Land-use change reduces soil nitrogen retention of both particulate and mineral-associated organic matter in a temperate grassland

被引:6
|
作者
Yang, Lu [1 ,2 ]
Liu, Weixing [1 ,2 ]
Jia, Zhou [1 ,2 ]
Li, Ping [1 ,2 ]
Wu, Yuntao [1 ,2 ]
Chen, Yaru [1 ,2 ]
Liu, Chao [1 ,2 ]
Chang, Pengfei [1 ,2 ]
Liu, Lingli [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Xiangshan, Beijing 100093, Peoples R China
[2] Univ Chinese Acad Sci, Yuquan Rd, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
N-15; labeling; Tillage; Winter snow cover; recovery; Particle density fractions; MICROBIAL BIOMASS; SEQUESTRATION POTENTIALS; TERRESTRIAL ECOSYSTEMS; DIFFERENT TILLAGE; CARBON STORAGE; WIND EROSION; SNOW DEPTH; FRACTIONS; WINTER; MECHANISMS;
D O I
10.1016/j.catena.2022.106432
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Soil organic matter (SOM) fractions vary in formation and microbial activities, thus playing different roles in exogenous nitrogen (N) retention in terrestrial ecosystems. However, it remains unclear how land-use and environmental changes affect the behavior of SOM fractions in retaining exogenous N. Here, we investigated N distribution among four SOM fractions and how soil N retention capacity responds to tillage and increased snowfall. We monitored N retention in SOM fractions by adding (NH4NO3)-N-15-N-15 isotope in the field in a temperate grassland in Inner Mongolia. Our results showed that the fine mineral-associated organic matter (MOM < 20 mu m) had the largest N pool with a lower mass. The free particulate organic matter (fPOM) accounted for only 0.8% of total SOM mass, representing the second-largest N pool. The coarse mineral-associated organic matter (MOM > 20 mu m) represented the fewer N pool with the largest mass. MOM < 20 mu m and fPOM retained > 90% of the N-15 tracer in soil. Deepened snow did not affect N-15 retention in SOM fractions, while tillage decreased N-15 retention in MOM < 20 mu m, fPOM, and occluded particulate organic matter within aggregates (oPOM). We suggested that the reduction in soil total N retention under tillage conditions was mainly due to the reduced N retention in fPOM and MOM < 20 mu m. Structural equation modeling analysis revealed that tillage-induced decrease in N-15 retention of MOM < 20 mu m was regulated by both decreased microbial N-15 retention and reduced clay and silt contents. The decrease in N-15 retention of fPOM was probably due to the decreased microbial N-15 retention along with the increased plant N-15 uptake. This research reveals divergent pathways of N-15 retention among different SOM fractions in response to land-use change and provides novel insights into the estimation of soil N retention capacity with SOM fractions taken into consideration.
引用
收藏
页数:8
相关论文
共 50 条
  • [1] Divergent contribution of particulate and mineral-associated organic matter to soil carbon in grassland
    Liao, Jiaojiao
    Yang, Xuan
    Dou, Yanxing
    Wang, Baorong
    Xue, Zhijing
    Sun, Hui
    Yang, Yang
    An, Shaoshan
    [J]. JOURNAL OF ENVIRONMENTAL MANAGEMENT, 2023, 344
  • [2] Temperature effects on cropland soil particulate and mineral-associated organic carbon are governed by agricultural land-use types
    Li, Chengji
    Ran, Min
    Song, Liangying
    Zhang, Yuanyuan
    Li, Aiwen
    Shi, Wenjiao
    Li, Wendan
    Cheng, Jinli
    Zhao, Bin
    Luo, Youlin
    Tao, Qi
    Wu, Yingjie
    Gao, Xuesong
    Wilson, John P.
    Li, Qiquan
    [J]. Geoderma, 2024, 448
  • [3] Soil carbon storage informed by particulate and mineral-associated organic matter
    Cotrufo, M. Francesca
    Ranalli, Maria Giovanna
    Haddix, Michelle L.
    Six, Johan
    Lugato, Emanuele
    [J]. NATURE GEOSCIENCE, 2019, 12 (12) : 989 - +
  • [4] Different climate sensitivity of particulate and mineral-associated soil organic matter
    Emanuele Lugato
    Jocelyn M. Lavallee
    Michelle L. Haddix
    Panos Panagos
    M. Francesca Cotrufo
    [J]. Nature Geoscience, 2021, 14 : 295 - 300
  • [5] Soil aggregate formation and the accrual of particulate and mineral-associated organic matter
    Jastrow, JD
    [J]. SOIL BIOLOGY & BIOCHEMISTRY, 1996, 28 (4-5): : 665 - 676
  • [6] Soil carbon storage informed by particulate and mineral-associated organic matter
    M. Francesca Cotrufo
    Maria Giovanna Ranalli
    Michelle L. Haddix
    Johan Six
    Emanuele Lugato
    [J]. Nature Geoscience, 2019, 12 : 989 - 994
  • [7] Different climate sensitivity of particulate and mineral-associated soil organic matter
    Lugato, Emanuele
    Lavallee, Jocelyn M.
    Haddix, Michelle L.
    Panagos, Panos
    Cotrufo, M. Francesca
    [J]. NATURE GEOSCIENCE, 2021, 14 (05) : 295 - +
  • [8] Distinct bioenergetic signatures in particulate versus mineral-associated soil organic matter
    Williams, Elizabeth K.
    Fogel, Marilyn L.
    Berhe, Asmeret Asefaw
    Plante, Alain F.
    [J]. GEODERMA, 2018, 330 : 107 - 116
  • [9] Mineral-associated and particulate organic matter in aggregates as a proxy for soil C changes in pasture-sugarcane land use transitions
    Schiebelbein, Bruna Emanuele
    Bordonal, Ricardo de Oliveira
    Cerri, Carlos Eduardo Pellegrino
    Oliveira, Dener Marcio da Silva
    Cherubin, Mauricio Roberto
    [J]. REVISTA BRASILEIRA DE CIENCIA DO SOLO, 2023, 47
  • [10] Changes in particulate and mineral-associated organic carbon with land use in contrasting soils
    Sabina YEASMIN
    Balwant SINGH
    Cliff T.JOHNSTON
    Quan HUA
    Donald L.SPARKS
    [J]. Pedosphere, 2023, (03) : 421 - 435