长芦盐场
形成原因
长芦盐场地处渤海湾西岸,地势平坦、海滩宽广,并且长芦盐场所在地雨季短春季气温回升快,风多雨少,日照充足,蒸发旺盛,有利于海水蒸发。[1]
参考文献
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.