中文摘要：

水资源短缺已成为阻碍我国社会可持续发展的至关因素，而其中地下水资源短缺更甚。自1952年我国于干旱半干旱地区实施大规模人工造林以来，大量研究资料显示人工林的蒸散量要普遍高于当地自然植被的蒸散量，这可能会打破当地的地下水平衡。而以往我国有关人工造林对地下水位影响的研究较欠缺，因此在基于两种假设条件下。运用7种蒸散发模型测算了人工造林活动对北方干旱半干旱地区的地下水位影响。结果表明大规模的人工造林活动会降低地下水位高度．基于假设条件一，甘肃、宁夏和新疆地下水位下降严重；基于假设条件二，北京地下水位下降明显。提出我国在未来生态修复实践中要考虑对地下水供给的影响，确定合理造林规模并选择栽培乡土树种．真正提高地下水资源利用率。

英文摘要：

Water scarcity is a global environmental problem that jeopardizes human safety and socioeconomic development. In China, it has also become a potentially major obstacle for socioeconomic development, where 164 major groundwater areas are being exploited unsustainably. As a result, the depth of the groundwater table has increased by an average of 1.5 m per year in the arid and semi-arid regions of the north. Since 1952, China has implemented an unprecedented large-scale tree-planting program that focused on arid and semi-arid regions. The goal was to use trees to conserve water and combat desertification. Unfortunately, there is a serious risk that this program could exacerbate water shortages and lower the groundwater table because the trees were not chosen based on local environmental constraints, and their evapotranspiration is greater than the regional precipitation. Since precipitation is the major source of groundwater recharge in these semi-arid and arid areas of northern China, this imbalance will intensify the decline of the groundwater resource. Despite this risk,there has been limited research on the effect of afforestation on the groundwater table in China. In the present study, we selected nine provinces and provincial-level regions （ Beijing, Hebei, Henan, Shanxi, Shaanxi, Ningxia, Inner Mongolia, Gansu, and Xinjiang） in China that focused on the tree-planting program, and are environmentally fragile arid or semi-arid regions facing a serious water scarcity. We calculated the influence of the afforestation program on groundwater based on two assumptions using seven evapotranspiration models, without considering evapotranspiration of the underlying vegetation or accounting for differences among the tree species used in afforestation. We confirmed that there is a serious risk that afforestation will cause the groundwater table to decline, independent of any other human withdrawals of this water. Based on our assumptions that afforestation plots had insignificant groundwater recharge or losses as a r