Changes in organic C stability within soil aggregates under different fertilization patterns in a greenhouse vegetable field

被引:13
|
作者
Luan Hao-an [1 ,2 ]
Yuan Shuo [1 ]
Gao Wei [3 ]
Tang Ji-wei [1 ]
Li Ruo-nan [4 ]
Zhang Huai-zhi [1 ]
Huang Shao-wen [1 ]
机构
[1] Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, Key Lab Plant Nutr & Fertilizer, Minist Agr & Rural Affairs, Beijing 100081, Peoples R China
[2] Hebei Agr Univ, Coll Forestry, Baoding 071000, Peoples R China
[3] Tianjin Inst Agr Resources & Environm, Tianjin 300192, Peoples R China
[4] Hebei Acad Agr & Forestry Sci, Inst Agr Resources & Environm, Shijiazhuang 050051, Hebei, Peoples R China
关键词
fertilization; organic C stability; soil aggregates; thermogravimetric analysis; C-13 NMR spectroscopy; MICROBIAL COMMUNITY COMPOSITION; THERMAL-ANALYSIS; ENZYME-ACTIVITIES; CARBON FRACTIONS; RESIDUE CARBON; MATTER; MANAGEMENT; QUALITY; SEQUESTRATION; DYNAMICS;
D O I
10.1016/S2095-3119(21)63646-8
中图分类号
S [农业科学];
学科分类号
09 ;
摘要
Knowledge of the stability of soil organic C (SOC) is vital for assessing SOC dynamics and cycling in agroecosystems. Studies have documented the regulatory effect of fertilization on SOC stability in bulk soils. However, how fertilization alters organic C stability at the aggregate scale in agroecosystems remains largely unclear. This study aimed to appraise the changes of organic C stability within soil aggregates after eight years of fertilization (chemical vs. organic fertilization) in a greenhouse vegetable field in Tianjin, China. Changes in the stability of organic C in soil aggregates were evaluated by four methods, i.e., the modified Walkley-Black method (chemical method), 13C NMR spectroscopy (spectroscopic method), extracellular enzyme assay (biological method), and thermogravimetric analysis (thermogravimetric method). The aggregates were isolated and separated by a wet-sieving method into four fractions: large macroaggregates (>2 mm), small macroaggregates (0.25-2 mm), microaggregates (0.053-0.25 mm), and silt/clay fractions (<0.053 mm). The results showed that organic amendments increased the organic C content and reduced the chemical, spectroscopic, thermogravimetric, and biological stability of organic C within soil aggregates relative to chemical fertilization alone. Within soil aggregates, the content of organic C was the highest in microaggregates and decreased in the order microaggregates>macroaggregates>silt/clay fractions. Meanwhile, organic C spectroscopic, thermogravimetric, and biological stability were the highest in silt/clay fractions, followed by macroaggregates and microaggregates. Moreover, the modified Walkley-Black method was not suitable for interpreting organic C stability at the aggregate scale due to the weak correlation between organic C chemical properties and other stability characteristics within the soil aggregates. These findings provide scientific insights at the aggregate scale into the changes of organic C properties under fertilization in greenhouse vegetable fields in China.
引用
收藏
页码:2758 / 2771
页数:14
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