scholarly journals CALORIC VALUES AND ENERGY ALLOCATION OF A TROPICAL SEASONAL RAIN FOREST AND A MONTANE EVERGREEN BROAD-LEAVED FOREST IN SOUTHWEST CHINA

2007 ◽  
Vol 31 (6) ◽  
pp. 1103-1110 ◽  
Author(s):  
LIN Hua ◽  
◽  
CAO Min* ◽  
ZHANG Jian-Hou
2005 ◽  
Vol 167 (1-4) ◽  
pp. 295-309 ◽  
Author(s):  
Wen Jie Liu ◽  
Yi Ping Zhang ◽  
Hong Mei Li ◽  
Fan Rui Meng ◽  
Yu Hong Liu ◽  
...  

2004 ◽  
Vol 28 (2) ◽  
pp. 264-270
Author(s):  
LIU Wen-Jie ◽  
ZHANG Yi-Ping ◽  
LI Hong-Mei ◽  
DUAN Wen-Ping

2008 ◽  
Vol 20 (2) ◽  
pp. 207-215 ◽  
Author(s):  
Yuping YAN ◽  
Liqing SHA ◽  
Min CAO ◽  
Zheng ZHENG ◽  
Jianwei TANG ◽  
...  

2014 ◽  
Vol 1073-1076 ◽  
pp. 222-228
Author(s):  
Ming Qian Yu ◽  
Guang Tao Meng ◽  
Li Ping He ◽  
Ning Yun Li ◽  
Gui Xiang Li ◽  
...  

Sequential soil coring and in situ exposure of largely undisturbed soil columns technique was used to study the nitrogen mineralization of five forest types soils in the east side of Gaoligongshan mountains, which were Dry-Hot Vally (D), Montane Rain Forest (MR), Monsoon Evergreen Broad-leaved Forest (M), the Mid-Montane Humid Evergreen Broad-leaved Forest (H), Tsuga Forest (Ts). The results indicated that NH4+-N content decreased for all the forest types soil after four months training, the order of decrease proportion is monsoon evergreen broad-leaved forest (84.1%)> montane rain forest (69.3%)> the mid-montane humid evergreen broad-leaved forest (34.7%)> dry-hot vally (8.7%)> tsuga forest (7.3%). And NO3--N content increased for the soils, the increasing multiples is tsuga forest (39.0 times)> dry-hot vally (18.8 times)> the mid-montane humid evergreen broad-leaved forest (4.7 times)> monsoon evergreen broadleaf forest (4.0 times) > montane rainforest (2.8 times). We conclude that NH4+-N is the main form of inorganic nitrogen in forest soil, which is the main reason of changing the soil nitrogen mineralization and mineralization rate.


Sign in / Sign up

Export Citation Format

Share Document