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The potential for gamma-emitting radionuclides to contribute to an understanding of erosion processes in South Africa

机译:发射伽马射线放射性核素的潜力有助于了解南非的腐蚀过程

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摘要

Several research projects undertaken by the authors and others over the last 14 years have used fallout and geogenic radionuclides for understanding erosion processes and sediment yield dynamics in South Africa over the last 100–200 years as European settlers colonised the interior plains and plateaux of the country and imported new livestock and farming techniques to the region. These projects have used two fallout radionuclides (210Pb and 137Cs) to date sediments accumulating in reservoirs, farm dams, wetlands, alluvial fans and floodouts and have used other fallout nuclides (7Be) and long-lived geogenic radionuclides (e.g. 40K, 235U) as part of a composite fingerprint exploring contemporary sediment sources and changes to sources through time. While successful in many parts of the world, applying these techniques in Southern Africa has posed a number of challenges often not encountered elsewhere. Here we explore some of the benefits and challenges in using gamma-emitting radionuclides, especially 137Cs, in these landscapes. Benefits include the potential for discriminating gully sidewall from topsoil sources, which has helped to identify contemporary gully systems as sediment conduits, rather than sources, and for providing a time-synchronous marker horizon in a range of sedimentary environments that has helped to develop robust chronologies. Challenges include the spatial variability in soil cover on steep rocky hillslopes, which is likely to challenge assumptions about the uniformity of initial fallout nuclide distribution, the paucity of stable (non-eroding) sites in order to estimate atmospheric fallout inventories, and the limited success of 210Pb dating in some rapidly accumulating high altitude catchments where sediments often comprise significant amounts of sand and gravel. Despite these challenges we present evidence suggesting that the use of gamma-emitting radionuclides can make a significant contribution to our understanding of erosion processes and sediment yield dynamics. Future research highlighted in the conclusion will try to address current challenges and outline new projects established to address them more fully.
机译:在过去的14年中,作者和其他人进行的一些研究项目已经使用沉降物和地核放射性核素来了解过去100-200年间随着欧洲定居者在南非的内陆平原和高原定居,南非的侵蚀过程和沉积物产量动态。并向该地区引进了新的牲畜和耕作技术。这些项目使用了两个放射性放射性核素(210Pb和137Cs)来确定在水库,农田水坝,湿地,冲积扇和洪水中堆积的沉积物,并使用了其他放射性核素(7Be)和长寿命的地源放射性核素(例如40K,235U)作为沉积物。复合指纹的一部分,用于探索当代沉积物的来源以及时间的变化。尽管在世界许多地方都取得了成功,但在南部非洲应用这些技术带来了许多其他地方通常没有遇到的挑战。在这里,我们探讨了在这些环境中使用发射伽马射线的放射性核素(尤其是137C)的好处和挑战。好处包括将沟渠侧壁与表土来源区分开来的潜力,这有助于将当代的沟渠系统识别为沉积物管道而不是来源,并在一定范围的沉积环境中提供时间同步的标记层,这有助于建立可靠的年代学。挑战包括陡峭多岩石的山坡上土壤覆盖物的空间变异性,这可能会挑战有关初始沉降核素分布的均匀性,稳定(无侵蚀)场地的稀缺性以估算大气沉降清单的假设以及成功的有限性。在一些快速聚集的高海拔流域,其中210Pb的测年表明沉积物通常包含大量的沙子和砾石。尽管存在这些挑战,但我们提供的证据表明,使用发射伽马射线的放射性核素可以对我们对侵蚀过程和沉积物产量动态的理解做出重大贡献。结论中强调的未来研究将尝试应对当前挑战,并概述为更全面地应对这些挑战而建立的新项目。

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