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The influence of flood duration on the surface soil properties and grazing management of karst wetlands (turloughs) in Ireland

机译:洪水持续时间对爱尔兰喀斯特湿地(洼地)地表土壤特性和放牧管理的影响

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摘要

Irish turloughs are hydrologically dynamic karst wetlands that are frequently used as marginal grazing land. We hypothesised that flood duration (FD) is a key driver of the spatial distribution of selected soil properties, and consequently turlough grazing practices. Six soil samples were collected during dry periods from eighteen turloughs between 2006 and 2008. Samples (n = 104) were analysed for pH, organic matter (OM) content, calcium carbonate content (CaCO3), sand/silt/clay content (INORG), total nitrogen (TN) and total phosphorus (TP). Data on flooding duration, flood frequency, grazing regime and vegetation type were collated for each soil sampling point. Multivariate and univariate statistical analyses were used to examine the relationships between soil properties, grazing regime and flooding variables. There was a positive association between CaCO3, FD and sedge-dominated communities, whereas INORG had a positive association with grazing and grassland. There was a strong positive association between TN, TP, OM and soil depth rather than FD, and OM was found to be an efficient predictor of TN. Extended FDs in ephemeral karst wetlands are likely to increase the extent and degree of calcium carbonate accumulation in soils, thus, reducing the grazing potential of land.
机译:爱尔兰洼地是水文动态的喀斯特湿地,经常被用作边缘放牧地。我们假设洪水持续时间(FD)是选定土壤性质的空间分布的主要驱动力,因此是严格的放牧习惯。在2006年至2008年期间,从18个凹陷处采集了六个土壤样品,这些样品在干旱时期进行了分析(n = 104),包括pH,有机物(OM)含量,碳酸钙含量(CaCO3),砂/粉砂/粘土含量(INORG) ,总氮(TN)和总磷(TP)。整理每个土壤采样点的洪水持续时间,洪水频率,放牧方式和植被类型等数据。使用多变量和单变量统计分析来检验土壤性质,放牧状况和洪水变量之间的关系。 CaCO3,FD和以莎草为主的群落之间存在正相关,而INORG与放牧和草地具有正相关。 TN,TP,OM和土壤深度而不是FD之间存在很强的正相关性,并且发现OM是TN的有效预测因子。临时岩溶湿地的扩展FDs可能会增加土壤中碳酸钙积累的程度和程度,从而降低土地的放牧潜力。

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