Mineralization characteristics of soil organic carbon under different herbaceous plant mosaics in semi-arid grasslands

被引:1
作者
Cheng, Bo [1 ,2 ]
Dai, Hai-yan [3 ]
Liu, Tie-jun [1 ,2 ]
Liu, Hu [1 ,2 ]
Li, Jin-rong [1 ,2 ]
Qiao, Rui-jun [4 ]
Shao, Yang [5 ]
Wang, Sheng-li [5 ]
Wang, Jian [1 ,2 ]
机构
[1] China Inst Water Resources & Hydropower Res, Yinshanbeilu Grassland Ecohydrol Natl Observat & R, A-1 Fuxing Rd, Beijing 100038, Peoples R China
[2] Minist Water Resources, Inst Water Resources Pastoral Area, Hohhot 010020, Peoples R China
[3] Inner Mongolia Agr Univ, Hohhot 010018, Inner Mongolia, Peoples R China
[4] Guyang Cty Water Conservancy Dev Ctr, Hohhot 014200, Inner Mongolia, Peoples R China
[5] Inner Mongolia Yin Chao Ji Liao Water Supply Co Lt, Ulanhott 137400, Inner Mongolia, Peoples R China
关键词
Semi-arid grassland; Organic carbon mineralization; Plant community; Soil aggregate; Potential mineralization; Promotion effect; PHOTOSYNTHESIS CONTROLS; MATTER POOLS; CO2; EFFLUX; SEQUESTRATION; DYNAMICS;
D O I
10.1038/s41598-024-73018-2
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
We aimed to explore the mineralization characteristics of soil organic carbon(SOC) under different plant species in semi-arid grassland and provide basic soil carbon cycling data. Leymus chinensis, Stipa krylovii Roshev, Artemisia frigida, and Agrophorn cristam (L.) Gaertn were selected as the plant species. Incubation experiment were conducted on SOC mineralization in soil aggregates with particle sizes of > 2, 1-2, 0.25-1, and < 0.25 mm. The cumulative SOC mineralization amount in L. chinensis with a particle size > 2 mm was the highest, exceeding that of A. cristam (L.) Gaertn by approximately 136.14%. S. krylovii Roshev (70.73%), L. chinensis (58.05%), and A. frigida (33.73%) exhibited pronounced promotion effects on mineralization. The potential SOC mineralization of S. krylovii Roshev was the greatest among all species at the same soil particle size. The potential SOC mineralization was highest at a particle size of > 2 mm for all plant types. All plant types increased the SOC mineralization rate and cumulative mineralization in soils with large particle sizes, the mineralization reaction occurred more strongly. Organic carbon cumulative SOC mineralization rapidly increased in all tests during the first 20 days and gradually slowed thereafter.
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页数:10
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