Abstract
In a 5-year field trial, we examined plant productivity and soil organic matter decomposition on plots with a mixture of Chinese fir (Cunninghamia lanceolata (Lamb.) Hook.) and broadleaved trees. We compared pure fir (PF) plots to two mixed plots (2:1 ratio of fir to broadleaved trees): MP1 (C. lanceolata and Liquidambar formosana Hance) and MP2 (C. lanceolata and Alnus cremastogyne Burk). The mixed plots differed in that the MP2 plots incorporated a nitrogen-fixing tree (A. cremastogyne). We hypothesized that the mixed plots would have higher soil organic matter decomposition rates than the PF plots as a result of increased primary productivity. The increased productivity would increase carbon input into soils, thus resulting in greater microbial biomass and soil basal respiration. We measured tree biomass, soil organic matter decomposition rates, microbial biomass carbon, total organic carbon, metabolic quotient and microbial quotient for each plot. The results showed that the productivity, microbial biomass carbon, and total carbon in the MP2 plots were significantly higher than in the PF and MP1 plots. Path analyses suggested that soil respiration varied with the amount of tree biomass produced. However contrary to our hypothesis, soil basal respiration was higher in the PF plots than in the MP2 plots.
Similar content being viewed by others
References
Bardgett RD, Shine A (1999) Linkages between plant litter diversity, soil microbial biomass and ecosystem function in temperate grasslands. Soil Biol Biochem 31:317–321
Binkley D, Sollins P (1990) Factors determining differences in soil pH in adjacent conifer and alder-conifer stands. Soil Sci Soc Am J 54:1427–1433
Brown D, Lugo AE (1982) The storage and production of organic matter in tropical forests and their role in the global carbon cycle. Biotropica 14:161–187
Dick RP (1992) A review: long-term effects of agricultural systems on soil biochemical and microbial parameters. Agr Ecosyst Environ 40:25–36
Feng ZW, Chen CY, Zhang JW et al (1988) A coniferous broad-leaved mixed forest with higher productivity and ecological harmony in subtropics-study on mixed forest of Cunninghamia lanceolata and Michelia macclurei. Acta Phytoecogica Et Geobotanica Sinica 12(3):165–180
Giardina CP, Huffinan S, Binkley D, Cauldwell BA (1995) Alders increase soil phosphorus availability in a Douglas-fir plantation. Can J For Res 25:1652–1657
Guo J (2008) Comparison of soil organic carbon and nitrogen pool between mixed and pure forests of Chinese fir. J Fujian For Sci Tech 35(2):5–9
Hu Y, Wang S, Zeng D (2006) Effects of single Chinese fir and mixed leaf litters on soil chemical, microbial properties and soil enzyme activities. Plant Soil 282:379–386
Huang Y, Feng Z, Wang S et al (2004) Effects of Chinese-fir mixing with N-fixing and non-N fixing tree species on forestland quality and forest-floor solution chemistry. [J] Acta Ecologica Sinia 24(10):2192–2199
Insam H, Domsch KH (1988) Relationship between soil organic carbon and microbial biomass on chronosequences of reclamation sites. Microb Ecol 15:177–188
Jia Y, Wang T, Du R (2005) Study on variety of the content of carbon and nitrogen in different type of soil. J Beijing Agri Col 20(3):63–66
Landi F, Valori J, Ascher J, Renella G, Falchini L, Nannipieri P (2006) Root exudates effects on the bacterial communities, CO2 evolution, nitrogen transformations and ATP content of rhizosphere and bulk soils. Soil Biol Biochem 38(3):509–516
Lei JF (2005) Forest resources of China. Chinese Forestry, Beijing, pp 172–173
Liao L, Yang Y, Wang S et al (1999) Distribution, decomposition and nutrient return of the fine root in pure Cunninghamia lanceolata, Michelia macclurei and the mixed plantation. [J] Acta Ecologica Sinia 19(3):342–346
Liu Y, Han S, Hu Y, Dai G (2005) Effects of soil temperature and humidity on soil respiration rate under pinus sylvestriformis forest. Chin J Appl Ecol 16(9):1581–1585
Lu RK (1999) Analysis methods of soil agricultural chemistry. China Agricultural Science and Technology, Beijing, pp 228–233
Montagnini F, Porras C (1998) Evaluating the role of plantations as carbon sinks: an example of an integrative approach from the humid tropics. Environ Manage 22(3):459–470
Mu S (2004) Respiration of soils under temperate deciduous, coniferous and mixed forest. Acta Pedologia Sin 41(4):564–570
Murphy M, Balser T, Buchmann N, Hahn V, Potvin C (2008) Linking tree biodiversity to belowground process in a young tropical plantation: impacts on soil CO2 flux. For Eco Manage 255:2577–2588
Piao HC, Zhu JM, Liu GS, Liu CQ, Tao FX (2006) Changes of natural 13C abundance in microbial biomass during litter decomposition. Appl Soil Ecol 33(1):3–9
Raich JW, Schlesinger WH (1992) The global carbon dioxide flux in soil respiration and its relation to vegetation and climates. Tellus 44B:81–99
Redondo-Brenes A, Montagnini F (2006) Growth, productivity, aboveground biomass, and carbon sequestration of pure and mixed native tree plantations in the Caribbean lowlands of Costa Rica. For Eco Manage 232:168–178
Van Miegroet H, Cole D, Binkley D, Sollins P (1989) The effect of nitrogen accumulation and nitrification on soil chemical properties in alder forests. In: Olson RK, LeFohn AS (eds) Effects of air pollution on western forests. Air Waste Manage. Assoc, Pittsburgh, pp 515–528
Vance ED, Brookes PC, Jenkinson DS (1987) An extraction method for measuring soil microbial biomass C. Soil Biol Biochem 19:703–707
Wang S, Liao L, Ma Y (1997) Nutrient return and productivity of mixed Cunninghamia lanceolata and Michelia Maoclurei plantations. Chin J Appl Ecol 8(4):347–352
Wang Q, Wang S, Fan B, Yu X (2007) Litter production, leaf litter decomposition and nutrient return in Cunninghamia lanceolata plantation in south China: effect of planting conifers with broadleaved species. Plant Soil 297:201–211
Wang Q, Wang S, Huang Y (2008a) Comparison of litterfall, litter decomposition and nutrient return in a monoculture Cunninghamia lanceolata and a mixed stand in southern China. For Ecol Manag 255:1210–1218
Wang W, Lei Y, Wang X et al (2008b) A review of forest biomass models. J Northwest For Univ 23(2):58–63
Xu GH, Zhen HY (1986) Manual on microbial analysis method of soil. Agriculture, Beijing
Xu M, Qi Y (2001) Soil surface CO2 efflux and its spatial and temporal variations in a young ponderosa pine plantation in northern California. Glob Chang Biol 7:667–677
Yan S, Wang S, Yu X (2004) Effect of mixtures with alders on soil fauna in plantation forest of Chinese fir. Chin J Appl Environ 10:462–466
Yang Q, Li M, Wang B (2004) Study on soil respiration of the lower subtropical successive forest communities. Guihaia 24(5):443–449
Zhang L, Wang B, Liu Y, Chen B, Ao J (2007) A study on the soil respiration under four forest types in dagangshan in summer and autumn. Acta Agri Univ Jiangxiensis 29(1):72–77
Zhang J, Wang S, Wang Q, Liu Y (2009) Content and seasonal change in soil labile organic carbon under different forest covers. Chin J Eco-Agri 17(1):41–47
Zheng YS, Ding YX (1998) Effect of mixed forests of Chinese fir and tsoong’s tree on soil properties. Pedosphere 8(2):161–168
Acknowledgements
This study was made possible with financial support from the Knowledge Innovation Program of the Chinese Academy of Sciences (KZCX2-YW-405) and the National Science Foundation projects (30590381-07). We also thank Zhang Xiuyong and Xu Guangbiao for assistance in collecting samples in the field.
Author information
Authors and Affiliations
Corresponding author
Additional information
Responsible Editor: Eric Paterson.
Appendix
Appendix
Linear Regression to Estimate Biomass in Kilograms for the Three Tree Species in This Study
species | component | Equation | R2 |
---|---|---|---|
C. lamcealata | Coarse root | \( {\hbox{Y}} = {1}.{932} \times {\hbox{V}} + {47}.{89} \) | 0.624 |
Medium root | \( {\hbox{Y}} = {1}.0{7}0 \times {\hbox{V}} + {36}.{31} \) | 0.601 | |
Fine root | \( {\hbox{Y}} = {1}.00{1} \times {\hbox{V}} + {9}.{546} \) | 0.643 | |
Stem wood | \( {\hbox{Y}} = {12}.{68} \times {\hbox{V}} + {184}.{3} \) | 0.944 | |
Stem bark | \( {\hbox{Y}} = {3}.{447} \times {\hbox{V}} + {61}.{89} \) | 0.759 | |
Branches | \( {\hbox{Y}} = {3}.{844} \times {\hbox{V}} + {85}.{66} \) | 0.660 | |
Foliage | \( {\hbox{Y}} = {7}.0{67} \times {\hbox{V}} + {152}.{2} \) | 0.746 | |
Stem root | \( {\hbox{Y}} = {2}.{873} \times {\hbox{V}} + {62}.{66} \) | 0.820 | |
Aboveground | \( {\hbox{Y}} = {25}.{59} \times {\hbox{V}} + {519}.0 \) | 0.895 | |
Belowground | \( {\hbox{Y}} = {6}.{89}0 \times {\hbox{V}} + {154}.{9} \) | 0.786 | |
Total biomass | \( {\hbox{Y}} = {32}.{48} \times {\hbox{V}} + {674}.0 \) | 0.900 | |
L. formosana | Coarse root | \( {\hbox{Y}} = {526}.{\hbox{6ln}}\left( {\hbox{V}} \right) - {1},{5}00 \) | 0.368 |
Medium root | \( {\hbox{Y}} = 0.{731} \times {\hbox{V}} + {124}.0 \) | 0.273 | |
Stem wood | \( {\hbox{Y}} = {21}.{9} \times {\hbox{V}} + {534}.{9} \) | 0.843 | |
Stem bark | \( {\hbox{Y}} = {3}.{717} \times {\hbox{V}} + {99}.{28} \) | 0.808 | |
Branches | \( {\hbox{Y}} = {8}.{683} \times {\hbox{V}} + {99}.{18} \) | 0.775 | |
Foliage | \( {\hbox{Y}} = {368}.{\hbox{5ln}}\left( {\hbox{V}} \right) - {1},0{57} \) | 0.537 | |
Stem root | \( {\hbox{Y}} = {592}.{\hbox{3ln}}\left( {\hbox{V}} \right) - {1},{649} \) | 0.650 | |
Aboveground | \( {\hbox{Y}} = {37}.{99} \times {\hbox{V}} + {928}.{1} \) | 0.892 | |
Belowground | \( {\hbox{Y}} = {11}.{56} \times {\hbox{V}} + {873}.{5} \) | 0.613 | |
Total biomass | \( {\hbox{Y}} = {49}.{56} \times {\hbox{V}} + {1},{8}0{1} \) | 0.875 | |
A. cremastogyne | Coarse root | \( {\hbox{Y}} = {2}.{1}0{2} \times {\hbox{V}} + {232}.{3} \) | 0.586 |
Medium root | \( {\hbox{Y}} = - 0.{36} \times {\hbox{V}} + {726} \) | 0.614 | |
Fine root | \( {\hbox{Y}} = - 0.{171} \times {\hbox{V}} + {289}.{7} \) | 0.450 | |
Stem wood | \( {\hbox{Y}} = {13}.{21} \times {\hbox{V}} + {1},{513} \) | 0.918 | |
Stem bark | \( {\hbox{Y}} = {13}.{21} \times {\hbox{V}} + {1},{513} \) | 0.798 | |
Branches | \( {\hbox{Y}} = {5}.{359} \times {\hbox{V}} + {4}0{8}.{9} \) | 0.600 | |
Foliage | \( {\hbox{Y}} = {5}.{333} \times {\hbox{V}} - {1},{1}0{9} \) | 0.598 | |
Cone | \( {\hbox{Y}} = {2}.{691} \times {\hbox{V}} - {527}.{8} \) | 0.654 | |
Stump root | \( {\hbox{Y}} = {1}.{883} \times {\hbox{V}} + {513}.{5} \) | 0.790 | |
Aboveground | \( {\hbox{Y}} = {28}.{24} \times {\hbox{V}} + {5}0{3}.{1} \) | 0.838 | |
Belowground | \( {\hbox{Y}} = {3}.{77}0 \times {\hbox{V}} + {1},{399} \) | 0.725 | |
Total biomass | \( {\hbox{Y}} = {32}.0{1} \times {\hbox{V}} + {1},{9}0{2} \) | 0.840 |
Y: the biomass of each component in gram. V = (DBH)2*height
Rights and permissions
About this article
Cite this article
Wang, S., Zhang, W. & Sanchez, F. Relating net primary productivity to soil organic matter decomposition rates in pure and mixed Chinese fir plantations. Plant Soil 334, 501–510 (2010). https://doi.org/10.1007/s11104-010-0400-8
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11104-010-0400-8