首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Pedological properties related to formation and functions of ancient ridge and furrow cultivation in Central and Northern Germany
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Pedological properties related to formation and functions of ancient ridge and furrow cultivation in Central and Northern Germany

机译:与德国中部和北部古岭和沟草栽培相关的Podologology属性

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摘要

Ridge and furrow cultivation is an example for a historic agriculture technique that has been very common in Germany, especially during medieval times. It seemed to be well-known how the ridge and furrows (RIFUs) were used and formed but previous studies came to contradictory conclusions which raised additional questions concerning their formation. Furthermore, the RIFUs' morphological and physicochemical soil properties and their influence on current soils that developed after the RIFUs had been abandoned are not fully understood. In order to answer these questions, morphological and physicochemical analyses (pH, EC, TOC, TN, delta N-15, C:N ratios, "Olsen P", soil texture) were conducted on 11 preserved RIFUs in forested areas of Northern and Central Germany. The results showed that the studied RIFUs occur on sites with different properties (e.g. soil texture, inclination, vegetation) and presented various morphological shapes. They are also characterised by differences in the formation of soil horizons and general low TN (<1.5 g kg(-1)) and TOC (<10 g kg(-1)) contents. However, higher contents at some sites comparing to their references, indicated that the RIFU cultivation promoted a slight long-lasting soil improvement if not induced by secondary soil processes after RIFU use. Moreover, for some sites, high P and delta N-15 values may suggest the application of manure. Recent morphological changes also had a significant influence on some study sites. In summary, neither the formation and agricultural strategies of RIFU cultivation nor their function and any influences on the current soil and woodland characteristics can be regarded as identical for all RIFU sites.
机译:垄沟耕作是一种历史悠久的农业技术,在德国非常常见,尤其是在中世纪。人们似乎很清楚垄沟(RIFUs)是如何使用和形成的,但之前的研究得出了相互矛盾的结论,这就提出了有关其形成的其他问题。此外,尚未完全了解裂谷的形态和物理化学土壤特性及其对裂谷被废弃后形成的现有土壤的影响。为了回答这些问题,对德国北部和中部森林地区11个保存的裂谷进行了形态学和物理化学分析(pH、EC、TOC、TN、δN-15、C:N比率、“奥尔森P”、土壤质地)。结果表明,所研究的裂谷出现在具有不同性质(如土壤质地、倾斜度、植被)的场地上,呈现出不同的形态。它们的特点还包括土壤层的形成和一般低TN(<1.5 g kg(-1))和TOC(<10 g kg(-1))含量的差异。然而,与他们的参考相比,一些地点的含量更高,这表明,如果不是由使用RIFU后的次生土壤过程诱导,RIFU种植促进了轻微的长期土壤改良。此外,对于某些地点,高P和δN-15值可能表明施用肥料。最近的形态学变化也对一些研究地点产生了重大影响。综上所述,无论是里福种植的形成和农业策略,还是它们的功能,以及对当前土壤和林地特征的任何影响,都不能被视为所有里福地点都是相同的。

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