张琛悦, 赵霞, 辛玉春, 唐文家, 王蕾. 青海省草地生态系统碳储量及其分布特征[J]. 北京师范大学学报(自然科学版), 2022, 58(2): 286-292. DOI: 10.12202/j.0476-0301.2021105
引用本文: 张琛悦, 赵霞, 辛玉春, 唐文家, 王蕾. 青海省草地生态系统碳储量及其分布特征[J]. 北京师范大学学报(自然科学版), 2022, 58(2): 286-292. DOI: 10.12202/j.0476-0301.2021105
ZHANG Chenyue, ZHAO Xia, XIN Yuchun, TANG Wenjia, WANG Lei. Carbon storage and distribution of grassland ecosystems in Qinghai Province[J]. Journal of Beijing Normal University(Natural Science), 2022, 58(2): 286-292. DOI: 10.12202/j.0476-0301.2021105
Citation: ZHANG Chenyue, ZHAO Xia, XIN Yuchun, TANG Wenjia, WANG Lei. Carbon storage and distribution of grassland ecosystems in Qinghai Province[J]. Journal of Beijing Normal University(Natural Science), 2022, 58(2): 286-292. DOI: 10.12202/j.0476-0301.2021105

青海省草地生态系统碳储量及其分布特征

Carbon storage and distribution of grassland ecosystems in Qinghai Province

  • 摘要: 以第2次土壤普查形成的土壤图和草地资源清查图为本底,通过文献搜集及实测数据的结合,对青海省草地的碳储量进行了估算.结果表明:1)青海省草地生态系统碳储量约为6.12 Pg,平均碳面密度为18.08 kg·m−2,其中:地上植被碳储量(包括凋落物)为0.0097 Pg,平均碳面密度为0.03 kg·m−2;地下植被碳储量为0.0967 Pg,平均碳面密度为0.29 kg·m−2;土壤有机碳储量为6.01 Pg,平均碳面密度为17.76 kg·m−2;土壤储存的有机碳是植被的54倍多.2)从9大草地类来看,总碳储量从大到小依次为高寒草甸类(3.64 Pg)、高寒草原类(0.94 Pg)、低地草甸类(0.61 Pg)、温性草原类(0.35 Pg)、温性荒漠类(0.33 Pg)、温性荒漠草原类(0.08 Pg)、山地草甸类(0.08 Pg)、高寒草甸草原类(0.05 Pg)、高寒荒漠类(0.04 Pg);从5大功能区来看,总碳储量从大到小依次为三江源地区(3.95 Pg)、柴达木盆地(1.31 Pg)、祁连山地区(0.45 Pg)、青海湖流域(0.31 Pg)、河湟谷地(0.10 Pg).3)从9大草地类总碳面密度来看,低地草甸类的总碳面密度最高(57.37 kg·m−2),温性草原类的最低(14.04 kg·m−2);从5大功能区总碳面密度来看,柴达木盆地的最高(24.41 kg·m−2),河湟谷地的最低(14.05 kg·m−2).

     

    Abstract: Based on the soil map from the second soil census and grassland resource inventory map , the carbon storage of grassland in Qinghai province was estimated by literature collection and measured data.And it turns out, carbon storage was about 6.12 Pg, with an average carbon surface density of 18.08 kg·m−2.Aboveground vegetation carbon storage (including litters) was 0.0097 Pg, with an average carbon surface density of 0.03 kg·m−2.Carbon storage of underground vegetation was 0.0967 Pg, with average carbon surface density at 0.29 kg·m−2.Soil organic carbon storage was 6.01 Pg, carbon surface density at 17.76 kg·m−2.Soil was found to store > 54 times as much carbon as vegetation.Of the nine grassland types in the region, total carbon storage was: alpine meadow (3.64 Pg), alpine steppe (0.94 Pg), lowland meadow (0.61 Pg), warm steppe (0.35 Pg), warm desert (0.33 Pg), warm desert steppe (0.08 Pg), mountain meadow (0.08 Pg) , alpine meadow steppe (0.05 Pg) , alpine desert (0.04 Pg).Of the five functional areas, total carbon storage was:Sanjiangyuan region, Qaidam Basin, Qilian Mountain area, Qinghai Lake basin, Hehuang Valley.The total carbon surface density in the nine different grassland types was highest in lowland meadow (57.37 kg·m−2), lowest in warm steppe (14.04 kg·m−2).Total carbon density in five functional areas was highest in Qaidam Basin (24.41 kg·m−2) but lowest in Hehuang Valley (14.05 kg·m−2).

     

/

返回文章
返回