Adaptation of the LIGNUM model for simulations of growth and light response in Jack pine

LIGNUM is a whole tree model, developed for Pinus sylvestris in Finland, that combines tree metabolism with a realistic spatial distribution of morphological parts. We hypothesize that its general concepts, which include the pipe model, functional balance, yearly carbon budget, and a set of architectural growth rules, are applicable to all trees. Adaptation of the model to Pinus banksiana, a widespread species of economic importance in North America, is demonstrated.

Conversion of the model to Jack pine entailed finding new values for 16 physiological and morphological parameters, and three growth functions. Calibration of the LIGNUM Jack pine model for open grown trees up to 15 years of age was achieved by matching crown appearance and structural parameters (height, foliage biomass, aboveground biomass) with those of real trees. A sensitivity study indicated that uncertainty in the photosynthesis and respiration parameters will primarily cause changes to the net annual carbon gain, which can be corrected through calibration of the growth rate. The effect of a decrease in light level on height, biomass, total tree branch length, and productivity were simulated and compared with field data. Additional studies yielded insight into branch pruning, carbon allocation patterns, crown structure, and carbon stress. We discuss the value of the LIGNUM model as a tool for understanding tree growth and survival dynamics in natural and managed forests.     

Rapid production of high-strength cement-bonded particleboard using gaseous or supercritical carbon dioxide

This study deals with the effects of curing treatment with gaseous and supercritical carbon dioxide on the properties of cement-bonded particleboard (CBP) manufactured by the conventional cold-pressing method. The hydration of cement and the mechanism of improvement were examined using X-ray diffractometry (XRD), thermal gravimetry (TG-DTG), and scanning electron microscopy (SEM) observations. The results are as follows: (1) The curing of cement was accelerated concomitantly with the improvement in mechanical and dimensional properties of CBP significantly by curing with gaseous or supercritical carbon dioxide. (2) Supercritical carbon dioxide curing imparted boards optimal properties at a faster rate than did gaseous curing. (3) Accelerated formation of calcium silicate hydrate and calcium carbonate and the interlocking of those hydration products on the wood surface are potentially the main reasons for the superior strength of carbon dioxide-cured boards.     

Management effects on carbon stocks and fluxes across the Orinoco savannas

Across the physiognomic types of the Orinoco llanos, periodic inventories and changes in land-use between 1982–1992 are estimated. Results indicate that the area under pastures and forest plantations is increased by 0.005337×10⁶ km², whilts reducing the area of croplands by 0.000119×10⁶ km². This is a net increase of 0.005218×10⁶ km². The gross carbon release is 174.66 Tg C per year to the atmosphere and transferring from cultivated and native vegetation to wood products (1.62 Tg C per year) and slash (1.18 Tg C per year). The processes of land preparation contribute 1.40 Tg C per year to the atmosphere. From the tree savannas, woodlands and forests 0.73 Tg C per year are estimated to have been transferred to the soil following clearance and burning over this period, and 1.05 Tg C per year from herbaceous savannas when were buried and decomposed at 0.84 Tg C per year. The estimate of carbon balance here by inventories and changes in land-use approach indicates that the Orinoco llanos is a sink of −17.53 Tg C per year. The carbon turnover time in the Orinoco system is 68 years, which provides a limited route for carbon sequestration. The calculated potential of the Orinoco llanos for storing carbon is 8300 Tg C. Ecological options to achieve this potential value are addressed. However, nutrient deficiency and seasonal water supply are serious drawbacks to take into account for increasing carbon accretion. These results are particular for the Orinoco llanos, even though described processes could be similar to world-wide savannas, where a gradient of carbon heterogeneity exists.     

森林、造林、再造林和毁林的定义与碳计量问题

森林的定义与土地利用，土地利用变化和林业（LULUCF）碳吸收或排放的计量密切相关。同时也是造林，再造林和毁林（ARD）定义的基础；ARD的定义直接关系到《京都议定书》第三条第三款（3.3条款）ARD活动引起的汇清除的计量和大小。本文基于森林有关定义国际研讨会和IPCC有关LULUCF碳计量的方法学指南的研讨和交流。通过大量资料收集和信息查询，对主要国际公约，国际组织和各国森林和ARD的定义进行了调研。并分析讨论了不同定义及其对LULUCF碳计量的影响。提出了碳计量中需要关注的焦点问题。     

Nitrogen-fixation dynamics in a cut-and-carry silvopastoral system in the subhumid conditions of Guadeloupe, French Antilles

This paper summarizes several studies on N recycling in a tropical silvopastoral system for assessing the ability of the system to increase soil fertility and insure sustainability. We analyzed the N₂ fixation pattern of the woody legume component (Gliricidia sepium), estimated the recycling rate of the fixed N in the soil, and measured N outputs in tree pruning and cut grass (Dichanthium aristatum). With this information, we estimated the N balance of the silvopastoral system at the plot scale. The studies were conducted in an 11-year-old silvopastoral plot established by planting G. sepium cuttings at 0.3 m × 2 m spacing in natural grassland. The plot was managed as a cut-and-carry system where all the tree pruning residues (every 2-4 months) and cut grass (every 40-50 days) were removed and animals were excluded. No N fertilizer was applied. Dinitrogen fixation, as estimated by the ¹⁵N natural abundance method, ranged from 60-90% of the total N in aboveground tree biomass depending on season. On average, 76% of the N exports from the plot in tree pruning (194 kg [N] ha^–1 yr^–1) originated from N₂ fixation. Grass production averaged 13 Mg ha^–1 yr^–1 and N export in cut grass was 195 kg [N] ha^–1 yr^–1. The total N fixed by G. sepium, as estimated from the tree and grass N exports and the increase in soil N content, was about 555 kg [N] ha^–1 yr^–1. Carbon sequestration averaged 1.9 Mg [C] ha^–1 yr^–1 and soil organic N in the 0-0.2 m layer increased at a rate of 166 kg [N] ha^–1 yr^–1, corresponding to 30% of N₂ fixation by the tree. Nitrogen released in nodule turnover (10 kg [N] ha^–1 yr^–1) and litter decomposition (40 kg [N] ha^–1 yr^–1) contributed slightly to this increase, and most of the recycled N came from the turnover or the activity of other below-ground tree biomass than nodules. This revised version was published online in June 2006 with corrections to the Cover Date.     

Forest soils and carbon sequestration

Soils in equilibrium with a natural forest ecosystem have high carbon (C) density. The ratio of soil:vegetation C density increases with latitude. Land use change, particularly conversion to agricultural ecosystems, depletes the soil C stock. Thus, degraded agricultural soils have lower soil organic carbon (SOC) stock than their potential capacity. Consequently, afforestation of agricultural soils and management of forest plantations can enhance SOC stock through C sequestration. The rate of SOC sequestration, and the magnitude and quality of soil C stock depend on the complex interaction between climate, soils, tree species and management, and chemical composition of the litter as determined by the dominant tree species. Increasing production of forest biomass per se may not necessarily increase the SOC stocks. Fire, natural or managed, is an important perturbation that can affect soil C stock for a long period after the event. The soil C stock can be greatly enhanced by a careful site preparation, adequate soil drainage, growing species with a high NPP, applying N and micronutrients (Fe) as fertilizers or biosolids, and conserving soil and water resources. Climate change may also stimulate forest growth by enhancing availability of mineral N and through the CO₂ fertilization effect, which may partly compensate release of soil C in response to warming. There are significant advances in measurement of soil C stock and fluxes, and scaling of C stock from pedon/plot scale to regional and national scales. Soil C sequestration in boreal and temperate forests may be an important strategy to ameliorate changes in atmospheric chemistry.     

Amazonian deforestation and global warming: carbon stocks in vegetation replacing Brazil''s Amazon forest

Carbon stocks in vegetation replacing forest in Brazilian Amazonia affect net emissions of greenhouse gases from land-use change. A Markov matrix of annual transition probabilities was constructed to estimate landscape composition in 1990 and to project future changes, assuming behavior of farmers and ranchers remains unchanged. The estimated 1990 landscape was 5.4% farmland, 44.8% productive pasture, 2.2% degraded pasture, 2.1% ‘young’ (1970 or later) secondary forest derived from agriculture, 28.1% ‘young’ secondary forest derived from pasture, and 17.4% ‘old’ (pre-1970) secondary forest. The landscape would eventually approach an equilibrium of 4.0% farmland, 43.8% productive pasture, 5.2% degraded pasture, 2.0% secondary forest derived from agriculture, and 44.9% secondary forest derived from pasture. An insignificant amount is regenerated ‘forest’ (defined as secondary forest over 100 years old). Average total biomass (dry matter, including below-ground and dead components) was 43.5 t ha⁻¹ in 1990 in the 410 × 10³ km² deforested by that year for uses other than hydroelectric dams. At equilibrium, average biomass would be 28.5 t ha⁻¹ over all deforested areas (excluding dams). These biomass values are more than double those forming the basis of deforestation emission estimates currently used by the Intergovernmental Panel on Climate Change (IPCC). Although higher replacement landscape biomass decreases net emissions from deforestation, these estimates still imply large net releases.     

复合农林业系统碳贮量研究进展

CO2作为一种主要温室气体,其固存与排放对全球气候变化有重要影响。本文以复合农林业系统为研究对象,介绍了农林复合类型中林木、农作物、凋落物、土壤碳贮量的估算方法,并指出目前碳贮量研究方面的问题和发展方向,为碳循环研究提供部分基础研究数据和理论支持。     

井冈山自然保护区森林资源变化分析

以井冈山林相图为基础图形资料,根据1999年的二类清查资料建立数据库,建立森林资源地理信息系统,论述了森林资源的分布特征;统计了各种森林类型的面积;实现了资源现状的可视化以及森林类型自动查询和检索;并输出专题图.关于森林资源变化动态分析得出:从1988年至1999年井冈山自然保护区的森林覆盖率从73.1%增长到85%:有林地比例从77.80%增加到88.38%,1988年、1995年、1999年单位面积的蓄积量分别为65.25m3/hm2、96.15m3/hm2、105.50m3/hm2,蓄积显著增加后趋于稳定.1995年和1999年保护区总生物量分别为6 160 986.70t和6 245 181.834t,碳储量密度分别为86.82t/hm2和90.93t/bm2,平均增长1.83t/hm2·a,碳汇作用明显.     

黑龙江林业的发展应该关注森林碳汇问题

森林生态系统在全球碳循环与平衡中具有极为重要的和不可替代的地位和作用,随着《京都议定书》正式生效,森林碳汇问题已经越来越受到世界各国的重视。黑龙江省森林资源丰富,是我国最主要的林区,巨大的“碳汇”既具有重要的生态功能,也蕴藏着潜在的巨大经济利益,因此,研究我省应对《京都议定书》生效、开展森林碳汇项目的对策研究是极为必要的。