Sphagnum mire occupy extensive tracts of land throughout the Boreal and Subarctic regions.
泥炭藓沼泽多分布于北半球的温带到负极带地区,在我国,泥炭藓沼泽主要发育在大、小兴安岭和长白山等地。
Plant Diversity of Subalpine Sphagnum Mires in Western Hubei Province;
鄂西亚高山泥炭藓沼泽湿地的植物多样性
ON THE PURIFICATION EFFECTS OF THE SPHAGNUM WETLAND ON Cd(Ⅱ),Cu(Ⅱ),Pb(Ⅱ),Zn(Ⅱ) IN DAJIUHU BASIN OF SHENNONGJIA MOUNTAINS
神农架大九湖泥炭藓沼泽湿地对镉(Ⅱ)、铜(Ⅱ)、铅(Ⅱ)、锌(Ⅱ)的净化模拟
The Sphagnum Bog Plant Resources in Tianbaoyan Nature Reserve in Fujian
福建天宝岩自然保护区泥炭藓沼泽植物资源调查
Records of Surface Wetness from Hani Mire in Changbai Mountains
哈泥泥炭藓泥炭记录的沼泽地表湿度变化
A swamp or bog formed by an accumulation of sphagnum moss, leaves, and decayed matter resembling peat.
厚苔沼类似泥炭地的沼泽地，由水藓、叶子和腐烂物质的堆积物形成
A cutting in a peat bog.
泥炭沼泽地中的草地块
a large genus constituting the order Sphagnales: atypical mosses of temperate bogs with leaves that can hold much water.
泥炭藓目的一属；一种非典型的温带沼泽苔藓，其叶子可以保留很多水份。
bogwood:Wood that has been preserved in a peat bog.
泥炭木,沼木:久埋于泥炭沼泽之中的树木。
Wood that has been preserved in a peat bog.
泥炭木，沼木久埋于泥炭沼泽之中的树木
Any of certain other wetland areas, such as a fen, having a peat substrate.
沼泽地区任一种其它的湿地，有泥炭底面，如沼泽
A Study on the Transmission and Distribution of Rainfall in Hani-peat Mire
降水在哈泥泥炭沼泽中的传输与分配作用研究
An area having a wet, spongy, acidic substrate composed chiefly of sphagnum moss and peat in which characteristic shrubs and herbs and sometimes trees usually grow.
沼泽，湿地底面为酸性和湿软的地带，主要由灌木、草类及一些树的水藓泥沼和泥煤构成
FORMATION MECHANISM AND TIME-SPACE DISTRIBUTION OF COASTAL PEAT MOOR OF THE BOHAI BAY
渤海湾沿岸泥炭沼泽形成机制与时空分布
Study on the Distribution, Transformation and Environmental Effects of Nitrogen in Peat Mire;
泥炭沼泽氮素分布、转化及其环境效应研究
Study on Soil Water Physical Features of Typical Peat Swamps in Xiaoxing'anling Mountain
小兴安岭典型泥炭沼泽土壤水分物理性质研究
Soil water drainage and excessive grazing in pastureland of m ire and peat soils are accountable for the deterioration and quality decline of mire and peat soils.
人类疏干沼泽、过度放牧等活动是沼泽土和泥炭土退化、质量下降的主要原因。
synsedimentary fallout ash alteration in the nearshore peat swamp and march environment.
它们是在近岸泥炭沼泽或沼泽环境中由同期降落的火山灰蚀变而成。
Thick accumulations of peat can form only if the swamp basin slowly subsides.
只有当沼泽盆地慢慢下陷时，厚厚的泥炭堆积才能形成。