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Antropogenic input of nitrogen and riverine export from a Mediterranean catchment. The Celone, a temporary river case study

机译:从地中海集水区输出氮和河流的人为输入。 Celone,临时河流案例研究

摘要

In a catchmnent, nitrogen (N) export from terrestrial ecosystems to rivers is controlled by the hydrological processes and N balance. In the present paper, the soil system N budget and riverine export were quantified in a Mediterranean watershed, the Celone (South-East, Italy). The study area (72 km2) consists of agricultural land (70%) and deciduous forests with three small residential areas. Major N inputs derived from fertilizers and animal manure, corresponding for the whole watershed area to 68 and 12 kg N ha−1 yr−1, respectively. N input from point sources was 1% of total input and atmospheric depositions measured in a gauging station near the study area was quantified in ∼6 kg N ha−1 yr−1. Crop N uptake was the main N output from agricultural land; it was estimated in ∼37 kg N ha−1 yr−1 by using data on crop yields provided by local farmers. Total flux of N in surface water was quantified for a year at the outlet of the study area by using continuous measures of flow and discrete measures of N concentrations carried out with a different frequency during the normal and low flow and when floods occurred. The hydrological regime of the stream, which is a temporary river, plays an important role in N transport. Water quality was found to vary considerably through the year in terms of both nutrient concentrations and loads. Riverine N export was quantified in 41% of total N input, and it was mainly transported during flood events, ∼60% of the annual load was delivered during floods occurred in 38 days. Organic nitrogen and nitrate were the main N forms in surface water, and the contribution per hectare was about 24 and 14 kg N, respectively. On a yearly basis, the difference between N inputs and outputs including riverine export was estimated in about 4 kg N ha−1 yr−1 for the whole watershed area. This amount partly accumulates in soils in different N forms and the remaining part, mainly in form of nitrate, percolates through unsaturated soil towards groundwater. This study reports an important analysis of N pollution in a Mediterranean watershed with a temporary river system and limited data availability. Data acquisition and handling have proved to be an important challenge to overcome in N balance quantification. The results and the methodology of the present work can be useful for understanding nitrogen loss dynamics and for functional water management and land use planning.
机译:在一个广域,从陆地生态系统向河流的氮(N)出口受水文过程和氮平衡的控制。在本文中,定量分析了地中海分水岭Celone(意大利东南部)的土壤系统N预算和河流出口。研究区域(72平方公里)由农田(70%)和落叶林组成,并有三个小居民区。氮的主要来源来自化肥和动物粪便,分别对应于整个流域面积分别为68和12 kg N ha-1 yr-1。来自点源的N输入量占总输入量的1%,在研究区域附近的测量站中测得的大气沉积量约为6 kg N ha-1 yr-1。作物吸收氮是农业用地的主要氮素输出。通过使用当地农民提供的农作物产量数据,估计约为37 kg N ha-1 yr-1。在研究区域的出口处,通过使用连续的流量测量和离散的N浓度测量(在正常流量和低流量期间以及洪水发生时以不同的频率进行测量),对地表水中N的总通量进行了一年的量化。溪流的水文状况是一条临时河,在氮的运输中起着重要的作用。发现全年的水质在营养物浓度和负荷方面都有很大的不同。河流氮的出口量占总氮输入量的41%,主要是在洪水事件中运输,在38天的洪水期间约有60%的年负荷被输送。有机氮和硝酸盐是地表水中的主要N形态,每公顷贡献量分别约为24和14 kgN。每年,整个流域面积的N投入与产出之间的差异(包括河流出口)估计约为4 kg N ha-1 yr-1。该量部分以不同的N形式累积在土壤中,其余部分(主要为硝酸盐形式)通过非饱和土壤渗入地下水。这项研究报告了对具有临时河流系统和有限数据可用性的地中海流域氮污染的重要分析。事实证明,数据采集和处理是氮平衡定量分析中要克服的重要挑战。当前工作的结果和方法学对于理解氮素流失动态以及功能性水管理和土地利用规划可能是有用的。

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