孟加拉国农业生态区第9区土地利用对土壤固碳潜力的影响

S. Yeasmin, Eshara Jahan, A. Islam, M. Anwar, T. Hoque
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摘要

本研究旨在确定不同土地利用方式(农田、果园、草地和休耕)对0 ~ 10 cm和40 ~ 50 cm深度土壤有机碳库的影响。颗粒有机质(POM)(> 53µm)和矿物有机质(MOM)(< 53µm)池从大块土壤中分离出来,进行OC和N分析。在两个深度,草地土壤的OC值(0.96 ~ 1.47%)和N值(0.084 ~ 0.095%)均显著高于其他土地利用。表层土壤OC最低的是耕地土壤(0.83%),次表层土壤OC最低的是休耕地土壤(0.75%),果园土壤在两个深度的OC均为中等。深度显示OC分布有显著差异。表层土壤的有机碳含量高于亚表层土壤,这可以解释为表层土壤不断添加有机残留物(作物/叶片/干草)。不同土地利用方式土壤中POM和MOM组分的分布存在差异。有趣的是,与相对较少受干扰的草地和休耕地土壤相比,农田和果园土壤的MOM-OC (MOC)高于POC (POC)。在不同土地利用方式下,有机质池的OC和N含量存在显著差异。在表层土壤中,耕地土壤POC含量最低,果园和休耕地土壤POC含量相对较高。MOC含量以闲耕地最高(2.73%),果园最低(1.30%),农田中等。在次表层土壤中,有机质含量高于表层土壤,有机质在POM和MOM之间的分布趋势不同。草地土壤有机碳含量最高(2.89 ~ 3.10%),农田>果园>休耕。这些结果表明,在农田中,土壤扰动只会使土壤中最不稳定的POM库中的有机碳消耗殆尽,而稳定的MOM库中的有机碳几乎保持不变。对原生土壤条件(如草地)的干扰较少并不总是有利于提高/维持有机碳,而是取决于植被覆盖土壤中添加的有机碳的质量和数量。
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Impact of land use on carbon sequestration potential of soils in Agroecological Zone-9 of Bangladesh
This study aimed to ascertain the effect of land uses (cropland, orchard, grassland, and fallow) on soil OC pools in two depths (0–10 and 40–50 cm). Particulate organic matter (POM) (> 53 µm) and mineral associated OM (MOM) (< 53 µm) pools were physically separated from bulk soils and analyzed for OC and N analysis. For both depths, the soil from grassland showed considerably higher OC (0.96-1.47%) and N (0.084-0.095%) values than the other land uses. In surface depth, the lowest OC was found in cropland soil (0.83%) and in sub-surface, it was in fallow land soil (0.75%), whereas the orchard soil had moderate OC in both depths. Depth showed significant differences in OC distribution. Surface soils had higher OC than the sub-surface soils which can be explained by the continuous addition of organic residues (crop/leaf/dried grasses) on the top soil. The distribution of POM and MOM fractions among the soils of different land uses were different. Interestingly, cropland and orchard soils had higher MOM-OC (MOC) than POM-OC (POC) in comparison to the relatively less disturbed grassland and fallow land soils. The amount of OC and N in OM pools was significantly different among the land uses in both depths. In surface depth, cropland soil showed the lowest POC content whereas the orchard and fallow land soils showed relatively higher. The MOC content was highest in fallow land (2.73%), lowest in orchard (1.30%) and cropland had moderate amount. In sub-surface depth, amount of OC was higher than surface soils and the trend of OC distribution between POM and MOM was different. Grassland soil had the highest OC (2.89-3.10%) for both fractions, followed by cropland > orchard > fallow. These findings showed that in cropland disturbance in soil could aid in depleting OC only from the most labile POM pool keeping the OC almost intact in stable MOM pool. Less disturbance in native soil condition such as grassland does not always benefit in enhancing/maintaining OC, rather it depends on the quality and quantity of OM added in the soils from the vegetation cover.
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