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Long‐term field fertilization affects soil nitrogen transformations in a rice‐wheat‐rotation cropping system
Author(s) -
Zhang Jinbo,
Cai Zucong,
Yang Wenyan,
Zhu Tongbin,
Yu Yongjie,
Yan Xiaoyuan,
Jia Zhongjun
Publication year - 2012
Publication title -
journal of plant nutrition and soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.644
H-Index - 87
eISSN - 1522-2624
pISSN - 1436-8730
DOI - 10.1002/jpln.201200149
Subject(s) - mineralization (soil science) , nitrification , chemistry , agronomy , straw , nitrogen cycle , crop rotation , soil water , fertilizer , ammonium , environmental chemistry , nitrogen , biology , crop , ecology , organic chemistry
Mineralization and nitrification are the key processes of the global N cycle and are primarily driven by microorganisms. However, it remains largely unknown about the consequence of intensified agricultural activity on microbial N transformation in agricultural soils. In this study, the 15 N‐dilution technique was carried out to investigate the gross mineralization and nitrification in soils from a long‐term field fertilization experiment starting from 1988. Phospholipid fatty acids (PLFA) analysis was used to determine soil microbial communities, e.g., biomasses of anaerobic bacterial, bacterial, fungi, and actinobacteria. The abundance of ammonia‐oxidizing bacteria (AOB) and archaea (AOA) were measured using real‐time quantitative polymerase chain reaction. The results have demonstrated significant stimulation of gross mineralization in the chemical‐fertilizers treatment (NPK) ([6.53 ± 1.29] mg N kg –1 d –1 ) and chemical fertilizers– plus –straw treatment (NPK+S1) soils ([8.13 ± 1.68] mg N kg –1 d –1 ) but not in chemical fertilizers– plus– two times straw treatment (NPK+S2) soil when compared to the control‐treatment (CK) soil ([3.62 ± 0.86] mg N kg –1 d –1 ). The increase of anaerobic bacterial biomass is up to 6‐fold in the NPK+S2 compared to that in the CK soil ([0.7 ± 0.5] nmol g –1 ), implying that exceptionally high abundance of anaerobic bacteria may inhibit gross mineralization to some extent. The gross nitrification shows upward trends in the NPK+S1 and NPK+S2 soils. However, it is only significantly higher in the NPK soil ([5.56 ± 0.51] mg N kg –1 d –1 ) compared to that in the CK soil ([3.70 ± 0.47] mg N kg –1 d –1 ) ( p < 0.05). The AOB abundance increased from (0.28 ± 0.07) × 10 6 copies (g soil) –1 for the CK treatment to (4.79 ± 1.23) × 10 6 copies (g soil) –1 for the NPK treatment after the 22‐year fertilization. In contrast, the AOA abundance was not significantly different among all treatment soils. The changes of AOB were well paralleled by gross nitrification activity (gross nitrification rate = 0.263 AOB + 0.047 NH $ _4^+ $ ‐N + 2.434, R 2 = 0.73, p < 0.05), suggesting the predominance of bacterial ammonia oxidation in the fertilized fields.