黄土高原撂荒草地土壤碳库对两年增温增雨的响应
作者:
中图分类号:

Q143;S154.1

基金项目:

国家林业和草原局林草科技创新发展与研究项目(2020132111)和国家自然科学基金项目(41877543)资助


Responses of Soil Carbon Pool of Abandoned Grassland on the Loess Plateau to Two-years Warming and Increased Precipitation
Author:
Fund Project:

Supported by the Forest and Grass Technology Innovation Development and Research Project of the State Forestry and Grassland Administration of China (No. 2020132111), and the National Natural Science Foundation of China (No. 41877543)

  • 摘要
  • | |
  • 访问统计
  • |
  • 参考文献 [32]
  • |
  • 相似文献
  • | | |
  • 文章评论
    摘要:

    阐明暖湿的气候趋势下黄土高原土壤有机碳库不同活性组分和碳库稳定性的变化特征,对脆弱生态区碳库的可持续发展以及评估区域生态效益具有重要意义。以黄土丘陵区自然撂荒草地为研究对象,人工模拟增温和增雨,分析了在增温(W)、增雨(P50%)及其交互作用(WP50%)下植被群落变化特征、土壤有机碳库组分含量、碳库组分的分配比例以及碳库稳定性的变化特征。结果发现:(1)增雨显著增加了植被丰富度指数,而增温和增温增雨显著降低了植被丰富度指数。(2)增雨处理下土壤有机碳、酸解有机碳、易氧化有机碳、溶解性有机碳含量及分配比例在两个取样年均显著高于对照;增温增雨处理则进一步增加了土壤易氧化有机碳和微生物生物量碳含量以及分配比例。相关性分析表明,土壤有机碳与各个活性碳组分之间存在显著相关性。(3)增温增雨处理下土壤碳库活度、碳库活度指数以及碳库管理指数均高于其他处理。酸解有机碳和微生物生物量碳的敏感指数在气候变化处理下相对较高。综上所述,暖湿化的气候背景下黄土丘陵区撂荒草地土壤有机碳、有机碳活性组分含量和分配比例以及碳库稳定性显著提高,有助于碳库良性发展,酸解有机碳和微生物生物量碳可作为未来土壤有机碳变化的重要指示。

    Abstract:

    【Objective】Global climate change has had a huge impact on the carbon pool of terrestrial ecosystems, and the changes in average temperature and precipitation patterns pose severe challenges to the management of terrestrial carbon pools. This is especially serious in the Loess Plateau where the ecological environment is fragile. Therefore, understanding the changes of different fractions of soil organic carbon pool and the stability of this carbon pool under the background of the warming and humid climate of the Loess Plateau is of great significance. This will be of importance in the sustainable development of the carbon pool in fragile ecological areas and the evaluation of regional ecological benefits.【Method】In this study, natural abandoned grassland in the loess hilly region was taken as the research object. Soil warming and increased precipitation were artificially simulated and the changes in vegetation community, soil carbon fractions content and distribution, carbon pool stability index under warming (W), precipitation (P50%) and their interactions (WP50%) were analyzed. 【Result】The results showed that: (1) P50% significantly increased the vegetation Gleason richness index, W and WP50% significantly reduced the Gleason richness index (P < 0.05) and the leaf organic carbon content under the WP50% was significantly higher than the control treatment. Both P50% and WP50% treatments reduced the Shannon-wiener diversity index and pielou evenness index. (2) Soil organic carbon (SOC), acid hydrolyzable organic carbon (AHC), easily oxidizable carbon (EOC), dissolved organic carbon (DOC) content and their distribution ratio of the two sampling years under P50% were significantly higher than the control treatment. Also, warming based on P50% can further increase soil EOC, microbial biomass carbon (MBC) content and distribution ratio. However, only the soil MBC showed a significant difference compared with the control under W treatment. Recalcitrant organic carbon (ROC) presents an opposite trend to AHC. The correlation analysis showed that there was a significant correlation between soil total organic carbon and each active carbon fractions (P < 0.05). (3) The soil carbon pool activity (CA), carbon pool activity index (CAI), and carbon pool management index (CPMI) under WP50% treatment were higher than other treatments. The sensitivity index of AHC and MBC was relatively high under the treatment of climate change.【Conclusion】In summary, the total organic carbon, the content and distribution ratio of active fractions of organic carbon, and the stability of the carbon pool in abandoned grassland of the loess-hilly area will be significantly improved under background warming and humid climate. This will contribute to the healthy development of the carbon pool. From a sensitivity point of view, AHC and MBC can be used as early important indicators of changes in soil organic carbon under warm and humid climates in the future. This study provides a theoretical and scientific basis for research on climate change and carbon pool management in fragile ecological areas.

    参考文献
    [1] Zhuoting W U,Dijkstra P,Koch G W,et al. Responses of terrestrial ecosystems to temperature and precipitation change:A meta-analysis of experimental manipulation[J]. Global Change Biology,2011,17(2):927-942
    [2] Crowther T W,Todd-Brown K E O,Rowe C W,et al. Quantifying global soil carbon losses in response to warming[J]. Nature,2016,540(7631):104-108.
    [3] Wang Q K. Responses of forest soil carbon pool and carbon cycle to the changes of carbon input[J]. Chinese Journal of Applied Ecology,2011,22(4):1075-1081.[王清奎. 碳输入方式对森林土壤碳库和碳循环的影响研究进展[J]. 应用生态学报,2011,22(4):1075-1081.]
    [4] Shi Z,Crowell S,Luo Y Q,et al. Model structures amplify uncertainty in predicted soil carbon responses to climate change[J]. Nature Communications,2018,9(1):2171.
    [5] Scharlemann J P,Tanner E V,Hiederer R,et al. Global soil carbon:Understanding and managing the largest terrestrial carbon pool[J]. Carbon Management,2014,5(1):81-91.
    [6] Chen P Q. Carbon cycle of earth system[M]. Beijing:Science Press,2004.[陈泮勤. 地球系统碳循环[M]. 北京:科学出版社,2004.]
    [7] Yu J,Fang L,Bian Z F,et al. A review of the composition of soil carbon pool[J]. Acta Ecologica Sinica,2014,34(17):4829-4838.[余健,房莉,卞正富,等. 土壤碳库构成研究进展[J]. 生态学报,2014,34(17):4829-4838.]
    [8] Wang Q K,Wang S L,Feng Z W,et al. Active soil organic matter and its relationship with soil quality[J]. Acta Ecologica Sinica,2005,25(3):513-519.[王清奎,汪思龙,冯宗炜,等. 土壤活性有机质及其与土壤质量的关系[J]. 生态学报,2005,25(3):513-519.]
    [9] Xi D,Weng H D,Hu Y L,et al. Effects of canopy nitrogen addition and understory removal on soil organic carbon fractions in a Chinese fir plantation[J]. Acta Ecologica Sinica,2021,41(21):8525-8534.[习丹,翁浩东,胡亚林,等. 林冠氮添加和林下植被去除对杉木林土壤有机碳组分的影响[J]. 生态学报,2021,41(21):8525-8534.]
    [10] Yang X Y,Lin L,Li Y,et al. Effects of warming and altered precipitation on soil physical properties and carbon pools in a Tibetan alpine grassland[J]. Acta Scientiarum Naturalium Universitatis Pekinensis,2017,53(4):765-774.[杨新宇,林笠,李颖,等. 青藏高原高寒草甸土壤物理性质及碳组分对增温和降水改变的响应[J]. 北京大学学报(自然科学版),2017,53(4):765-774.]
    [11] Zhou X,Chen C,Wang Y,et al. Warming rather than increased precipitation increases soil recalcitrant organic carbon in a semiarid grassland after 6 years of treatments[J]. PLoS One,2013,8(1):e53761
    [12] Chen Q Y,Niu B,Hu,Y L,et al. Warming and increased precipitation indirectly affect the composition and turnover of labile-fraction soil organic matter by directly affecting vegetation and microorganisms[J]. Science of the Total Environment,2020,714:136787.
    [13] Blair G J,Lefroy R D B,Lisle L. Soil carbon fractions based on their degree of oxidation,and the development of a carbon management index for agricultural systems[J]. Australian Journal of Agricultural Research,1995,46(7):1459-1466
    [14] Liang Q,Chen H Q,Gong Y S,et al. Effects of 15 years of manure and inorganic fertilizers on soil organic carbon fractions in a wheat-maize system in the North China Plain[J]. Nutrient Cycling in Agroecosystems,2012,92(1):21-33.
    [15] Tuo D F,Gao G Y,Chang R Y,et al. Effects of revegetation and precipitation gradient on soil carbon and nitrogen variations in deep profiles on the Loess Plateau of China[J]. Science of the Total Environment,2018,626:399-411.
    [16] Sun K H,Zeng X D,Li F. Climate change characteristics in ecological fragile zones in China during 1980-2014[J]. Climatic and Environmental Research,2019,24(4):455-468.[孙康慧,曾晓东,李芳. 1980~2014年中国生态脆弱区气候变化特征分析[J]. 气候与环境研究,2019,24(4):455-468.]
    [17] Zhang Y Q,Li Z C,Hou LY,et al. Effects of stand density on understory species diversity and soil nutrients in Chinese fir plantation[J]. Acta Pedologica Sinica,2020,57(1):239-250.[张勇强,李智超,厚凌宇,等.林分密度对杉木人工林下物种多样性和土壤养分的影响[J].土壤学报,2020,57(1):239-250.]
    [18] Bao S D. Analysis for soil and agrochemistry[M]. Beijing:China Agriculture Press,2000.[鲍士旦. 土壤农化分析[M]. 3版. 北京:中国农业出版社,2000.]
    [19] Yin D,Li H,Xu J B,et al. Composition characteristics of organic carbon pool in upland red soil under long-term application of straw and pig manure[J]. Acta Pedologica Sinica,2020,57(5):1259-1269.[殷丹,李欢,徐江兵,等. 长期配施秸秆与猪粪的红壤旱地有机碳库组成特征[J]. 土壤学报,2020,57(5):1259-1269.]
    [20] Wang C Y,He N P,Lü Y L. Latitudinal patterns and factors affecting different soil organic carbon fractions in the eastern forests of China[J]. Acta Ecologica Sinica,2016,36(11):3176-3188.[王春燕,何念鹏,吕瑜良. 中国东部森林土壤有机碳组分的纬度格局及其影响因子[J]. 生态学报,2016,36(11):3176-3188.]
    [21] Yan L J,Li G,Wu J Q,et al. Effects of four typical vegetations on soil active organic carbon and soil carbon in Loess Plateau[J]. Acta Ecologica Sinica,2019,39(15):5546-5554.[闫丽娟,李广,吴江琪,等. 黄土高原4 种典型植被对土壤活性有机碳及土壤碳库的影响[J]. 生态学报,2019,39(15):5546-5554.]
    [22] Belay-Tedla A,Zhou X,Su B,et al. Labile,recalcitrant,and microbial carbon and nitrogen pools of a tallgrass prairie soil in the US Great Plains subjected to experimental warming and clipping[J]. Soil Biology and Biochemistry,2009,41(1):110-116
    [23] Fang X,Zhou G,Qu C,et al. Translocating subtropical forest soils to a warmer region alters microbial communities and increases the decomposition of mineral-associated organic carbon[J]. Soil Biology and Biochemistry,2020,142:107707.
    [24] Zhong Z,Wu S,Lu X,et al. Organic carbon,nitrogen accumulation,and soil aggregate dynamics as affected by vegetation restoration patterns in the Loess Plateau of China[J]. Catena,2021,196:104867.
    [25] Hoeppner,SS,Dukes,et al. Interactive responses of old-field plant growth and composition to warming and precipitation[J]. Global Change Biology,2012,18(5):1754-1768.
    [26] Alon M,Sternberg M. Effects of extreme drought on primary production,species composition and species diversity of a Mediterranean annual plant community[J]. Journal of Vegetation Science,2019,30(6):1045-1055.
    [27] Chen Q,Lei T,Wu Y,et al. Comparison of soil organic matter transformation processes in different alpine ecosystems in the Qinghai‐Tibet Plateau[J]. Journal of Geophysical Research:Biogeosciences,2019,124(1):33-45.
    [28] Althuizen I H J,Lee H,Sarneel J M,et al. Long-term climate regime modulates the impact of short-term climate variability on decomposition in alpine grassland soils[J]. Ecosystems,2018,21(8):1580-1592.
    [29] Yang H,Wu M,Liu W,et al. Community structure and composition in response to climate change in a temperate steppe[J]. Global Change Biology,2011,17(1):452-465.
    [30] Liu F R,Zhang Y M,Luo J X. The effects of experimental warming and CO2 concentration doubling on soil organic carbon fractions of a montane coniferous forest on the eastern Qinghai-Tibetan Plateau[J]. European Journal of Forest Research,2018,137(2):211-221.
    [31] Xu X,Sherry R A,Niu S L,et al. Long-term experimental warming decreased labile soil organic carbon in a tallgrass prairie[J]. Plant and Soil,2012,361(1/2):307-315.
    [32] Teng Z,Cao X Q,Sun M Y,et al. Effect of different ecological restoration patterns on soil labile organic carbon and carbon pool management index of lakeside wetland of Chaohu Lake[J]. Ecology and Environmental Sciences,2019,28(4):752-760.[滕臻,曹小青,孙孟瑶,等. 不同生态恢复模式对巢湖湖滨湿地土壤活性碳库及其管理指数的影响[J]. 生态环境学报,2019,28(4):752-760.]
    相似文献
    引证文献
    网友评论
    网友评论
    分享到微博
    发 布
引用本文

王兴,钟泽坤,王佳懿,简俊楠,杨改河,任成杰,韩新辉.黄土高原撂荒草地土壤碳库对两年增温增雨的响应[J].土壤学报,2023,60(2):523-534. DOI:10.11766/trxb202106120307 WANG Xing, ZHONG Zekun, WANG Jiayi, JIAN Junnan, YANG Gaihe, REN Chengjie, HAN Xinhui. Responses of Soil Carbon Pool of Abandoned Grassland on the Loess Plateau to Two-years Warming and Increased Precipitation[J]. Acta Pedologica Sinica,2023,60(2):523-534.

复制
分享
文章指标
  • 点击次数:530
  • 下载次数: 1543
  • HTML阅读次数: 1416
  • 引用次数: 0
历史
  • 收稿日期:2021-06-12
  • 最后修改日期:2021-10-07
  • 录用日期:2021-12-02
  • 在线发布日期: 2021-12-06
  • 出版日期: 2023-03-28
文章二维码