Chin J Plant Ecol ›› 2005, Vol. 29 ›› Issue (2): 296-303.DOI: 10.17521/cjpe.2005.0038
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YANG Jing-Cheng1,2(), HUANG Jian-Hui1, TANG Jian-Wei3, PAN Qing-Min1, HAN Xing-Guo*()
Received:
2003-11-21
Accepted:
2004-07-21
Online:
2005-11-21
Published:
2005-03-10
Contact:
HAN Xing-Guo
About author:
*E-mail:xghan@ns.ibcas.ac.cnSupported by:
YANG Jing-Cheng, HUANG Jian-Hui, TANG Jian-Wei, PAN Qing-Min, HAN Xing-Guo. CARBON SEQUESTRATION IN RUBBER TREE PLANTATIONS ESTABLISHED ON FORMER ARABLE LANDS IN XISHUANGBANNA, SW CHINA[J]. Chin J Plant Ecol, 2005, 29(2): 296-303.
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Site | Age (a) | Location | Altitude (m) | Aspect | Slope | Soil type | Biomass (103 kg·hm-2) | Soil C stocks (×103 kg C·hm-2) (cm) | ||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Biomass_1 | Biomass_2 | 0-20 | 0-40 | 0-100 | ||||||||
Guanlei | 3 | 21°42′N, 101°15′E | 895 | Northeast | 5° | Latosols | 6.8 | 3.1 | 43.8 | 73.7 | 133.4 | |
Menglun | 3 | 21°55′N, 101°15′E | 750 | South | 5° | Latosols | 7.4 | 3.6 | 46.8 | 86.2 | 179.0 | |
Daka | 4 | 21°53′N, 101°14′E | 750 | Southeast | 15° | Latosols | 9.6 | 5.8 | 55.8 | 92.6 | 147.7 | |
Jinghong | 6 | 21°43′N, 100°44′E | 530 | South | 5° | Latosols | 24.5 | 16.1 | 45.5 | 91.5 | 176.9 | |
Guanlei | 7 | 21°42′N, 101°15′E | 870 | Northeast | 10° | Latosols | 34.2 | 24.5 | 42.3 | 84.2 | 154.9 | |
Menglun | 11 | 21°54′N, 101°16′E | 600 | East | 5° | Latosols | 63.8 | 48.8 | 46.1 | 84.9 | 170.8 | |
Chengzi | 16 | 21°55′N, 101°14′E | 580 | East | 20° | Latosols | 124.8 | 95.0 | 34.4 | 63.4 | 126.4 | |
Menglun | 16 | 21°53′N, 101°19′E | 650 | West | 10° | Latosols | 140.5 | 106.1 | 37.2 | 62.1 | 112.5 | |
Mengla | 21 | 21°33′N, 101°34′E | 710 | Northeast | 15° | Latosols | 222.6 | 165.1 | 51.8 | 96.9 | 202.5 | |
Mengxing | 28 | 21°55′N, 101°17′E | 550 | West | 15° | Latosols | 267.3 | 232.2 | 35.2 | 60.0 | 111.4 | |
Jinghong | 38 | 21°51′N, 100°22′E | 800 | Southeast | 10° | Latosols | 340.0 | 326.5 | 37.9 | 73.5 | 142.5 |
Table 1 Site characteristics of eleven rubber tree plantations with different ages (from 3 to 38 years) in Xishuangbanna, Southwest China
Site | Age (a) | Location | Altitude (m) | Aspect | Slope | Soil type | Biomass (103 kg·hm-2) | Soil C stocks (×103 kg C·hm-2) (cm) | ||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
Biomass_1 | Biomass_2 | 0-20 | 0-40 | 0-100 | ||||||||
Guanlei | 3 | 21°42′N, 101°15′E | 895 | Northeast | 5° | Latosols | 6.8 | 3.1 | 43.8 | 73.7 | 133.4 | |
Menglun | 3 | 21°55′N, 101°15′E | 750 | South | 5° | Latosols | 7.4 | 3.6 | 46.8 | 86.2 | 179.0 | |
Daka | 4 | 21°53′N, 101°14′E | 750 | Southeast | 15° | Latosols | 9.6 | 5.8 | 55.8 | 92.6 | 147.7 | |
Jinghong | 6 | 21°43′N, 100°44′E | 530 | South | 5° | Latosols | 24.5 | 16.1 | 45.5 | 91.5 | 176.9 | |
Guanlei | 7 | 21°42′N, 101°15′E | 870 | Northeast | 10° | Latosols | 34.2 | 24.5 | 42.3 | 84.2 | 154.9 | |
Menglun | 11 | 21°54′N, 101°16′E | 600 | East | 5° | Latosols | 63.8 | 48.8 | 46.1 | 84.9 | 170.8 | |
Chengzi | 16 | 21°55′N, 101°14′E | 580 | East | 20° | Latosols | 124.8 | 95.0 | 34.4 | 63.4 | 126.4 | |
Menglun | 16 | 21°53′N, 101°19′E | 650 | West | 10° | Latosols | 140.5 | 106.1 | 37.2 | 62.1 | 112.5 | |
Mengla | 21 | 21°33′N, 101°34′E | 710 | Northeast | 15° | Latosols | 222.6 | 165.1 | 51.8 | 96.9 | 202.5 | |
Mengxing | 28 | 21°55′N, 101°17′E | 550 | West | 15° | Latosols | 267.3 | 232.2 | 35.2 | 60.0 | 111.4 | |
Jinghong | 38 | 21°51′N, 100°22′E | 800 | Southeast | 10° | Latosols | 340.0 | 326.5 | 37.9 | 73.5 | 142.5 |
Fig.1 Relationship of biomass and age of rubber tree plantations in Xishuangbanna, Southwest China The lines denoted regression by sigmoidal curve. Biomass data in curve a, and b were calculated according to allometric biomass growth equations of Tang et al.(2003) and Brown (1997)
Fig.2 Linear relationship between biomass and age of rubber tree plantations in Xishuangbanna, Southwest China Biomass data in a and b were calculated according to allometric biomass growth equations of Tang et al.(2003) and Brown (1997)
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