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土壤电导率、酸度和有机质对野生杏仁和麻黄下土壤固碳能力的影响

Effects of electrical conductivity, acidity, and organic matter on carbon sequestration ability of soils beneath Amygdalus scoparia and Ephedra procera

  • 摘要:
    目的 植物和土壤的固碳在碳循环中发挥着至关重要的作用,有助于降低二氧化碳水平并提高土壤生产力。识别具有高固碳潜力的植物物种对于牧场的恢复和维护至关重要。
    方法 本研究考察2种植物野生杏仁(Amygdalus scoparia)和麻黄(Ephedra procera)的根、茎和叶等不同器官的固碳能力。通过采集植物基部和株间0−15 cm和15−30 cm深度的土壤样本,评估土壤特性和碳固存水平。第1个试验包含2个因素:植物种类(野生杏仁和麻黄)和植物器官(叶、茎和根)。第2个试验也包含2个因素。第1个因素是3种土壤团块类型(分别采集于野生杏仁、麻黄和对照植物的基部),第2个因素是土壤采样深度(0–15 cm和15–30 cm)。试验在伊朗法尔斯省多拉塔巴德地区进行。
    结果 野生杏仁下方的土壤有机碳、有机质和碳固存量均高于麻黄和对照土壤。此外,0–15 cm深度的土壤中这些指标的含量也高于15–30 cm深度的土壤。随着土壤深度的增加,有机碳、有机质和固碳量均有所下降,而土壤酸度则有所上升。然而,2个深度之间的土壤含水量差异并不显著。土壤类型和深度对电导率有显著影响。对照土壤的电导率显著高于麻黄和野生杏仁土壤。此外,平均值表明土壤表层的电导率显著高于其他深度。值得注意的是,对照土壤的2个深度在所有处理中均表现出最高的电导率,且与其他组存在显著差异。土壤的高电导率可能表明其盐度较高。野生杏仁和麻黄下方的土壤在不同深度之间的黏粒含量存在显著差异,其中0−15 cm深度的黏粒含量在所有处理中最高。
    结论 野生杏仁组织中储存的有机碳和有机质含量显著高于麻黄。由于耐旱性强,野生杏仁的栽培非常可行;而其他需水量大的物种,若在大片牧场种植,则可能需要精细的管理。有机碳在决定土壤固碳量方面比有机质发挥着更重要的作用。土壤质地,尤其是黏土含量,是影响固碳的最重要因素之一。

     

    Abstract:
    Objective Carbon sequestration in plants and soils plays a crucial role in the carbon cycle, contributing to the reduction of carbon dioxide levels and enhancing soil productivity. Identifying plant species with high carbon sequestration potential is essential for the restoration and maintenance of rangelands.
    Methods This study examined carbon sequestration in various plant organs—roots, stems, and leaves—of two plant species: wild almond (Amygdalus scoparia) and Ephedra (Ephedra procera). In addition, soil characteristics and carbon sequestration levels were assessed by collecting soil samples from depths of 0–15 cm and 15–30 cm, both at the base of plants and in the inter-plant spaces. In this study, the first experiment comprised two factors: plant species (A. scoparia and E. procera) and plant organs (leaves, stems, and roots). The second experiment also had two factors. The first factor was three types of soil masses (collected at the bases of A. scoparia, E. procera, and the control), and the second factor was soil sampling depth (0–15 cm and 15–30 cm). The study was conducted in the Dolatabad region of Fars Province, Iran.
    Results Soil beneath A. scoparia had higher levels of organic carbon, organic matter, and carbon sequestration than E. procera and control soils. Furthermore, the 0–15 cm depth showed greater levels of these factors than the 15–30 cm depth. As soil depth increased, organic carbon, organic matter, and carbon sequestration decreased, while soil acidity increased. However, soil moisture content did not significantly vary between the two depths. Soil type and depth had significant effects on electrical conductivity. The control soil exhibited a significantly higher electrical conductivity than E. procera and A. scoparia soils. Additionally, average values indicated that electrical conductivity was significantly greater at the soil surface. Notably, both depths of the control soil showed the highest conductivity among all treatments, with the control differing significantly from the other groups. High electrical conductivity in the soil may indicate high salinity levels. Soils beneath A. scoparia and E. procera showed significant differences in clay content between the two soil depths, with the 0–15 cm depth exhibiting the highest clay content among all treatments.
    Conclusions A. scoparia is found to store significantly higher amounts of organic carbon and organic matter in its tissues than E. procera. The cultivation of A. scoparia is highly feasible due to its high tolerance to drought, whereas other water-dependent species may require extensive management if cultivated in vast areas of rangelands. Organic carbon plays a more significant role than organic matter in determining the extent of carbon sequestration in the soil. Soil texture, particularly clay content, emerges as one of the most influential factors in carbon sequestration.

     

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