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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Terrace agriculture in a mountainous arid environment - A study of soil quality and regolith provenance: Jabal Akhdar (Oman)
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Terrace agriculture in a mountainous arid environment - A study of soil quality and regolith provenance: Jabal Akhdar (Oman)

机译:山区农业在山区干旱环境中 - 对土壤质量和鲁代术来源的研究:Jabal Akhdar(阿曼)

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In the Sultanate of Oman remnants of deteriorating terrace agricultural systems offer important insights into long-term human adaptation in the arid tropics. Irrigation and terrace agriculture in the mountainous Jabal Akhdar region reveal historic agricultural practices in a rugged, high elevation context. The present study examines soil quality and regolith provenance in abandoned agricultural soil terraces. Three soil profiles in each of the Villages of Hadash and Wijma were excavated and analyzed. Physical, chemical and mineralogical analyses were conducted for all soil horizons. In addition, six other soils, 3 possible soil parent rocks (regolith) and soil's bedrock were collected. Soil ages were constrained by C-14 assays and stable isotope, (C-13 and O-18) on the bulk carbonates in the calcrete (caliche). The results demonstrate that both sites display poor soil quality with very low average total organic carbon (TOC) (6.2-5.0 g kg(-1)) and mean weight diameter (MWD; 0.27-0.48 mm), with low water stable aggregate content ( < 42%). All the geochemical, mineralogical and the thin section analyses show that the soils exhibit unique characteristics that differ from those of other sediments (possible parent regolith) and soils in the vicinity. The finding of ostracod shells in the soil terraces in both areas and C-14 dating of calcrete (10.193 +/- 30-13.887 +/- 40 a BP) indicate that regolith was human-transported to terraces to create soil. The C-14 ages of the bulk carbonates match well with a dry period of high calcite precipitation contemporaneous to the Younger Dryas. The Hadash and Wijma soil terraces are located similar to 45 km away from each other, but still display significant similarities in terms of regolith provenance and soil development and were likely filled with regolith from the same source. These results offer new perspective on agricultural terrace development and oasis agriculture in a rugged, high-elevation, arid environment.
机译:在恶化露台的阿曼遗址的苏丹国农业系统在干旱热带地区的长期人类适应方面提供了重要的见解。 Mountainous Jabal Akhdar Region中的灌溉和露台农业揭示了崎岖,高海拔环境中的历史农业实践。本研究研究了废弃的农业土壤露台中的土壤质量和鲁代质量。挖掘和分析了每个哈什和Wijma村庄的三种土壤曲线。为所有土壤视野进行了物理,化学和矿物学分析。此外,收集了六个其他土壤,3种可能的土壤父母岩石(凝固)和土壤的基岩。土壤时代受C-14测定和稳定同位素,(C-13和O-18)在Calcrete(Caliche)的批量碳酸盐上约束。结果表明,两种部位显示出差的土壤质量,平均总有机碳(TOC)(6.2-5.0g kg(-1))和平均重量直径(mwd; 0.27-0.48 mm),具有低水稳定的骨料含量(<42%)。所有地球化学,矿物学和薄剖面分析表明,土壤具有与附近其他沉积物(可能的父母regolith)和土壤不同的独特特征。在土壤露台中发现奥特拉科德壳在屠克的C-14约会(10.193 +/- 30-13.887 +/- 40 A BP)中表明,概述是人类运送到露台以产生土壤。批量碳酸盐盐的C-14岁与干燥时期与较年轻的Dratas一起出现的干燥时期。哈什和威娘土壤露台与彼此相比,距离距离45公里,但仍然展示了极大的原子能和土壤开发方面的显着相似之处,并且可能从同一来源充满了极乐的推出。这些结果在崎岖,高度高度,干旱的环境中提供了新的农业露台开发和绿洲农业的新视角。

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