1) Mat-Cryic Cambisols
寒冻雏形土
1.
The climate change difference of Mat-Cryic Cambisols and area in south and north Qinghai is significant because of different elevation and geological environment.
青海南北二地寒冻雏形土分布区,由于海拔高度及地理环境不同,气候变化差异显著。
2) Mat-Cryic Cambisols
草毡寒冻雏形土
1.
A Study on Replenishment and Decomposition of Organic Matter in and Mat-Cryic Cambisols CO_2 Flux Between Vegetation and Atmosphere;
草毡寒冻雏形土有机质补给、分解及大气CO_2通量交换
2.
Earth temperature was studied respectively, in Fib-Orthic Histosols area and Mat-Cryic Cambisols soil area at the same elevation and near in distance.
在海拔高度相同、距离相近的纤维正常有机土与草毡寒冻雏形土地区，虽然区域气候一致，但二者地温具有显著的分布差异。
3) Mollic Gryic cambisols
暗沃寒冻雏形土
4) Mat Cryo-sod soil
草毡寒冻雏形土
1.
Analysis of three different methods of estimating CO 2 emission was carried out by comparing the data obtained from filed determination of soil CO 2 emission from Mat Cryo-sod soil in 1998～1999.
应用 1 998年 5月～ 1 999年 4月草毡寒冻雏形土土壤CO2 释放通量的实测资料 ,通过对常用的三种土壤CO2 释放量估测方法的比较分析 ,提出了适合草毡寒冻雏形土土壤CO2 日及年释放量的估测方法。
5) frigid
寒冻
6) frozen soil
寒冻土壤
参考词条
补充资料：冻寒
1.挨冻受寒。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。