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Effect of fertilization on decomposition of 14C labelled plant residues and their incorporation into soil aggregates
被引:106
作者:
Majumder, Bidisha
[1
]
Kuzyakov, Yakov
[1
]
机构:
[1] Univ Bayreuth, Agroecosyst Res Dept, BayCEER, D-95440 Bayreuth, Germany
关键词:
Aggregate size fraction;
C-14-labelled plant residue;
Soil organic matter;
Decomposition;
CO2;
efflux;
C sequestration;
Microbial biomass;
ORGANIC-CARBON POOLS;
MICROBIAL BIOMASS C;
ENZYME-ACTIVITIES;
DENSITY FRACTIONS;
NO-TILLAGE;
MACROAGGREGATE DYNAMICS;
FUMIGATION EXTRACTION;
NITROGEN ADDITIONS;
ARABLE SOILS;
SILTY SOILS;
D O I:
10.1016/j.still.2010.05.003
中图分类号:
S15 [土壤学];
学科分类号:
090301 [土壤学];
摘要:
Returning crop residues to soil helps to maintain soil C stocks. Organic C stocks and microbial biomass are important factors controlling the decomposition or retention of crop residues in soil and the formation of aggregates. Little is known about the specific contribution of crop residues to soil aggregate size fractions in the framework of long-term fertilization. This study investigated the effects of long-term fertilization on the decomposition of C-14-labelled plant residues and their incorporation into soil organic matter (SOM) of different aggregate size fractions. Soils were collected from 0-10 cm in the Ap horizon of a long-term (since 1988) field experiment at Grossbeeren (Germany). The following four fertilization treatments were used: 1) without fertilization or manuring (Control), 2) nitrogen applied by mineral fertilizer (N), and 3) manure with low (M) and 4) high (2 M) application doses. Soils were incubated for 100 days at 20 degrees C, with or without C-14-labelled plant residue. The incorporation of C-14 into three aggregate size fractions-large macroaggregates (2-1 mm), small macroaggregates (1-0.25) and microaggregates (<0.25 mm)-was analyzed. After 15 days of incubation, 44-57% of plant residue was mineralized in the order: M > N > control soil > 2 M. Adding plant residues increased soil beta-glucosidase activity and microbial biomass C. On day 16 of incubation, more residue C-14 was retained in small and large macroaggregates than in microaggregates in the control soil. In contrast, in fertilized soils the reverse was measured. Additionally, N, M and 2 M soils showed significant differences by incorporation of C-14 in microbial biomass and beta-glucosidase activity in different aggregate size fractions. The results imply that long-term fertilization significantly increased the residue C-14 retention in microaggregate size fractions and its decomposition in soils. (C) 2010 Elsevier B.V. All rights reserved.
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页码:94 / 102
页数:9
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