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首页> 外文期刊>Arabian journal of geosciences >Impact of spate irrigation of flood waters on agricultural drought and groundwater recharge: case of Sidi Bouzid plain, Central Tunisia
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Impact of spate irrigation of flood waters on agricultural drought and groundwater recharge: case of Sidi Bouzid plain, Central Tunisia

机译:洪水的大量灌溉对农业干旱和地下水补给的影响:以突尼斯中部西迪·布兹德平原为例

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In Sidi Bouzid plain, rainfall alone is insufficient to satisfy crop water requirements. Within this framework, and in order to improve water resources in the region, the Tunisian State adopted non-conventional water mobilization techniques, among which artificial spate irrigation. The objective of the study is to evaluate the impact of spate irrigation of flood water on the mitigation of agricultural drought and the enhancement of groundwater recharge. Annual and monthly rainfall data as well as flood water volumes were monitored. The study focused on the groundwater drawdown monitoring. Results showed a high flood water contribution to crop water requirements that exceeded rainfall. This water prevented drought in the spate perimeters. The groundwater drawdown was found to fluctuate over time, with an average decreasing rate of 0.4 to 0.5 m/year. Groundwater recharge was found to be highly correlated with flood water contribution through spate irrigation (R-2 = 84 %). Out of the spate zone, a high decrease in the groundwater level was noted. The lowest rate of 1 m/year was that of the farthest piezometer from the spate perimeters. This is influenced by the excessive pumping out of the spate zone. In 1980, groundwater flew from the west to the east. In 2015, the flow movement from the east to the center of the plain did not change due to the presence of the spate perimeters. Nevertheless, excessive pumping around sabkhas changed the flow directions at the outlet zone. A variation in groundwater salinity was observed in both space and time. In 1975, salinity was very low. The outlet zone was the most affected where the drawdown reached several meters, causing saltwater intrusion from the surrounding sabkhas.
机译:在西迪布兹德平原,仅降雨不足以满足作物需水量。在此框架内,为了改善该地区的水资源,突尼斯国家采用了非常规的水动员技术,其中包括人工灌溉。该研究的目的是评估洪水的大量灌溉对缓解农业干旱和提高地下水补给的影响。监测年和月降雨量数据以及洪水量。该研究的重点是地下水渗漏监测。结果表明,洪水对农作物需水的贡献超过降雨。这种水防止了后备区域的干旱。发现地下水的流失量随时间波动,平均下降速度为0.4至0.5 m /年。发现地下水补给与通过大量灌溉的洪水贡献高度相关(R-2 = 84%)。在交汇区之外,注意到地下水位高度下降。最低的1 m /年的速率是离接壤周长最远的测压仪。这受过多的泵送出接续区的影响。 1980年,地下水从西向东飞散。在2015年,由于有波状周长的存在,从东部到平原中心的水流运动没有改变。尽管如此,在萨布哈斯周围过度抽水改变了出口区域的流向。在时间和空间上都观察到了地下水盐度的变化。 1975年,盐度很低。出口区受到最大影响,水位下降到几米,导致盐水从周围的萨布哈斯河入侵。

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