Different responses of priming effects in long-term nitrogen- and phosphorus-fertilized soils to exogenous carbon inputs

被引:4
作者
Qin, Wenkuan [1 ,2 ]
Feng, Jiguang [1 ,2 ]
Zhang, Qiufang [1 ,2 ,3 ]
Yuan, Xia [4 ]
Ren, Fei [5 ]
Zhou, Huakun [6 ]
Zhu, Biao [1 ,2 ]
机构
[1] Peking Univ, Inst Ecol, Coll Urban & Environm Sci, Beijing 100871, Peoples R China
[2] Peking Univ, Coll Urban & Environm Sci, Key Lab Earth Surface Proc, Minist Educ, Beijing 100871, Peoples R China
[3] Fujian Normal Univ, Sch Geog Sci, Fuzhou 350117, Peoples R China
[4] Hangzhou Normal Univ, Coll Life & Environm Sci, Hangzhou 311121, Peoples R China
[5] Qinghai Univ, State Key Lab Plateau Ecol & Agr, Xining 810000, Peoples R China
[6] Chinese Acad Sci, Northwest Inst Plateau Biol, Qinghai Prov Key Lab Restorat Ecol Cold Area, Xining 810008, Peoples R China
关键词
Priming effect; Nitrogen fertilization; Phosphorus fertilization; Microbial activities; Alpine meadow; ORGANIC-MATTER; MICROBIAL COMMUNITIES; ALPINE GRASSLAND; USE EFFICIENCY; PLANT; PATTERNS; MINERALIZATION; MECHANISMS; LIMITATION; STORAGE;
D O I
10.1007/s11104-024-06510-3
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Background and aimsLong-term nitrogen (N) and phosphorus (P) fertilization could immensely alter plant-soil-microbial properties, thereby impacting the priming effect (PE). However, previous studies mostly simulated PE responses to fertilization by adding nutrient in the laboratory, which could not represent PE changes under long-term fertilization-induced ecosystem alteration. Our aim is to clarify the PE alteration in soils with long-term fertilization history in an alpine meadow.MethodsSoil samples (0-10 cm) were collected from a 9-year field fertilization experiment (including four treatments: control, + N with urea, + P with triple superphosphate, + NP with both fertilizers), and incubated for 30 days with 13C-labeled glucose amendment (2% SOC). Plant-soil-microbial properties were measured before/after incubation.ResultsGlucose addition induced a positive PE in all soils with a range from 0.56 to 1.37 mg C g-1 soil. N fertilization did not affect PE intensity due to the microbial adaptation and fast utilization of the added glucose for metabolic needs. P fertilization caused P accumulation in soils, and decreased available N and pH. Such changes inhibited microbes, and glucose activated microbial activities, causing higher PE intensity.ConclusionLong-term N fertilization did not significantly affect PE, while P fertilization stimulated PE intensity. Overall, we highlight that P fertilization may induce higher risk of CO2 release, which deserves more attention when applying P fertilizers in this alpine meadow.
引用
收藏
页码:647 / 663
页数:17
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