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首页> 外文期刊>Quaternary International >Dirt road: A geomorphological and geochemical record of Late-Holocene human activity in the catchment of Lake Radacz (Central Pomerania, Poland)
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Dirt road: A geomorphological and geochemical record of Late-Holocene human activity in the catchment of Lake Radacz (Central Pomerania, Poland)

机译:土路:拉达奇湖(波兰中波美拉尼亚)流域晚全新世人类活动的地貌和地球化学记录

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摘要

The paper offers a discussion of the record of human activity in the relief and sediments of a selected lake catchment in Central Pomerania in Poland. One of the basic markers of human activity here is a change in the lake-water level. The dropping level (on average, 1 m/100 years) made it possible for people to develop successively exposed stretches of land along the shore. An analysis of the Polish National Archeological Records and archival maps showed that human development and impact appeared in the lakeshore zone as early as the Neolithic. In Central Pomerania, the changes were especially intensive in the Late Holocene; in the catchment of the lake under study they included a 100% increase in the length of nearby roads. In the archives of its paleoenvironmental data, most traces have been left on farming terraces, while a poorly studied form of record of human activity is a dirt road running parallel to the shoreline. Geodetic and geochemical examination has revealed that the road is a stimulant of change. Its wheeled traffic mixes the accumulated and eroded material, and this causes changes in the shoreline section: the road cutting, which is 2 mwide, deepened, while material accumulates in the form of 0.5-m-wide lateral bars. The compaction of the material brings about changes in the structure of the ground or soil (its density, porosity, compactness, moisture), which affects its level of oxygenation and water-logging, and, consequently, its iron content. To establish this, a speciation analysis was carried out using the Fe(III)/Fe(II) ratio. It was determined that the lower the ratio, the higher the susceptibility of land to deformation owing to an increase in soil density, a drop in its water capacity, reduction conditions, and the predominance of Fe(II). The research discussed here is only a pilot study, but the authors see extensive opportunities for using speciation analysis in geoarcheology. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译:本文讨论了波兰波美拉尼亚中部某个湖泊集水区的浮雕和沉积物中人类活动的记录。这里人类活动的基本标志之一是湖泊水位的变化。水位的下降(平均1 m / 100年)使人们有可能沿海岸陆续开发裸露的土地。对波兰国家考古记录和档案地图的分析表明,人类发展和影响最早出现在新石器时代的湖岸地区。在中波美拉尼亚,新世晚期的变化尤为明显。在所研究的湖泊集水区,附近道路的长度增加了100%。在其古环境数据档案中,大多数痕迹都留在了耕作梯田上,而对人类活动记录的研究很少,是一条平行于海岸线的土路。大地测量和地球化学检查显示这条路是变化的刺激物。它的轮式交通将积聚的和侵蚀的物料混合在一起,这会导致海岸线部分发生变化:2 m宽的道路切割加深,而物料以0.5 m宽的侧杆形式积聚。材料的压实会导致地面或土壤的结构发生变化(其密度,孔隙率,致密性,湿度),这会影响其氧化和浸水程度,进而影响其铁含量。为了确定这一点,使用Fe(III)/ Fe(II)比进行了形态分析。已确定该比率越低,由于土壤密度增加,水容量下降,还原条件和Fe(II)占优势,土地对变形的敏感性就越高。这里讨论的研究只是一项初步研究,但是作者发现在地球考古学中使用形态分析的广泛机会。 (C)2015 Elsevier Ltd和INQUA。版权所有。

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