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Teak plantations date back to 1871 in Bangladesh.This study was designed to assess how teak monoculture has impacted the soil properties in Bangladesh.Multiple linear regression and correlation matrices were estimated to evaluate these impacts.The means of soil physicochemical properties were compared across various attributes of the plantations.Older plantations accumulated more organic carbon in the soils than the younger plantations.Excessive removal of litter from the forest floor resulted in reduced levels of N, P, K, and other nutrients in the soils.Since bulk density was continuously decreasing deeper into the soil, the penetration of mineral nutrients into the soil was low.Furthermore, moisture content in the topsoil was significantly lower than that in the bottom layers due to the exposed and dry condition of the forest floor under teak plantations.For improving depleted teak plantation soils, teak could be planted with other tree species rather than just in monocultures.In addition, the forest floor could be enriched with leguminous herbs and shrubs to improve soil health in these plantations. 相似文献
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不同造林措施对桉树人工林地土壤养分的影响 总被引：4，自引：0，他引：4
针对桉树人工林地力退化问题,通过比较两种造林措施下桉树人工林地土壤肥力特征发现,皆伐和造林时的人为活动对浅土层(0～20 cm)的土壤有松动作用,在一定程度上降低土壤容重,部分提高土壤持水量和孔隙度,但造林后林地土壤物理特性变差,炼山+机械挖桩造林措施对林地土壤物理性质破坏作用要明显高于伐根催腐造林;与皆伐前相比,两种造林措施均导致了林地土壤pH向酸性化方向发展;伐根催腐造林使得林地土壤有机质含量、全N、全K、Ca和Mg含量均较皆伐前大,炼山措施导致大量养分烧失和流失,故其最小;土壤微量元素中除了Cu以炼山造林地最大外,Fe、Mn、Zn、B均以伐根催腐造林地最大。 相似文献
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The Atlantic Forest has been deforested to the point that only about 7% of the original forest remains. Soil degradation, including loss of soil organic carbon (SOC), has often been associated with deforestation. In extensive areas previously occupied by Atlantic Forest the soil has a naturally compact subsoil horizon called the coeso. This layer challenges root development and plant productivity. The purpose of this study was to investigate soil carbon and selected physical characteristics under the influence of the native forest and post-deforestation agricultural practices. The management regimes were a native forest, a rubber tree plantation, a pasture and annual cropping. Two soil depths were investigated: 0 to 15 cm, corresponding to the A horizon; and 35 to 50 cm, corresponding to the coeso. Management influenced both SOC concentration and soil bulk density; however, SOC content was not significantly changed by any of the post-deforestation land uses. This result supports the annual cropping system that has been adapted by small landholders. Most interesting was the quantity of SOC found in the coeso, which was as much as 50% of the surface horizon. 相似文献
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云南热区西南桦人工纯林林地土壤的有机碳含量研究 总被引：1，自引：1，他引：1
在云南西双版纳的普文试验林场,通过对不同龄期西南桦人工纯林林地土壤有机碳含量的比较,并以当地的山地雨林、林龄较为接近的西南桦次生林和黄水(黄牛水 水锦树)次生林林地的土壤有机碳含量为参照,作了对比分析;还对西南桦人工纯林林地土壤的有机碳含量与其土壤肥力状况及物理性状的相关性进行了研究。结果表明:西南桦人工纯林随着林龄的增长,其林地土壤有机碳含量呈现出先维持再积累上升的趋势;15年生的西南桦人工纯林林地土壤的有机碳含量水平与黄水(黄牛水 水锦树)次生林相近,随其林龄的增长,预计会超过黄水(黄牛水 水锦树)次生林而接近于山地雨林。西南桦人工纯林林地土壤有机碳含量与其土壤全N、水解N、速效K含量、总孔隙度和毛管孔隙度等指标呈显著正相关,与土壤容重呈显著负相关,因此,西南桦人工纯林林地土壤的有机碳水平可用以指示其土壤的肥力状况。 相似文献
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桉树人工林与天然林土壤养分的对比研究 总被引：8，自引：0，他引：8
在野外调查取样和室内实验分析的基础上,对人工林与天然林的土壤养分进行比较分析,结果表明人工林土壤表层的有机质、全氮、全磷、全钾含量都明显低于天然林,反映了人工林对养分的旺盛需求和消耗,并且人工林还会造成土壤阳离子交换量的降低和土壤容重的增大。提出变炼山全垦为块状整地、轮栽并适当休闲养地、提高人工林生物多样性、建立复杂的人工林群落等措施,以实现桉树人工林土壤养分平衡与生态系统的良性循环。 相似文献
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On alluvial sandy loams in the western Llanos of Venezuela, biomass and inventories of macronutrients were determined for ten teak plantations (0.5–9 years old) and a mature forest stand which preceded them. Mean tree and stratified random sampling methods of estimating biomass are compared with regression estimates.Aboveground biomass of the mature forest averages 398 t ha?1. The average yearly productivity of biomass per ha of the teak plantations is greater on sites with soils having higher clay contents; It was measured as 23 t (9-year-old plantation), 16 t (7 years), 10–14 t (6 years) and 7–14 t (4 years).The original ecosystem stores per ha for these sites range between 8380 and 8840 kg N (total), 4550 and 4890 kg P, 2290 and 2540 kg K, 6720 and 6850 kg Ca and 960 and 1760 kg Mg.In the mature forest most N, P and Mg is stored in the soil, whereas 70% of the K and 40–50% of the Ca is stored in the vegetation. The ecosystem K stores of the teak plantations are an average of 40% lower than in the original forest. This difference is interpreted as being due to leaching loss caused by replacement of the original forest.Using data from the literature and from this study, a nutrient budget has been calculated for the first rotation period of teak. It is predicted that substantial amounts of Ca will be removed from the site by the teak harvest. These exports may not be replenished by atmospheric inputs and soil mineral weathering, especially on the highly productive sites. 相似文献
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Reclaiming sodic soils for wheat production by Prosopis juliflora (Swartz) DC afforestation in India
A green house pot trial was conducted to assess the impact of Prosopis afforestation on the productivity and fertility of degraded sodic soils in Haryana, India. Wheat (Triticum aestivum, L; cultivar HD 2329) plants were grown from seed on top soils collected from a chronosequence of 0, 5, 7, and 30-year-old Prosopis juliflora plantations established on highly sodic soils and a non-sodic reference soil collected from a local farm. The afforestation improved physical and chemical properties of surface soils by decreasing pH, electrical conductivity and exchangeable Na levels, and increasing infiltration capacity, organic C, total N, available P, and exchangeable Ca, Mg, and, K levels. The amelioration effect of the trees on top soil increased with duration of tree occupancy. Soil nutrient status under the 30-year-old plantation was higher than that of the non-sodic farm soil. The reduced soil sodicity and improved fertility contributed to higher germination, survival, growth, and grain yield of wheat plants grown on the Prosopis chronosequence soils, even surpassing the yield attained on the farm soil in the case of 30-year-old plantation soil. Sodium accumulation in the crop declined while N, P, K, Ca, and Mg uptake increased with soil plantation age reflecting the changing nutrient status of the rooting zone due to afforestation. Results confirmed that successful tree plantation may restore the productivity and fertility of highly degraded sodic soils. 相似文献
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Acacia plantation establishment might cause soil acidification in strongly weathered soils in the wet tropics because the base cations in the soil are translocated rapidly to plant biomass during Acacia growth. We examined whether soils under an Acacia plantation were acidified, as well as the factors causing soil acidification. We compared soils from 10 stands of 8-year-old Acacia mangium plantations with soils from 10 secondary forests and eight Imperata cylindrica grasslands, which were transformed into Acacia plantations. Soil samples were collected every 5–30 cm in depth, and pH and related soil properties were analyzed. Soil pH was significantly lower in Acacia plantations and secondary forests than in Imperata grasslands at every soil depth. The difference was about 1.0 pH unit at 0–5 cm and 0.5 pH unit at 25–30 cm. A significant positive correlation between pH and base saturation at 0–20 cm depth indicated that the low pH under forest vegetation was associated with exchangeable cation status. Using analysis of covariance (ANCOVA), with clay content as the covariate, exchangeable Ca (Ex-Ca) and Mg (Ex-Mg) stocks were significantly lower in forested areas than in Imperata grasslands at any clay content which was strongly related to exchangeable cation stock. The adjusted average Ex-Ca stock calculated by ANCOVA was 249 kg ha−1 in Acacia plantations, 200 kg ha−1 in secondary forests, and 756 kg ha−1 in Imperata grasslands at 0–30 cm. Based on a comparison of estimated nutrient stocks in biomass and soil among the vegetation types, the translocation of base cations from soil to plant biomass might cause a decrease in exchangeable cations and soil acidification in Acacia plantations. 相似文献
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Soil properties under an exotic plantation (Pinus caribaea) and an indigenous plantation (Podocarpus imbricatus) were compared with adjacent secondary forests and abandoned land in the tropical forest areas of Jianfengling National Nature
Reserve in Hainan province, southern China. The surface soil (0–0.2 m) under Pi. caribaea has higher bulk density, lower soil organic carbon, total N, total K, available N, microbial biomass carbon, and smaller
soil microbial communities (as indicated by soil Biolog profiles) than under Po. imbricatus. Both land use types showed negative cumulative soil deterioration index (DI) compared to secondary forests. However, compared
to abandoned land (DI = –262), the soil quality of Po. imbricatus showed improvement (DI = –194) while that of Pi. caribaea showed deterioration (DI = –358). These results demonstrated that these exotic pine plantations can significantly and negatively
influence soil properties. By contrast, our results showed that adoption of indigenous species in plantations, or natural
regeneration, can improve soil quality. 相似文献
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马尾松人工幼林土壤肥力变化及其综合评价研究 总被引：1，自引：0，他引：1
通过分析广西环江县桉树林及砍伐后种植马尾松和荒地的土壤化学性质,运用灰色关联分析方法,研究和评价马尾松和荒地取代桉树后土壤肥力变化状况。研究结果显示:取代桉树林后,4.0a马尾松和荒地的土壤碱解N、有效P、速效K、交换性Ca和有效Zn有所提高,土壤pH值有所改善,而全N、全P、全K、交换性Mg和有效Cu有所减少。0～20cm层土壤有机质和有效B有所降低,20～40cm层的反而有所提高。不同林龄马尾松和荒地的土壤综合肥力普遍较差。造林4年后,同土层马尾松林的土壤综合肥力低于荒地。除4.0a荒地0～20cm层的土壤综合肥力基本无变化外,其他4.0a马尾松和荒地土壤综合肥力都有不同程度退化,而以4.0a马尾松20～40cm层的土壤肥力退化最严重。研究结果可为马尾松人工幼林的配方施肥提供理论依据。 相似文献
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土壤水分-物理性质是衡量土壤质量的重要指标。本文测定了岷江上游理县云杉人工林、灌木林、经济林和农耕地的土壤物理性质。结果表明:(1)云杉人工林的土壤容重最小,土壤毛管孔隙度、非毛管孔隙度、田间最大持水量、毛管持水量显著高于其余3种植被类型;(2)灌木林与经济林的非毛管孔隙度、毛管持水量、田间最大持水量差异不显著,但灌木林的土壤容重显著小于经济林;(3)农耕地的土壤容重显著高于其余3种植被类型,非毛管孔隙度、毛管持水量、田间最大持水量显著低于其余3种植被类型。研究结果说明4种植被类型的土壤物理性质存在较大差异,选择合理的植被类型和减少人为干扰对于岷江上游地区植被恢复和生态功能改善具有重要的作用。 相似文献
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为了保持我国人工林的长期生产力和提高森林质量,达到可持续经营的目的。作者在以往研究工作的基础上,广泛收集了国内外有关成果与资料,概括论述了我国人工林森林生产力的现状、不能保持生产力的原因与机理以及长期保持人工林生产力的技术对策。按第八次清查的全国森林资源数据,每公顷蓄积量为89.79 m^3,其中天然林为104.6 m^3,人工林为52.76 m^3,人工林森林生产力明显低于天然林;我国优势树种人工林每公顷蓄积量也不高,如杉木为69.8 m^3,马尾松为56.2 m^3,落叶松为58.6 m^3,这些数据比日本2002年3月公布的人工林相似树种的数据低很多,如日本针叶树蓄积量为227.97 m^3·hm-2,柳杉为295.83 m^3·hm-2,落叶松为189.88 m^3·hm-2。关于年生长量,按全国第七次资源清查的中龄林与近熟林的数据做统计:杉木人工林5.2~4.2 m^3·hm-2,马尾松为3.2~1.8 m^3·hm-2,柏木为3.4~3.2 m^3·hm-2;但按作者掌握的我国重点或示范性、试验性小面积人工林生长量看,却很高,按我国编制的速生丰产林标准的生长量数据看比较高。我国大面积人工林生产力不高,短周期经营的杨树、桉树人工林也不高,主要原因是:(1)纯林化与针叶化严重。按第八次全国森林资源统计,纯林占人工林的85%,而且针叶化明显,人工乔木林10个优势树种中针叶林比例高达56.9%。人工纯林结构简单,生物多样性低,生物学上缺乏稳定性。人工纯林特别是针叶纯林,抗性低,抗自然灾害和大气污染能力均差,人工纯林维护地力的能力也弱。(2)集约育林的技术措施:立地控制技术未得到推广,适地适树适品种原则在育林中未能认真贯彻;密度、植被、地力控制技术也执行不力,大面积上的人工林仍属于粗放经营;连作引起林地土壤理、化、生物特性恶化,土壤质量衰退,导致林木生长不良,林分生产力逐代下降;造林作业造成水土流失,如杉木造林,传统的育林技术未得到明显改进,福建尤溪炼山后进行的3年观测结果表明,炼山和水土流失损失的有机质高达989.35 kg·hm-2,养分586.26 kg·hm-2。桉树在砖红壤进行的机耕整地,水土流失也很严重,不合理的造林作业,最终导致土壤质量与森林生产力下降。短周期培育人工林带来了2个重要问题,一是对林地肥力要求高,二是如何利用无性系才能保持长期生产力。短周期经营采用的无性系,生长速度快,生长量大,轮伐期短,养分需求量大,如刚果12号W5无性系,通常利用地上部分,以5~7 a的轮伐期计,消耗的养分达571.75 kg·hm-2,我国培养短周期人工林的土壤质量本底原本普遍不高,如果采取连作,土壤有机质养分会明显下降,土壤质量衰退,并对其功能产生危害。我国杨树、桉树等人工林要达到短周期持续经营,还需要实行多无性系造林。我国人工林长期生产力保持的技术对策,应采取先进的集约育林措施,包括遗传控制、立地控制、密度控制、植被控制与地力控制。 相似文献
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While edge effects on tree water relations are well described for closed forests, they remain under-examined in more open forest types. Similarly, there has been minimal evaluation of the effects of contrasting land uses on the water relations of open forest types in highly fragmented landscapes. We examined edge effects on the water relations and gas exchange of a dominant tree (Eucalyptus arenacea Marginson & Ladiges) in an open forest type (temperate woodland) of south-eastern Australia. Edge effects in replicate woodlands adjoined by cleared agricultural land (pasture edges) were compared with those adjoined by 7- to 9-year-old eucalypt plantation with a 25m fire break (plantation edges). Consistent with studies in closed forest types, edge effects were pronounced at pasture edges where photosynthesis, transpiration and stomatal conductance were greater for edge trees than interior trees (75m into woodlands), and were related to greater light availability and significantly higher branch water potentials at woodland edges than interiors. Nonetheless, gas exchange values were only ～50% greater for edge than interior trees, compared with ～200% previously found in closed forest types. In contrast to woodlands adjoined by pasture, gas exchange in winter was significantly lower for edge than interior trees in woodlands adjoined by plantations, consistent with shading and buffering effects of plantations on edge microclimate. Plantation edge effects were less pronounced in summer, although higher water use efficiency of edge than interior woodland trees indicated possible competition for water between plantation trees and woodland edge trees in the drier months (an effect that might have been more pronounced were there no firebreak between the two land uses). Scaling up of leaf-level water relations to stand transpiration using a Jarvis-type phenomenological model indicated similar differences between edge types. That is, transpiration was greater at pasture than plantation edges in summer months (most likely due to greater water availability at pasture edges), resulting in significantly greater estimates of annual transpiration at pasture than plantation edges (430 vs. 343lm(-2)year(-1), respectively). Our study highlights the need for landscape-level water flux models to account for edge effects on stand transpiration, particularly in highly fragmented landscapes. 相似文献
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采用时序研究法对甘肃小陇山林区日本落叶松人工林不同发育阶段(6、15、23、35 a)的土壤物理性质、化学性质进行多因子综合比较,利用主成分分析的方法,以主成分特征贡献率为权重,计算土壤肥力综合指标值,分析土壤性质的演变规律。结果表明:日本落叶松人工林发育至近熟林阶段,土壤物理性质变差,表现为土壤密度最大1.62g·cm-3,毛管孔隙度和最大持水量降至最低,分别为29.69%、24.45%,并且土壤有机质、氮、磷、钾、镁、钙含量也明显降低;而到成熟林阶段,土壤理化性质有显著改善,土壤密度降低为1.21 g·cm-3、毛管孔隙度和最大持水量恢复至45.56%、42.65%,土壤养分含量也有了很大的提高,甚至超过了中龄林阶段的水平;同时幼龄林、中龄林、近熟林和成熟林土壤性质综合得分分别为-0.329、0.188、-0.565、0.739,也表明近熟林土壤性质最差,成熟林土壤性质最好。 相似文献