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A Study on Carbon Sink of Reforestation Under Different 'Grain for Green' Models in the Southern Ningxia Province of Loess Hilly Region

机译:黄土丘陵地区南部南部不同“绿色”模型中不同“绿色”模型的重新造林碳汇研究

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Based on biomass collected from field surveys and carbon contents determined in laboratory, carbon storage of different reforestation under different models for conversion of cropland to forestland or pasture and its distribution characteristics were examined. The results showed as follow: the carbon stock of the different reforestation models is L. gmelini (106.12 t-hm~(-2)) > P. sibirica (85.08 t-hm~(-2)) > P. davidiana (77.78 t-hm~(-2)) > Hippophae rhamnoides (63.29 t-hm~(-2)) > Caragana korshinskii (52.82 t-hm~(-2)). Compared to that of the sloping cropland (59.55 thm~(-2)), carbon densities of P. sibirica and L gmelini ecosystems increased by 42.90% and 78.20%, respectively; for the Hippophae rhamnoides and P. davidiana ecosystems, the number increased by 6.28% and 30.61%; carbon content in soil layer between 0-100cm reduced significantly with the depth, the distribution pattern of carbon sequestration was in the order of soil layer > vegetation layer.
机译:基于从实验室调查和实验室中确定的碳含量收集的生物量,检查了不同模型中不同重新造林的碳储存,以便将农田转换为林地或牧场及其分布特征。结果表明如下:不同重新造林模型的碳库存是L.gmelini(106.12 T-HM〜(-2))> P.Sibirica(85.08 T-HM〜(-2))> P. Davidiana(77.78 T-HM〜(-2))> Hippophae rhamnoides(63.29 T-HM〜(2))> Caragana Korshinskii(52.82 T-HM〜(-2))。与倾斜的农作物(59.55吨〜(-2))相比,P.Sibirica和L Gmelini生态系统的碳密度分别增加了42.90%和78.20%;对于Hippophae rhamnoides和P. Davidiana生态系统,该数字增加了6.28%和30.61%;土壤层中的碳含量在0-100cm之间明显减小,深度显着,碳封存的分布模式为土壤层>植被层的顺序。

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