我国泥炭资源丰富,储量占世界第12位,相对集中分布于西南若尔盖高原、云贵高原、东部长江中下游平原、东北兴安岭、长白山和三江平原等地区。我国高腐植酸泥炭亦分布于上述区内。 我国泥炭资源一般是有机质含量不高,中强分解度,纤维含量少、发热量低、偏酸性,并富氮而贫磷、钾,这就决定了其基本利用方 China is rich in peat resources and reserves account for the 12th largest in the world. It is relatively concentrated in areas such as the Zoige Plateau in the southwest, the Yunnan-Guizhou Plateau, the plain in the middle and lower reaches of the Yangtze River in the east, the Xing’an Mountains in Northeast China, the Changbai Mountain and the Sanjiang Plain. China’s high humic acid peat also distributed in the above area. Peat resources in China are generally low organic matter content, strong decomposition, fiber content, low calorific value, acidic, and rich in nitrogen and phosphorus, potassium, which determines the basic use of party