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1.
Eugenio Díaz-Pinés Agustín RubioHelga Van Miegroet Fernando MontesMarta Benito 《Forest Ecology and Management》2011,262(10):1895-1904
We compared soil organic carbon (SOC) stocks and stability under two widely distributed tree species in the Mediterranean region: Scots pine (Pinus sylvestris L.) and Pyrenean oak (Quercus pyrenaica Willd.) at their ecotone. We hypothesised that soils under Scots pine store more SOC and that tree species composition controls the amount and biochemical composition of organic matter inputs, but does not influence physico-chemical stabilization of SOC. At three locations in Central Spain, we assessed SOC stocks in the forest floor and down to 50 cm in the mineral in pure and mixed stands of Pyrenean oak and Scots pine, as well as litterfall inputs over approximately 3 years at two sites. The relative SOC stability in the topsoil (0-10 cm) was determined through size-fractionation (53 μm) into mineral-associated and particulate organic matter and through KMnO4-reactive C and soil C:N ratio.Scots pine soils stored 95-140 Mg ha−1 of C (forest floor plus 50 cm mineral soil), roughly the double than Pyrenean oak soils (40-80 Mg ha−1 of C), with stocks closely correlated to litterfall rates. Differences were most pronounced in the forest floor and uppermost 10 cm of the mineral soil, but remained evident in the deeper layers. Biochemical indicators of soil organic matter suggested that biochemical recalcitrance of soil organic matter was higher under pine than under oak, contributing as well to a greater SOC storage under pine. Differences in SOC stocks between tree species were mainly due to the particulate organic matter (not associated to mineral particles). Forest conversion from Pyrenean oak to Scots pine may contribute to enhance soil C sequestration, but only in form of mineral-unprotected soil organic matter. 相似文献
2.
对江西大岗山地区不同发育阶段杉木林林地土壤有机碳变化特征进行了研究,并利用相关分析和逐步回归分析方法探讨了土壤因子对其的影响.结果表明,不同发育阶段土壤有机碳含量随土壤深度的增加而降低,各层次有机碳含量表现出明显的变异特征,变异程度为:40～60 cm土层>20～40 cm土层>0～20 cm土层,其中中龄林土壤变异最为显著;随杉木的生长发育,土壤有机碳含量从幼龄林到中龄林呈下降趋势,中龄林到过熟林则呈上升趋势;土壤有机碳含量与全N量、碱解N量、有效P含量等土壤因子密切相关;建立的从幼龄林到过熟林各阶段的土壤有机碳回归方程具有较高的回归精度,比较标准化回归系数法处理显示,土壤N状况是影响土壤有机碳变异的主导因子. 相似文献
3.
Carbon sequestration in the woody biomass of shelterbelts has been investigated but there have been no measurements of the
C stocks in soil and tree litter under this agroforestry practice. The objective of this study was to quantify C stored in
surface soil layers and tree litter within and adjacent to a 35-year-old shelterbelt in eastern Nebraska, USA. The 2-row shelterbelt
was composed of eastern red cedar (Juniperus virginiana) and scotch pine (Pinus sylvestris). A sampling grid was established across a section of the shelterbelt on Tomek silt loam (fine, smectitic, mesic Pachic Argiudolls).
Four soil cores were collected at each grid point, divided into 0–7.5 and 7.5–15 cm depth increments, and composited by depth.
Soil samples were analyzed for total, organic, and inorganic C, total N, texture, pH, and nutrient content. Under the shelterbelt,
all surface litter in a 0.5 × 0.5 m2 area at each grid point was collected prior to soil sampling, dried, weighed, sorted, and analyzed for total C and N. Average
soil organic carbon (SOC) in the 0–15 cm layer within the shelterbelt (3,994 g m−2) was significantly greater than in the cultivated fields (3,623 g m−2). The tree litter contained an additional ∼1,300 g C m−2. Patterns of litter mass and soil pH and texture suggested increased organic inputs by tree litter and deposition of wind-blown
sediment may be responsible for greater SOC beneath the shelterbelt. Further research is needed to identify the mechanism(s)
responsible for the observed patterns of SOC within and adjacent to the shelterbelt and to quantify the C in biomass and deeper
soil layers.
相似文献
| Thomas J. SauerEmail: |
4.
【目的】了解覆盖对毛竹Phyllostachys edulis林土壤物理性质及养分含量的影响,为毛竹笋用林覆盖经营提供理论依据。【方法】以湖北省咸宁市毛竹林为研究对象,采用不同覆盖措施连续覆盖3 a,分析比较不同土壤层次间物理性质及养分含量的差异。【结果】覆盖可改善表层(0~10 cm)土壤的物理性质,使该层土壤容重显著降低,毛管孔隙度、毛管持水量和最大持水量等显著提高(P<0.05)。覆盖对土壤全钾、有效磷和速效钾含量有显著影响,覆盖能显著提高表层土壤全氮、全磷、有效磷和速效钾含量及较深层(10~20 cm和20~40 cm)土壤有效磷和速效钾含量。总体来说,随着土壤层次的加深,覆盖对土壤养分的影响程度逐渐减小。毛竹林覆盖后,不同土层间土壤物理性质及养分含量存在显著差异,主要表现为随着土壤层次的加深,土壤最大持水量、毛管持水量、毛管孔隙度和总孔隙度等显著降低,土壤容重则表现出相反的趋势;除全钾外,其他土壤养分含量均在0~10 cm层最高。【结论】在不考虑其他因素的情况下,以稻草20 cm+谷壳10 cm方式覆盖对毛竹林土壤物理性质及养分含量的影响较好。 相似文献
5.
Youtao Si Li Xiong Yuehmin Chen Jinmao Zhu Jinsheng Xie Ren Gao Yusheng Yang 《Annals of Forest Science》2018,75(3):79
Key message
The vertical transport of dissolved organic carbon (DOC) is an important determinant of carbon distribution across a soil profile. The transport of DOC down a soil profile can be largely influenced by incoming DOC and soil organic carbon (SOC) levels, which insulate DOC from adsorption processes regulated by soil texture and Fe/Al mineralogy.Context
Uncertainties about how soil properties affect DOC transport through the soil profile require study because soils can differ strongly with respect to texture or Fe/Al mineralogy and yet retain similar quantities of DOC.Aims
This study aimed to assess the role of incoming DOC and native SOC in regulating DOC migration in soils and investigate the contribution of DOC movement to SOC allocation.Methods
We leached a standard DOC solution extracted from Castanopsis carlesii litter through two distinct soil types, using two leaching strategies: single leaching and sequential leaching. The two soil types under a natural Castanopsis carlesii (Hemsl.) Hayata forest and a natural Castanopsis fargesii Franch. forest, respectively, differ strongly with respect to soil texture, Fe/Al oxide abundances, and SOC nature.Results
With single leaching, where each of six soil layers making up an entire 0–100-cm soil depth profile received single doses of standard DOC solution, deeper soil layers retained more DOC than upper soil layers, with native SOC largely masking the effects of soil texture and Fe/Al mineralogy on DOC migration. Following sequential leaching, where a sixfold larger amount of standard DOC solution sequentially percolated through the six soil layers, the upper soil layers generally retained more DOC than deeper layers. Nevertheless, in sequential leaching, desorption-induced transfer of carbon from upper soil layers to deeper soil layers resulted in greater total carbon retention than in single leaching.Conclusion
Forest subsoils (40–100 cm) are well below C saturation, but DOC vertical movement from top soils only transfers limited organic carbon to them. However, DOC vertical movement may greatly alter SOC allocation along the top soil profile (0–40 cm), with part of outer sphere native SOC displaced by incoming DOC and migrating downwards, which is a natural way to preserve SOC.6.
Naoki Murata Seiichi Ohta Atsushi Ishida Mamoru Kanzaki Chongrak Wachirinrat Taksin Artchawakom Hiroyuki Sase 《Journal of Forest Research》2009,14(4):212-220
In several areas in Northeast Thailand, evergreen and deciduous forests coexist under uniform terrain and climatic conditions.
We compared depth and physical properties of soils between evergreen and deciduous forests in the Sakaerat Environmental Research
Station to clarify what factor determines their distribution. The averaged soil depths were 79 ± 27 cm and 135 ± 58 cm in
the deciduous and evergreen forests, respectively. The soils in the deciduous forests were relatively coarser in soil texture
than those in the evergreen forests, particularly in the surface layers. The average available water capacity of the solum
was lower in the deciduous forest soils (78 mm) than in the evergreen forest soils (123 mm). Compared with the evapotranspiration
from the evergreen forest in the study area, the available water capacity of the evergreen forest soil was almost the same
as the water deficit during the dry season (November–February), while that of the deciduous forest soil was lower and insufficient
to maintain the evapotranspiration. These results suggest that the distribution of deciduous and evergreen forests in the
study area was associated with soil water availability, which mainly depends on soil depth. 相似文献
7.
Mohammad Shaheed Hossain Chowdhury Shampa Biswas Md. Abdul Halim S. M. Sirajul Haque Nur Muhammed Masao Koike 《林业研究》2007,18(1):27-30
Status of organic carbon （C）, total nitrogen （N）, available potassium （K）, calcium （Ca） and phosphorus （P） in three different depths （0-5 cm, 5-15 cm and 15-30 cm） on two hill slopes of 35% and 55% in orange orchard cultivated by the Mro tribe of Chittagong Hill. Tracts （CHTs） were evaluated and compared with those in degraded bush forests, through digging three profiles in each land use. The content of all the five nutrients was found to be higher in the soil of orange orchard than in the soil of forest. But the variation was not consistent for both the slopes. The content varied depth wise also, having the highest value in surface soil in case of both the land uses on both the slopes. A mean available K content was significantly higher in orange orchard than in forest on 55% slope, while it was lower on 35% slope. Surface soil contained the nutrients of K and Ca with the amount of 0.2905-mg·g^-1 soil and 3.025-mg·g^-1 soil respectively in the orchard, while 0.1934-mg·g^-1 soil and 1.6083-mg·g^-1 soil were respectively in the forest. Organic carbon and total nitrogen were found more or less similar in surface soil on both the land uses showing a slight difference. Available P was found only in orange orchard, and in forest it was too little in amount to detect by the spectrophotometer. The degraded forests were poor in nutrient content due to high rate of soil erosion, which would be possible to be improved by bringing it under tree cover as proved by the adaptation of orange orchard there. 相似文献
8.
Quintino R. Araujo Guilherme A. H. A. Loureiro Sandoval O. Santana Virupax C. Baligar 《Journal of Sustainable Forestry》2013,32(6):625-647
Information concerning the classification of soils and their properties under cacao agroforestry systems of the Atlantic rain forest biome region in the Southeast of Bahia, Brazil is largely unknown. Soil and climatic conditions in this region are favorable for high soil carbon storage. This study is aimed to classify soils under cacao agroforestry and further, to quantify carbon stocks in these soil profiles. Soil classification was performed, and the amount of C stored was estimated, based on the thickness of the soil horizons, their bulk density, and total organic carbon stored. In the sites studied under cacao, four general classes of soils were identified: Ultisols, Oxisols, Alfisols, and Inceptisols. Carbon stocks in these soil profiles showed wide variation, ranging from 719.24 to 2089.93 Mg ha?1. Carbon stocks in soil surface and subsurface layers in different agroforestry systems with cacao (cacao cabruca, cacao?×?rubber tree, and cacao?×?erythrina) were comparable; however, total storage of organic C in these soils was higher than expected, compared to values reported for the International Soil Reference and Information Center (ISRIC), based on the FAO-UNESCO database, and were also higher than estimated regional soil data. 相似文献
9.
不同土地利用方式对土壤有机碳、氮含量的影响 总被引：3，自引：0，他引：3
土壤有机C、N的定量动态变化是评价不同土地利用方式对土壤质量影响的重要内容。本文比较了研究地区种植黑麦草(Lolium multiflorum Lam．)、百喜草(Paspalum notatum Flugge．)、桔树(Citrus reticulata Blanco．)和马尾松(Pinus Massoniana Lamb．)的四种土地利用方式对植物生物量和土壤有机C、N多年变化的影响。试验初期，四种土地利用方式的植物生物量几乎处于同一水平。经过10年长期试验后，黑麦草和百喜草的累计生物量分别是桔树的3．68和3．75倍，马尾松的2．06和2．14倍。地下部生物量的差异更为明显，黑麦草和百喜草两种草类地下部累计生物量都较桔树和马尾松高10倍之多。这表明草类较之乔木更有利于提高土壤有机C、N的含量。土壤有机C、N的含量变化主要发生在0．40cm土层。统计计算表明，10年期问，种植黑麦草和百喜草可使土壤有机C、N贮量每公顷分别约增加1．5吨和0．2吨，而种植桔树使土壤有机C、N贮量每公顷分别约减少1．2吨和0．02吨，种植马尾松使土壤有机C、N贮量每公顷分别约减少0．4吨和0．04吨。表4参10。 相似文献
10.
Land-use changes can modify soil carbon contents. Depending on the rate of soil organic matter (SOM) formation and decomposition, soil-vegetation systems can be a source or sink of CO2. The objective of this study was to determine the influence of land-use change on SOM distribution, and microbial biomass and respiration in an Andisol of the Chilean Patagonia. Treatments consisted of degraded natural prairie (DNP), thinned and pruned Pinus ponderosa plantations (PPP), and unmanaged second-growth Nothofagus pumilio forest (NPF). The soil was classified as medial, amorphic, mesic Typic Hapludands. Soil microbial respiration and microbial biomass were determined in the laboratory from soil samples taken at 0–5, 5–10, 10–20 and 20–40 cm depths obtained from three pits excavated in each treatment. Physical fractionation of SOM was performed in soil of the upper 40 cm of each treatment to obtain the three following aggregate-size classes: macroaggregates (>212 μm), mesoaggregates (212–53 μm) and microaggregates (<53 μm). Plant C content was 68% higher in PPP than in DNP and 635% higher in NPF than in PPP. Total soil and vegetation C content in both DNP and PPP were less than half of that in NPF. Total SOC at 0–10 cm depth decreased in the order DNP (7.82%) > NPF (6.16%) > PPP (4.41%), showing that land-use practices affected significantly (P < 0.01) SOC stocks. In all treatments, microbial biomass C and respiration were significantly higher (P < 0.05) in the upper 5 cm. Soil microbial respiration was also correlated positively with microbial biomass C and SOC. The different land uses affect the formation of organic matter, SOC and microbial biomass C, which in turn will affect soil microbial respiration. Conversion of DNP to PPP resulted in a 44% decrease of SOC stocks in 0–10 cm mineral soil. The largest amount of SOC was stabilized within the mesoaggregate fraction of the less disturbed system, NPF, followed by PPP. In the long term, formation of stable mesoaggregates in soils protected from erosion can behave as C sinks. 相似文献
11.
《Scandinavian Journal of Forest Research》2012,27(1-4):106-114
Decomposition of organic matter in forest soils controls mineralization of nutrients. The decomposition is to a large extent controlled by climatic and soil conditions. Four different soil treatments of water and nutrients were applied to a Norway spruce (Picea abies) stand in Denmark, and the relative changes in decomposition rate were quantified by the cotton strip assay. Additions of water and nutrients to the soil increased the decomposition of the cotton strips significantly, especially in the deeper soil layers. Reduced water addition during the summer, thereby creating ‘summer drought’, caused no changes in the decomposition compared to an untreated control situation, but the spatial variability in the decomposition within the treatment plot was strongly increased. The decomposition of the cotton strips decreased linearly with the soil depth (1st order). 相似文献
12.
Helga Van Miegroet Janis L. Boettinger Michelle A. Baker Julia Nielsen Dave Evans Alex Stum 《Forest Ecology and Management》2005,220(1-3):284-299
Relatively little is known about soil organic carbon (SOC) dynamics in montane ecosystems of the semi-arid western U.S. or the stability of current SOC pools under future climate change scenarios. We measured the distribution and quality of SOC in a mosaic of rangeland-forest vegetation types that occurs under similar climatic conditions on non-calcareous soils at Utah State University's T.W. Daniel Experimental Forest in northern Utah: the forest types were aspen [Populus tremuloides] and conifer (mixture of fir [Abies lasiocarpa] and spruce [Picea engelmannii]); the rangeland types were sagebrush steppe [Artemisia tridentata], grass-forb meadow, and a meadow-conifer ecotone. Total SOC was calculated from OC concentrations, estimates of bulk density by texture and rock-free soil volume in five pedons. The SOC quality was expressed in terms of leaching potential and decomposability. Amount and aromaticity of water-soluble organic carbon (DOC) was determined by water extraction and specific ultra violet absorbance at 254 nm (SUVA) of leached DOC. Decomposability of SOC and DOC was derived from laboratory incubation of soil samples and water extracts, respectively.
Although there was little difference in total SOC between soils sampled under different vegetation types, vertical distribution, and quality of SOC appeared to be influenced by vegetation. Forest soils had a distinct O horizon and higher SOC concentration in near-surface mineral horizons that declined sharply with depth. Rangeland soils lacked O horizons and SOC concentration declined more gradually. Quality of SOC under rangelands was more uniform with depth and SOC was less soluble and less decomposable (i.e., more stable) than under forests. However, DOC in grass-forb meadow soils was less aromatic and more bioavailable, likely promoting C retention through cycling. The SOC in forest soils was notably more leachable and decomposable, especially near the soil surface, with stability increasing with soil depth. Across the entire dataset, there was a weak inverse relationship between the decomposability and the aromaticity of DOC. Our data indicate that despite similar SOC pools, vegetation type may affect SOC retention capacity under future climate projections by influencing potential SOC losses via leaching and decomposition. 相似文献
13.
利用双指数模型预测中国不同森林带土壤有机碳矿化的动态变化 总被引：3，自引：0，他引：3
本文利用土壤培养实验和双指数模型(把土壤有机碳划分为活性碳和缓效性碳库)的方法,来分析确定长白山和祁连山的土壤有机碳的动态变化。分析和拟合土壤有机碳矿化释放的CO2的速率。结果表明:活性碳库占总有机碳的1.0%–8.5%,平均驻留时间的平均值为24天;缓效性碳库占总有机碳的91%–99%,平均驻留时间的平均值为179年。根据缓效性碳的大小和平均驻留时间可以得知,祁连山森林土壤的有机碳较长白山的难分解。通过分析影响森林土壤有机碳矿化的因素––土壤粘粒含量、海拔和温度,结果显示两种森林土壤有机碳的分解快慢与其温度正相关,并且长白山和祁连山的累积的土壤有机碳和缓效性碳的含量随土壤粘粒含量的增加而呈线性增加,其相关系数分别为0.7033和0.6575,充分表明温度和土壤粘粒含量对土壤有机碳的矿化有较大的影响。 相似文献
14.
Peter S. Homann Mark Harmon Suzanne Remillard Erica A.H. Smithwick 《Forest Ecology and Management》2005,220(1-3):270-283
How much organic C can a region naturally store in its ecosystems? How can this be determined, when land management has altered the vegetation of the landscape substantially? The answers may lie in the soil: this study synthesized the spatial distribution of soil properties derived from the state soils geographic database with empirical measurements of old-growth forest ecosystem C to yield a regional distribution of potential maximum total-ecosystem organic C stores. The region under consideration is 179,000 square kilometers extending from the southern Oregon border to the northern Washington border, and from the Pacific Ocean to the east side of the Cascade Mountains. Total ecosystem organic C (TEC) was measured in 16 diverse old-growth forests encompassing 35 stands and 79 pedons to a depth of 100 cm. The TEC ranged between 185 and 1200 Mg C ha−1. On an average, 63% of TEC was in the vegetation, 13% in woody detritus, 3% in the forest floor, 7% in the 0–20 cm mineral soil, and 13% in 20–100 cm mineral soil. The TEC was strongly related to soil organic C (SOC) in the 0–20 cm mineral soil, yielding a monotonically increasing, curvilinear relation. To apply this relation to estimate the TEC distribution throughout the region, 211 map units of the state soils geographic database (STATSGO) were used. The SOC in the 0–20 cm mineral soil of the map units was consistent with values from previously measured pedons distributed throughout the region. Resampling of 13 second-growth forests 25 years after initial sampling indicated no regional change in mineral SOC, and supported the use of a static state soils map. The SOC spatial distribution combined with the quantitative old-growth TEC–SOC relation yielded an estimate of potential TEC storage throughout the region under the hypothetical condition of old-growth forest coverage. The area-weighted TEC was 760 Mg C ha−1. This is 100 Mg C ha−1 more than a previous estimate based on a coarser resolution of six physiographic provinces, and 400 Mg C ha−1 more than current regional stores. The map of potential TEC may be useful in forecasting regional C dynamics and in land-management decisions related to C sequestration. 相似文献
15.
Gustavo álvarez-Arteaga Pavel Krasilnikov Norma Eugenia García-Calderón 《European Journal of Forest Research》2012,131(6):1643-1651
In montane cloud forests (MCF), the main soil organic carbon (SOC) pool is believed to be constituted by organic debris accumulated on soil surface and, to a lesser extent, by the organic fraction associated with the mineral matrix. The vertical distribution of SOC within soil has strong implications on the composition, stabilization and turnover of the soil organic matter (SOM). In ecosystems like MCF, where the climatic and edaphic conditions varied with altitude, the SOM accumulation and stabilization mechanisms possibly respond to these changes. For that reason, we studied the vertical distribution, accumulation and chemical composition of SOM in five montane cloud forest communities located between 1,500 and 2,500?m a.s.l. Two main SOC accumulation patterns were found: one at 1,500, 1,950 and 2,400?m a.s.l., with SOC content gradually decreasing with depth (cumulative); and another at 2,050 and 2,500?m a.s.l. where SOC had a strong maximum in the surface horizon and a less pronounced increase the spodic horizon (eluviation–illuviation pattern). The total SOC pool in soil decreased in inverse relation to altitude from 227?C?ha?1 at 1,500?m a.s.l. down to 143?mg?C?ha?1 at 2,500?m a.s.l. About 40–60?% of total SOC content corresponded to the surficial organic horizon. The chemical fractionation of the SOM denoted in general predominance of the fulvic acid fraction, and high content of humin and humic acid fractions. We considered that the main SOC vertical distribution processes were related to the raw humus accumulation, decomposition in situ, podzolization in the eluviation–illuviation pattern soils mainly. 相似文献
16.
Karna Hansson Bengt A. OlssonMats Olsson Ulf JohanssonDan Berggren Kleja 《Forest Ecology and Management》2011,262(3):522-530
Soil properties were compared in adjacent 50-year-old Norway spruce, Scots pine and silver birch stands growing on similar soils in south-west Sweden. The effects of tree species were most apparent in the humus layer and decreased with soil depth. At 20-30 cm depth in the mineral soil, species differences in soil properties were small and mostly not significant. Soil C, N, K, Ca, Mg, and Na content, pH, base saturation and fine root biomass all significantly differed between humus layers of different species. Since the climate, parent material, land use history and soil type were similar, the differences can be ascribed to tree species. Spruce stands had the largest amounts of carbon stored down to 30 cm depth in mineral soil (7.3 kg C m−2), whereas birch stands, with the lowest production, smallest amount of litterfall and lowest C:N ratio in litter and humus, had the smallest carbon pool (4.1 kg C m−2), with pine intermediate (4.9 kg C m−2). Similarly, soil nitrogen pools amounted to 349, 269, and 240 g N m−2 for spruce, pine, and birch stands, respectively. The humus layer in birch stands was thin and mixed with mineral soil, and soil pH was highest in the birch stands. Spruce had the thickest humus layer with the lowest pH. 相似文献
17.
[目的]以浙江省庆元县菇木林为研究对象,探讨菇木林目标树择伐后形成的人工林窗对土壤养分含量和土壤质量的影响.[方法]在对照林分和择伐后林窗内设置调查样地,分层采集0～60 cm土层土壤样品,对比分析土壤养分元素含量和土壤pH值的变化情况.[结果]1)与对照相比,择伐6 a后林窗0～20 cm土层,土壤有机碳、全氮、水解... 相似文献
18.
为揭示沉积在洼地不同位置土壤有机碳含量的分布特征和相关影响因素,以西南喀斯特典型小流域内洼地底部、落水洞不同部位土壤为研究对象,采集0~150 cm土壤剖面的土样,测定相关理化性质指标,分析土壤有机碳含量随空间位置的变化特征,并探讨土壤有机碳含量与理化性质的相关性。结果表明:落水洞、洼地底部土壤有机碳含量与土壤有机碳储量均为表层最高,呈表聚化现象;落水洞、洼地底部土壤有机碳含量与全氮含量均呈显著正相关,而与土壤含水率相关性不显著(P>0.05);落水洞土壤有机碳含量平均值大于洼地底部土壤有机碳含量平均值,土壤有机碳含量与土壤容重、总孔隙度分别呈极显著负相关、极显著正相关(P<0.01),与土壤pH值相关性不显著,表明落水洞土壤有机碳含量变化主要受土壤容重、总孔隙度等物理性质影响显著;洼地底部土壤有机碳含量变异系数大于落水洞土壤有机碳含量变异系数,土壤有机碳含量与土壤pH值呈显著的负相关关系(P<0.05),与土壤容重、总孔隙度相关性不显著,表明洼地底部土壤有机碳含量的分布特征主要受土壤pH值的影响。 相似文献
19.
Spatial pattern of soil carbon and nutrient storage at the alpine tundra ecosystem of Changbai Mountain,China 总被引：2，自引：2，他引：2
气候变化对土壤碳和养分的影响越来越受到生态学家的关注,尤其是对高山冻原生态系统的影响。本研究目的是长白山高山冻原系统土壤碳和养分的空间异质性。结果表明:不同土层深度的土壤碳在Meadow alpine tundra vegetation (MA)中显著地高于其他植被类型(p<0.05);在每一植被类型中,表层(010 cm)碳含量显著地高于1020 cm的土层;土壤氮的分布格局是氮素在表层和1020 cm土层变化规律相似;不同土层深度的土壤磷在Lithic alpine tundra vegetation (LA) 中显著地低于其他植被类型(p<0.05);土壤钾浓度在Felsenmeer alpine tundra vegetation (FA) 和LA中显著地高于其他植被类型,但在每一植被类型中土壤钾浓度随土壤深度没有明显的变化;不同深度土壤硫在MA中显著地高度其他植被类型;对每一植被类型而言,C: N, C: P, C: K 和C: S随土壤深度增加而降低。除了在SA的表层外,表层的土壤C: N高于1020 cm的土层。在长白山高山冻原系统中,随植被类型的变化,土壤碳和养分储量有着显著的空间异质性。参29表3图1。 相似文献
20.
Felipe García-Oliva Juan F. Gallardo Lancho Noé Manuel Montaño Pilar Islas 《Agroforestry Systems》2006,66(2):93-100
Gains and losses of soil carbon (C), have been reported when tropical forests are converted to pastures. Regional studies
are crucial for setting regional baselines and explaining each particular trend, in order to solve this controversy. Tropical
deciduous forest (TDF) is under high deforestation pressure, mainly for conversion to pastures. The present study compared
soil organic C (SOC) and nitrogen (SON) in the surface layer (0–5 cm) of forest and pasture soils in a TDF of western Mexico.
SOC and SON concentrations were 18 and 60% lower in pasture soils than in forest soils, and C:N ratio increased in pasture
soils. Furthermore, pasture soils had lower labile C and available inorganic nitrogen (N) than forest soils. These results
can be explained as a reduction in C inputs to pasture soils and management-induced disruption of soil aggregates. In forest
soils, macroaggregates (> 250 μm) were predominant (85%), whereas in pasture soils they were reduced to 35% of dry sand-free soil mass. The estimated SOC
and SON losses from the top 5 cm of soil were 3 Mg C ha−1 and 0.9 Mg N ha−1, respectively. 相似文献