摘要
通过对青岛即墨东北部大官庄乡这一剥蚀残丘垅岗区进行地下水资源探测，发现了延伸规模较大的东西向张性断裂破碎带，并在大旱之年的枯水季节（１９９７年１２月）于有利部位打出日产４００ｍ３的富水井，确认该断裂带富水。由此，为在青岛地区寻找基岩裂隙水开辟了新的断裂构造领域。
The pollution character and immigration mechanism of phenol and cyanogen are discussed through field surveys of the environmental hydrogeology, pollution sources, the current and historical pollution of phenol and cyanogen in groundwater. It is shown that the areas along the river banks and the sand/gravel areas along the waste water discharging ditch form the main channels for the pollutants entering the aquifers. Precipitation is the main influencing factor of the absorbed phenol/cyanogen immigration from the vadose zone to groundwater. Although no waste water with phenol and cyanogen discharge to the investigating area currently, the two kinds of pollutants still exist in the vadose zone for a long time and will enter ground water under the influence of rainfall. However, their concentrations tend to reduce.
关键词
青岛地区
垅岗
基岩
富水区
地下水
水资源探测
Phenol and Cyanogen pollution
immigration
groundwater
vadose zone
environmental hydrogeology
