Chin J Plant Ecol ›› 2008, Vol. 32 ›› Issue (6): 1285-1293.DOI: 10.3773/j.issn.1005-264x.2008.06.009
• Original article • Previous Articles Next Articles
CHEN Guang-Shui, YANG Yu-Sheng(), GAO Ren, XIE Jin-Sheng, YANG Zhi-Jie, MAO Yan-Ling
Received:
2008-07-11
Accepted:
2008-09-05
Online:
2008-07-11
Published:
2008-11-30
Contact:
YANG Yu-Sheng
CHEN Guang-Shui, YANG Yu-Sheng, GAO Ren, XIE Jin-Sheng, YANG Zhi-Jie, MAO Yan-Ling. CHANGES IN BELOWGROUND CARBON ALLOCATION IN A CHINESE FIR CHRONOSEQUENCE IN FUJIAN PROVINCE, CHINA[J]. Chin J Plant Ecol, 2008, 32(6): 1285-1293.
林龄 Stand age (a) | 龄组 Age class | 平均胸径 Mean DBH (cm) | 平均树高 Mean tree height (m) | 坡度 Slope | 坡向 Aspect | 密度 Stem density (株·hm-2) |
---|---|---|---|---|---|---|
7 | 幼龄 Young | 8.0 | 6.0 | 15° | NW20° | 4 892 |
16 | 中龄 Middle-age | 11.0 | 11.8 | 34° | NW25° | 3 875 |
21 | 近熟 Pre-mature | 14.7 | 13.0 | 32° | NW28° | 2 800 |
41 | 成熟 Mature | 24.3 | 25.2 | 40° | SW10° | 1 317 |
88 | 老龄 Old-growth | 32.8 | 32.2 | 30° | SW80° | 750 |
Table 1 Site characteristics in a Chinese fir chronosequence
林龄 Stand age (a) | 龄组 Age class | 平均胸径 Mean DBH (cm) | 平均树高 Mean tree height (m) | 坡度 Slope | 坡向 Aspect | 密度 Stem density (株·hm-2) |
---|---|---|---|---|---|---|
7 | 幼龄 Young | 8.0 | 6.0 | 15° | NW20° | 4 892 |
16 | 中龄 Middle-age | 11.0 | 11.8 | 34° | NW25° | 3 875 |
21 | 近熟 Pre-mature | 14.7 | 13.0 | 32° | NW28° | 2 800 |
41 | 成熟 Mature | 24.3 | 25.2 | 40° | SW10° | 1 317 |
88 | 老龄 Old-growth | 32.8 | 32.2 | 30° | SW80° | 750 |
林龄 Stand age (a) | 细根生物量 Fine root biomass (103 kg C·hm-2) | 细根净生产力 Fine root production (103 kg C·hm-2·a-1) | 细根周转速率 Fine root turnover rate (a-1) | ||||||
---|---|---|---|---|---|---|---|---|---|
0~1mm | 1~2mm | 总和total | 0~1mm | 1~2mm | 总和total | 0~1mm | 1~2mm | 总和total | |
7 | 0.879a | 0.379a | 1.258bc | 1.706a | 0.345ab | 2.051a | 1.94ab | 0.92a | 1.63a |
(0.115) | (0.047) | (0.105) | (0.248) | (0.058) | (0.195) | (0.04) | (0.19) | (0.07) | |
16 | 0.964a | 0.636b | 1.599a | 1.691a | 0.560c | 2.251a | 1.75ab | 0.89a | 1.41a |
(0.104) | (0.099) | (0.138) | (0.305) | (0.066) | (0.248) | (0.16) | (0.15) | (0.17) | |
21 | 0.864a | 0.530b | 1.394b | 1.876a | 0.432a | 2.308a | 2.17a | 0.82a | 1.65a |
(0.102) | (0.042) | (0.060) | (0.246) | (0.070) | (0.298) | (0.04) | (0.19) | (0.14) | |
40 | 0.674c | 0.420a | 1.094c | 1.072b | 0.316b | 1.388b | 1.63b | 0.76a | 1.28b |
(0.113) | (0.049) | (0.093) | (0.156) | (0.034) | (0.170) | (0.42) | (0.08) | (0.26) | |
88 | 0.379b | 0.224c | 0.603d | 0.593c | 0.138d | 0.731c | 1.61b | 0.64a | 1.22b |
(0.061) | (0.037) | (0.034) | (0.074) | (0.018) | (0.056) | (0.40) | (0.20) | (0.14) |
Table 2 Fine root biomass, production and turnover rate in a Chinese fir chronosequence
林龄 Stand age (a) | 细根生物量 Fine root biomass (103 kg C·hm-2) | 细根净生产力 Fine root production (103 kg C·hm-2·a-1) | 细根周转速率 Fine root turnover rate (a-1) | ||||||
---|---|---|---|---|---|---|---|---|---|
0~1mm | 1~2mm | 总和total | 0~1mm | 1~2mm | 总和total | 0~1mm | 1~2mm | 总和total | |
7 | 0.879a | 0.379a | 1.258bc | 1.706a | 0.345ab | 2.051a | 1.94ab | 0.92a | 1.63a |
(0.115) | (0.047) | (0.105) | (0.248) | (0.058) | (0.195) | (0.04) | (0.19) | (0.07) | |
16 | 0.964a | 0.636b | 1.599a | 1.691a | 0.560c | 2.251a | 1.75ab | 0.89a | 1.41a |
(0.104) | (0.099) | (0.138) | (0.305) | (0.066) | (0.248) | (0.16) | (0.15) | (0.17) | |
21 | 0.864a | 0.530b | 1.394b | 1.876a | 0.432a | 2.308a | 2.17a | 0.82a | 1.65a |
(0.102) | (0.042) | (0.060) | (0.246) | (0.070) | (0.298) | (0.04) | (0.19) | (0.14) | |
40 | 0.674c | 0.420a | 1.094c | 1.072b | 0.316b | 1.388b | 1.63b | 0.76a | 1.28b |
(0.113) | (0.049) | (0.093) | (0.156) | (0.034) | (0.170) | (0.42) | (0.08) | (0.26) | |
88 | 0.379b | 0.224c | 0.603d | 0.593c | 0.138d | 0.731c | 1.61b | 0.64a | 1.22b |
(0.061) | (0.037) | (0.034) | (0.074) | (0.018) | (0.056) | (0.40) | (0.20) | (0.14) |
Fig. 6 Linear regression of total belowground carbon allocation (TBCA) against aboreground net primarl productivity (ANPP) in a Chinese fir chronosequence
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