檢視粘土矿物的原始碼

[[File:粘土矿物.jpg|缩略图|[https://image.baidu.com/search/detail?ct=503316480&z=0&ipn=d&word=%E7%B2%98%E5%9C%9F%E7%9F%BF%E7%89%A9%20%20%E6%90%9C%E7%8B%90&step_word=&hs=0&pn=2&spn=0&di=24970&pi=0&rn=1&tn=baiduimagedetail&is=0%2C0&istype=2&ie=utf-8&oe=utf-8&in=&cl=2&lm=-1&st=-1&cs=2633271808%2C2876788731&os=3388981085%2C2681827753&simid=4224136098%2C701846181&adpicid=0&lpn=0&ln=590&fr=&fmq=1623277739087_R&fm=result&ic=&s=undefined&hd=&latest=&copyright=&se=&sme=&tab=0&width=&height=&face=undefined&ist=&jit=&cg=&bdtype=0&oriquery=&objurl=https%3A%2F%2Fgimg2.baidu.com%2Fimage_search%2Fsrc%3Dhttp%3A%2F%2F5b0988e595225.cdn.sohucs.com%2Fq_70%2Cc_zoom%2Cw_640%2Fimages%2F20180524%2F3bca1c3012224f6db56489a9d7d78b92.jpeg%26refer%3Dhttp%3A%2F%2F5b0988e595225.cdn.sohucs.com%26app%3D2002%26size%3Df9999%2C10000%26q%3Da80%26n%3D0%26g%3D0n%26fmt%3Djpeg%3Fsec%3D1625869755%26t%3De88ef1e463dd3a9dd4b050d60c9bd81e&fromurl=ippr_z2C%24qAzdH3FAzdH3F4_z%26e3Bf5i7_z%26e3Bv54AzdH3FwAzdH3Fdnd08m9na_ddllc0&gsm=3&rpstart=0&rpnum=0&islist=&querylist=&nojc=undefined 原图链接][https://m.sohu.com/a/232716430_229957 来自手机搜狐网]]]
'''粘土矿物'''（clay minerals），地质学专业术语，是组成粘土岩和土壤的主要矿物。它们是一些含铝、镁等为主的含水硅酸盐矿物。除海泡石、坡缕石具链层状结构外，其余均具层状结构。颗粒极细，一般小于0.01毫米。加水后具有不同程度的可塑性。