maize growth following the legumes for two subsequent cropping seasons was in most cases not directly related to the N inputs due to pest infestation and drought. On a sandy soil, these legumes adapted poorly and did not improve N cycling.
Soil samples for mineral N determination in profiles were taken at fallow termination and every two weeks during maize cropping with an auger in 0.2 m sections to 1.2 m depth. Pre-season NH 4+ amounts were > 12 kg N ha -1 in the 0-0.2 m layer for treatments that had a large litter layer. There was a flush of NO 3- -N in the Sesbania and Acacia plots with the first rains. Topsoil NO 3- had increased to >29 kg N ha -1 by the time of establishing the maize crop. NO 3- -N amounts decreased rapidly within three weeks of maize planting to 9 and 11 kg N ha -1 for the Sesbania and Acacia plots, respectively. Total NO 3- -N leaching losses from the 0-0.4mlayer ranged from 29-40 kg ha -1 for Sesbania and Acacia plots within two weeks when 104 mm rainfall was received to an already fully recharged soil profile. NO 3- -N then increased below the 0.4 m depth during early season when the maize had not developed a sufficient root length density to effectively capture nutrients. Nitrous oxide emissions were small, with a peak of 12 g N 2 O-N ha -1 day -1 from Sesbania plots and near background fluxes in maize monoculture plots. The decrease of mineral N concentration in the topsoil resulted in reduced N 2 O fluxes, despite very high soil moisture conditions. N 2 O-N emissions were greatest for Sesbania plots with only 0.3 kg ha -1 lost in 56 days.
The effects of improved fallows on rainfall partitioning and associated soil loss were investigated using simulated rainfall at 35 mm h -1 . Immediately after fallow clearance, infiltration rates were greater than water application rate for the Acacia and natural fallow treatments, but steady state infiltration rates were 24 mm h -1 in Sesban and 5 mm h -1 in continuous maize. The estimated runoff losses after 30 minutes of rainfall were 44% from continuous maize compared with 22% from Sesbania and none from Acacia and natural fallow plots. After one post-fallow crop, water infiltration was still greater than 35 mm h -1 in the Acacia plots. Steady state infiltration rates after 30 minutes of rainfall were 8 and 5 mm h -1 for Sesbania and continuous maize systems, respectively. Planted tree fallows increase infiltration rates, but the effect markedly decrease after one year of maize cropping in non-coppicing tree fallows.
In a field litterbag decomposition experiment, the course of the decomposition could be adequately described by the function Y = (Y0-Q)e -kt + Q, and the relative decomposition constants for Sesbania and Acacia litters were 0.053 and 0.039 d -1 , respectively. Under laboratory incubation conditions, N mineralized from fresh Sesbania prunings was 55% after 120 days compared with 27% only for the Sesbania litter. During the same period, fresh prunings of Acacia released only 12 % of the added N while Acacia litter released 9 %. N mineralization from Acacia fresh prunings was depressed by the high protein binding capacity of its polyphenols. Except for Sesbania litter, the rest of the senesced legume materials showed N immobilization up to 60 days.
The study showed that Sesbania, Acacia and Cajanus produced useful amounts of biomass on soils of at least loamy texture and improved N cycling significantly, but adapted poorly in lighter soils. Under conditions of severe texture constraints, mucuna showed robustness but has the disadvantage of having no direct food value. Gaseous N losses after incorporating legume materials were small, and the reduction of NO 3- leaching is the single largest challenge to increased N recovery in the highly porous soils.
Original language | English |
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Qualification | Doctor of Philosophy |
Awarding Institution |
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Supervisors/Advisors |
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Award date | 23 Mar 2004 |
Place of Publication | Wageningen |
Print ISBNs | 9789058089861 |
Publication status | Published - 2004 |
Keywords
- agroforestry systems
- nitrogen cycle
- fallow systems
- improved fallow
- nitrogen fixation
- leaching
- mineralization
- nitrogen
- zimbabwe
- agroecosystems