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The dynamics of cultivation and floods in arable lands of Central Argentina

机译:阿根廷中部耕地的耕作与洪水动态

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Although floods in watersheds have been associated with land-use changesince ancient times, the dynamics of flooding is still incompletelyunderstood. In this paper we explored the relations between rainfall,groundwater level, and cultivation to explain the dynamics of floods in theextremely flat and valuable arable lands of the Quinto river watershed, incentral Argentina. The analysis involved an area of 12.4 million hectareduring a 26-year period (1978–2003), which comprised two extensive floodingepisodes in 1983–1988 and 1996–2003. Supported by information from surveysas well as field and remote sensing measurements, we explored thecorrelation among precipitation, groundwater levels, flooded area and landuse. Flood extension was associated to the dynamics of groundwater level.While no correlation with rainfall was recorded in lowlands, a significantcorrelation (P<0.01) between groundwater and rainfall in highlands wasfound when estimations comprise a time lag of one year. Correlationsbetween groundwater level and flood extension were positive in all cases,but while highly significant relations (P<0.01) were found in highlands,non significant relations (P
机译:尽管自古以来流域的洪水与土地利用的变化有关,但对洪水的动态性仍未完全了解。在本文中,我们探索了降雨量,地下水位和耕作之间的关系,以解释阿根廷中部Quinto河流域的极其平坦和宝贵的耕地中的洪水动态。该分析涉及一个为期26年(1978年至2003年)的面积为1,240万公顷的土地,其中包括1983年至1988年和1996年至2003年的两次泛滥洪水。在来自调查以及野外和遥感测量的信息的支持下,我们探索了降水,地下水位,洪水区域和土地利用之间的相关性。洪水的扩展与地下水位的动态有关。虽然在低地上没有与降雨相关的记录,但当估算值包含一个时滞时,发现高地地下水与降雨之间存在显着的相关性( P <0.01)。年。在所有情况下,地下水位与洪水泛滥之间的相关性均为正相关,但在高地却发现高度相关性( P <0.01),而非显着性相关性( P

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