| Change log entry 79570 | |
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| Processed by: | richwarm (2023-09-19 23:50:27 GMT) |
| Comment: |
<< review queue entry 72367 >> 淤泥（Silt），又称沉泥或粉土，是泥土的基本组成成分之一。地质学中，淤泥是介于沙土及黏土之间，长约2到62微米、直径4到9微米的一种颗粒状物料（英语：granular material），主要由石英及长石这两种矿物组成[1]。 https://zh.m.wikipedia.org/wiki/%E6%B7%A4%E6%B3%A5 本书所考虑的组成部分包括漂砾，砾石，砂，粉土和粘土。 The components to be considered in this book include boulders, gravel, sand, silt and clay. 我国的海城和唐山相继发生地震后，粉土的液化问题也逐渐引起研究者的关注。 After Haicheng and Tangshan Earthquake in China, the liquefaction of silty soil has caused researcher's attention too. |
| Diff: |
- 粉土 粉土 [fen3 tu3] /dust/sand/ + 粉土 粉土 [fen3 tu3] /silt; silty soil/ |