月亮峰附近，隆起的泥炭和黑色水潭、酸性水形成有图案的泥炭地。
Ridges of peat and pools of dark, acidic water form a patterned peatland near Moon Point.
报告结果提升了泥炭的关注度，这与本周在《自然地球科学》上发表的一片关于森林砍伐的文章形成了对比。
The report's findings, raising the profile of peat, contrast with the conclusions of a paper on deforestation published this week in Nature Geoscience.
研究人员通过观测被称为泥炭丘的小丘来测量永冻带边界北退的程度，泥炭丘是在北部泥炭沼泽含冰的土壤上自然形成的。
The researchers measured the retreat of the permafrost border byobserving hummocks known as "palsas, " which form naturally over icecontained in the soil of northern peat bogs.
只有当沼泽盆地慢慢下陷时，厚厚的泥炭堆积才能形成。
Thick accumulations of peat can form only if the swamp basin slowly subsides.
一种极少排水的环境，其中草地沼泽维系着初等草本植物的生长，但不形成泥炭。
An environment from which water rarely drains that supports primarily grassy vegetation and does not form peat.
泥炭是煤形成的第一阶段，是一种低质煤。
Peat, the first stage in the formation of coal, is a low-rank material.
泥炭是煤炭形成的第一阶段。
此外，正是由于成煤时放射元素参与，加速了泥炭化成煤进程，对形成块煤起了重要作用。
Moreover, precisely because of radioactive elements into the coal in the participation accelerated the process of peat into coal, to play an important role in the formation of lump coal.
高位泥炭沼泽形成的煤可选性好，而低位泥炭沼泽形成的煤可选性差。
The washability of coal deposited in high peat bogs is better than that deposited in low peat moors.
泥炭沼泽的形成可分为水域泥炭沼泽化和陆地泥炭沼泽化两大类。
The formation of peat swamps can be divided into two major categories, i. e. waterlogged peatification and terrestrial.
海侵导致了陆表海盆地沼泽环境的形成，进而形成泥炭沼泽，而随后的海侵事件导致了先形成的泥炭迅速处于深水环境最终成煤。
Marine transgression resulted in the forming of swamp and then the peat swamp. And the transgression later on put the peat formed in advance in deep water environment to form coal in the end.
镜质组和惰质组分别作为镜煤和丝炭的主要物源，形成于截然不同的泥炭沼泽环境，致使结构和性质差异大。
Vitrinite and inertinite were formed distinct peat swamp environment as main origin of vitrain and fusain, which was essential reason for liquefaction properties.
这一特点与该区广泛发育的泥炭丘地的形成密切相关，而不代表区域性云杉森林—苔原植被面貌在过去的1230年中曾有明显的改变。
The regional spruce forest-tundra vegetation of the creek has had little change since the eruption of White River ash at 1230 yr B. P.
这一特点与该区广泛发育的泥炭丘地的形成密切相关，而不代表区域性云杉森林—苔原植被面貌在过去的1230年中曾有明显的改变。
The regional spruce forest-tundra vegetation of the creek has had little change since the eruption of White River ash at 1230 yr B. P.
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