marsh peat
- marsh peat的基本解释
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沼泽泥炭, 湿地泥炭
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The research of marsh initiated in the 1960s in our country. However, the study of marsh sedimentation and environmental changes was relatively weak, even though we have done some preliminary works on an approach to the characteristics of sporepollen assemblage of peat in the Holocene and paleoenvironmwent, and formation mechanism and deposition kinetics of peatland since 1990s. But we are lacking in systematic research on gleying marsh, especially on recent short timescale and highresolution sedimentation records of environmental changes. There is a certain disparity in this field compared with lake sedimentation and environmental changes.
我国沼泽研究起步于20 世纪60 年代,期间有关沼泽沉积与环境的研究相对薄弱,90 年代以来虽已在泥炭沼泽孢粉解译全新世环境变化与泥炭沉积动力学方面有初步积累,但对潜育沼泽缺乏系统研究,尤其缺乏近代短时间尺度高分辨率环境变化历史记录研究,这方面与湖泊沉积及其环境演变研究相比已形成一定的差距。
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In addition, there are constrained by the rock of the limestone soil and purple soil, and thick bone soil, paddy soil, brown soil, aquic soil, peat, marsh land, Carboniferous soil, rocky soil, mountain meadow soil, red clay, the new soil, such as soil type.
此外,还有受母岩制约的石灰土和紫色土、粗骨土、水稻土、棕壤、潮土、泥炭土、沼泽土、石炭土、石质土、山地草甸土、红粘土、新积土等土类。
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paludal:沼泽的
沼泽成煤学说 swamp theory | 沼泽的 paludal | 沼泽泥煤 marsh peat
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marshite:碘铜矿
marsh peat 湿地泥炭 | marshite 碘铜矿 | marshland 沼泽地