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A Pedogenic View of Ecosystem Restoration

机译:生态恢复的成因观

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Ecosystem response to site restoration depends in part on the physical, chemical, and biological properties of soils. Soil properties are influenced by the factors and processes of soil formation that determine soil profile characteristics and pedogenic pathways for soils. Loss of integrity of the original soil profiles or disruption of a past pedogenic pathway from site disturbance may limit the success of restoration if assessment is based on comparisons to previous ecosystems or mature reference systems. New profile characteristics and a pedogenic pathway will emerge over time if materials are used to construct soil profiles or if topsoil or organic matter amendments are added to enhance ecosystem develop ment during site restoration. Ecosystem restoration should include the following pedogenic evaluation of soils: 1) the integrity of existing soil profiles of a degraded site; 2) the soil types (based on soil orders) and past pedogenic pathways for sites of intact soil profiles or sites that require only surface horizon modification; 3) the relative contributions of soil forming factors and processes on future pedogenesis; 4) the conditions that promote or hinder horizon development; and 5) predictions of pedogenic pathways and potential soil types after site restoration. Understanding pedogenesis as a component of ecosystem restoration will improve our understanding of how soils influence ecosystem development, as well as our ability to predict potential success of ecosystem restoration.
机译:生态系统对场地恢复的反应部分取决于土壤的物理,化学和生物学特性。土壤特性受决定土壤剖面特征和土壤成岩途径的土壤形成因素和过程的影响。如果评估是基于与先前生态系统或成熟参考系统的比较而进行的,则原始土壤剖面完整性的丧失或场地干扰造成的过去的成岩途径的破坏可能会限制恢复的成功。如果使用材料构造土壤剖面或添加表土或有机质改良剂以增强场地恢复过程中的生态系统发育,则随着时间的流逝将出现新的剖面特征和成岩途径。生态系统的恢复应包括以下土壤成因评估:1)退化地点现有土壤剖面的完整性; 2)土壤类型(基于土壤次序)和过去的成岩途径,用于完整土壤剖面的地点或仅需要改变地表水平的地点; 3)土壤形成因子和过程对未来成岩作用的相对贡献; 4)促进或阻碍视界发展的条件; 5)场地恢复后的成土途径和潜在土壤类型的预测。了解成土作用是生态系统恢复的组成部分,将有助于我们更好地理解土壤如何影响生态系统的发展,以及我们预测生态系统恢复潜在成功的能力。

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