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资料表明:豫东平原地下软水、极软水分布是具有一定地质条件的,而且无论在水平方向与垂直方向上的变化,都是有規律性的。就其成因,目前看来是与温度、岩性、构造、所处地理部位等有一定关系的。软水、极软水是国家某种工业用水的宝贵资源,但目前由于发现不普遍,成因不清、储量不明仍然处于盲目开采阶段,水文地质工作者应当共同商讨、完善其成因,提出合理开发使用意见,以利于祖国四化建设,特将本文与读者商榷。
The data show that the underground soft water and extremely soft water distribution in the eastern Henan plain have certain geological conditions, and are regular in terms of both horizontal and vertical changes. Its cause, at present, appears to be related to temperature, lithology, structure, geographical location and so on. Soft water and soft water are the precious resources for some industrial water in our country. However, due to the fact that the discovery is not universal, the cause is unclear and the reserves are still unknown, the hydrogeology workers should discuss together to improve their causes and put forward suggestions for the rational exploitation of the water , In order to facilitate the building of the motherland’s four modernizations, especially with the readers of this article to discuss.