Litter decomposition and C and N dynamics as affected by N additions in a semi-arid temperate steppe, Inner Mongolia of China

被引:17
|
作者
Qin PENG [1 ]
YuChun QI [1 ]
YunShe DONG [1 ]
YaTing HE [1 ,2 ]
ShengSheng XIAO [3 ]
XinChao LIU [1 ,2 ]
LiangJie SUN [1 ,2 ]
JunQiang JIA [1 ,2 ]
ShuFang GUO [1 ,2 ]
CongCong CAO [1 ,2 ]
机构
[1] Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences
[2] University of Chinese Academy of Sciences
[3] Jiangxi Provincial Research Institute for Soil and Water Conservation
基金
中国国家自然科学基金;
关键词
litter decomposition; N deposition; N level; N form; C sequestration; semi-arid temperate grassland;
D O I
暂无
中图分类号
S812.2 [草原土壤学];
学科分类号
0713 ;
摘要
Litter decomposition is the fundamental process in nutrient cycling and soil carbon(C) sequestration in terrestrial ecosystems. The global-wide increase in nitrogen(N) inputs is expected to alter litter decomposition and,ultimately, affect ecosystem C storage and nutrient status. Temperate grassland ecosystems in China are usually N-deficient and particularly sensitive to the changes in exogenous N additions. In this paper, we conducted a 1,200-day in situ experiment in a typical semi-arid temperate steppe in Inner Mongolia to investigate the litter decomposition as well as the dynamics of litter C and N concentrations under three N addition levels(low N with 50 kg N/(hm2?a)(LN), medium N with 100 kg N/(hm2?a)(MN), and high N with 200 kg N/(hm2?a)(HN)) and three N addition forms(ammonium-N-based with 100 kg N/(hm2?a) as ammonium sulfate(AS), nitrate-N-based with 100 kg N/(hm2?a) as sodium nitrate(SN), and mixed-N-based with 100 kg N/(hm2?a) as calcium ammonium nitrate(CAN)) compared to control with no N addition(CK). The results indicated that the litter mass remaining in all N treatments exhibited a similar decomposition pattern: fast decomposition within the initial 120 days, followed by a relatively slow decomposition in the remaining observation period(120–1,200 days). The decomposition pattern in each treatment was fitted well in two split-phase models, namely, a single exponential decay model in phase I(<398 days) and a linear decay function in phase II(≥398 days). The three N addition levels exerted insignificant effects on litter decomposition in the early stages(<398 days, phase I; P>0.05). However, MN and HN treatments inhibited litter mass loss after 398 and 746 days, respectively(P<0.05). AS and SN treatments exerted similar effects on litter mass remaining during the entire decomposition period(P>0.05). The effects of these two N addition forms differed greatly from those of CAN after 746 and 1,053 days, respectively(P<0.05). During the decomposition period, N concentrations in the decomposing litter increased whereas C concentrations decreased, which also led to an exponential decrease in litter C:N ratios in all treatments. No significant effects were induced by N addition levels and forms on litter C and N concentrations(P>0.05). Our results indicated that exogenous N additions could exhibit neutral or inhibitory effects on litter decomposition, and the inhibitory effects of N additions on litter decomposition in the final decay stages are not caused by the changes in the chemical qualities of the litter, such as endogenous N and C concentrations. These results will provide an important data basis for the simulation and prediction of C cycle processes in future N-deposition scenarios.
引用
收藏
页码:432 / 444
页数:13
相关论文
共 50 条
  • [21] Effects of grassland degradation and precipitation on carbon storage distributions in a semi-arid temperate grassland of Inner Mongolia, China
    Li, Xiaobing
    Bai, Yunxiao
    Wen, Wanyu
    Wang, Hong
    Li, Ruihua
    Li, Guoqing
    Wang, Han
    ACTA OECOLOGICA-INTERNATIONAL JOURNAL OF ECOLOGY, 2017, 85 : 44 - 52
  • [22] Effects of the "Grain for Green" Program on Soil Water Dynamics in the Semi-Arid Grassland of Inner Mongolia, China
    Zhang, Zhi-Hua
    Peng, Hai-Ying
    Kong, Yuhua
    WATER, 2021, 13 (15)
  • [23] Atmospheric deposition of inorganic nitrogen in a semi-arid grassland of Inner Mongolia, China
    Zhang Yibo
    Xu Wen
    Wen Zhang
    Wang Dandan
    Hao Tianxiang
    Tang Aohan
    Liu Xuejun
    JOURNAL OF ARID LAND, 2017, 9 (06) : 810 - 822
  • [24] Atmospheric deposition of inorganic nitrogen in a semi-arid grassland of Inner Mongolia, China
    ZHANG Yibo
    XU Wen
    WEN Zhang
    WANG Dandan
    HAO Tianxiang
    TANG Aohan
    LIU Xuejun
    Journal of Arid Land, 2017, 9 (06) : 810 - 822
  • [25] Wind Erosion Changes in a Semi-Arid Sandy Area, Inner Mongolia, China
    Zhang, Hanbing
    Gao, Yang
    Sun, Danfeng
    Liu, Lulu
    Cui, Yanzhi
    Zhu, Wenjie
    SUSTAINABILITY, 2019, 11 (01):
  • [26] Belowground Biomass Changed the Regulatory Factors of Soil N2O Funder N and Water Additions in a Temperate Steppe of Inner Mongolia
    Qi Dong
    Yinghui Liu
    Pei He
    Wei Du
    Journal of Soil Science and Plant Nutrition, 2024, 24 : 606 - 617
  • [27] Atmospheric deposition of inorganic nitrogen in a semi-arid grassland of Inner Mongolia, China
    Yibo Zhang
    Wen Xu
    Zhang Wen
    Dandan Wang
    Tianxiang Hao
    Aohan Tang
    Xuejun Liu
    Journal of Arid Land, 2017, 9 : 810 - 822
  • [28] Belowground Biomass Changed the Regulatory Factors of Soil N2O Funder N and Water Additions in a Temperate Steppe of Inner Mongolia
    Dong, Qi
    Liu, Yinghui
    He, Pei
    Du, Wei
    JOURNAL OF SOIL SCIENCE AND PLANT NUTRITION, 2024, 24 (01) : 606 - 617
  • [29] Relationship between carbon pool changes and environmental changes in arid and semi-arid steppe-A two decades study in Inner Mongolia, China
    Li, Hang
    Yang, Banghui
    Meng, Yu
    Liu, Kai
    Wang, Shudong
    Wang, Dacheng
    Zhang, Hongyan
    Huang, Yuling
    Liu, Xingtao
    Li, Dehui
    Li, Long
    Li, Xueke
    SCIENCE OF THE TOTAL ENVIRONMENT, 2023, 893
  • [30] N2O fluxes from the native and grazed semi-arid steppes and their driving factors in Inner Mongolia, China
    Liu, Xing-Ren
    Dong, Yun-She
    Qi, Yu-Chun
    Li, Sheng-Gong
    NUTRIENT CYCLING IN AGROECOSYSTEMS, 2010, 86 (02) : 231 - 240