湿地林土壤的Fe2+,Eh及pH值的变化

通过在不同含水量 (田间持水量的 6 0 % :对照处理 ;田间持水量的 2 5 0 % :淹水处理 )和不同温度 (2 0℃ ,2 5℃ ,30℃ )条件下的室内培养 ,对江苏省里下河地区池杉湿地林土壤的二价铁离子 (Fe2 )浓度 ,氧化还原电位 (Eh)及 p H值进行了研究。结果表明 ,与对照处理相比 ,淹水土壤的 p H值和 Fe2 浓度明显提高 (P<0 .0 1) ,而 Eh值则明显降低 (P<0 .0 1)。在淹水条件下 ,高温处理的土壤 p H值和 Fe2 浓度明显高于低温处理土壤 (P<0 .0 1) ,Eh值则相反。研究表明 ,土壤 Eh值与 p H值之间存在着密切的 3次方程式关系 (P<0 .0 0 1)。就里下河地区湿地林土壤而言 ,Eh值下降至 2 0 0 m V以下时 ,才会有大量的铁元素被还原为Fe2 。     

Vegetation dynamics across a chronosequence of created wetland sites in Virginia, USA

Plant species composition, dominance, richness, and diversity were measured across a 15-year chronosequence of created wetland sites in Virginia, USA. Using an age-class categorization (1?C2?years, 3?C5?years, 6?C10?years, or 11?C15?years), all classes had a predominance of herbaceous species with perennial life history strategy, and perennials contributed 68.6?% to the overall dominance measure (importance value; IV) averaged across all sites. There was no significant difference in species richness or diversity among age classes. Analysis of Similarity (ANOSIM) indicated that herbaceous species composition was similar between the youngest and oldest age classes, but not the intermediate classes. For woody shrubs and saplings, planted species were more prevalent in the youngest age classes, and volunteer species predominated in the oldest age classes. These results suggest that perennial herbaceous species are important in early plant development on created wetland sites, and may be influential in observed patterns of species composition over time. In the context of plant development in newly created wetlands, dominance shifts from planted to volunteer woody species suggest that planting early successional species, or species with reproductive strategies attuned to created wetland site management, may favor survivorship and recruitment of other species over time.     

美国南卡罗来纳州森林湿地十种典型植物凋落叶的分解特征

凋落叶分解是控制森林湿地物质循环的重要生态过程,是全球C、N等元素循环的重要一部分。以美国南卡罗来纳州10种典型植物的凋落叶为研究对象,通过2a的分解实验测定分解阶段凋落叶的生物量残留率、分解速率常数k和C、N残留百分比,探讨初始凋落叶化学性质对分解速率常数k的影响。结果表明:(1)十种凋落叶生物量在两年内降解至初始的14.5%—66.2%,种间差异可达4倍以上;分解速率常数k在0.26—1.64a~(-1)之间,针叶分解速率阔叶分解速率;(2)分解速率常数k与初始凋落叶酸溶性组分(AS)极显著正相关(P0.001),与初始C含量、酸不溶组分(AIF)和AIF/N比均显著负相关(P0.05);(3)凋落叶C残留百分比持续下降至10.2%—66.1%,而N残留百分比因物种与分解阶段不同呈现不同变化规律。结果表明,森林湿地中凋落叶初始C组分差异是其分解速率的种间极大差异的主要原因,评估森林湿地的C、N循环应充分考虑种间差异。     

A comparison of wetland characteristics between Agricultural Conservation Easement Program and public lands wetlands in West Virginia,USA

In West Virginia, USA, there are 24 conservation easement program wetlands enrolled in the Agricultural Conservation Easement Program (ACEP). These wetlands are located on private agricultural land and are passively managed. Due to their location within fragmented agricultural areas, wetlands enrolled in ACEP in West Virginia have the potential to add wetland ecosystem services in areas that are lacking these features. We evaluated ACEP wetlands compared to reference wetlands on public land in West Virginia by using surrounding land cover, vegetative cover, and wetland features and stressors such as the presence or absence of erosion, upland inclusion, algal mats, and evidence of impacts from the surrounding landscape as surrogate measurements of wetland function on 13 ACEP wetlands and 10 reference wetlands. ACEP wetlands had higher percentages of tree coverage and a higher proportion of agricultural land in the areas immediately surrounding the wetland. Reference wetlands had higher percent coverage of emergent vegetation and had a higher proportion of forest in the immediate landscape. Our findings suggest that ACEP wetlands provide valuable early successional and forested wetland cover in a state that is largely forested. Because of this, it is important to maintain and even expand ACEP in West Virginia to continue providing a valuable source of early successional wetland habitat.     

Diversity of nitrite reductase (nirK and nirS) gene fragments in forested upland and wetland soils

The genetic heterogeneity of nitrite reductase gene (nirK and nirS) fragments from denitrifying prokaryotes in forested upland and marsh soil was investigated using molecular methods. nirK gene fragments could be amplified from both soils, whereas nirS gene fragments could be amplified only from the marsh soil. PCR products were cloned and screened by restriction fragment length polymorphism (RFLP), and representative fragments were sequenced. The diversity of nirK clones was lower than the diversity of nirS clones. Among the 54 distinct nirK RFLP patterns identified in the two soils, only one pattern was found in both soils and in each soil two dominant groups comprised >35% of all clones. No dominance and few redundant patterns were seen among the nirS clones. Phylogenetic analysis of deduced amino acids grouped the nirK sequences into five major clusters, with one cluster encompassing most marsh clones and all upland clones. Only a few of the nirK clone sequences branched with those of known denitrifying bacteria. The nirS clones formed two major clusters with several subclusters, but all nirS clones showed less than 80% identity to nirS sequences from known denitrifying bacteria. Overall, the data indicated that the denitrifying communities in the two soils have many members and that the soils have a high richness of different nir genes, especially of the nirS gene, most of which have not yet been found in cultivated denitrifiers.     

Characterization of aquabirnaviruses from flounder Pseudopleuronectes americanus and mummichog Fundulus heteroclitus in the Chesapeake Bay, Virginia, USA

Viruses were isolated in cell culture from tissue homogenates of flounder Pseudopleuronectes americanus and mummichog Fundulus heteroclitus in the Chesapeake Bay, Virginia, USA. Neutralization and immunofluorescence tests with aquabirnavirus (West Buxton strain)-specific polyclonal antisera indicated that both viruses were aquabirnaviruses belonging to Serogroup A, the most common aquabirnavirus serogroup in the United States. This was confirmed by RT-PCR, with primers targeting the VP3 and VP2 gene of aquabirnaviruses. The VP2-specific RT-PCR cDNA amplification product was sequenced and deduced amino-acid sequences were compared with known sequences of the type strains of the 9 serotypes of aquabirnavirus Serogroup A. This demonstrated that the viruses from both flounder and mummichog belong to aquabirnavirus Genogroup 1. The flounder isolate exhibited deduced amino acid sequence similarities of 98.1% with the Jasper strain of serotype A9, and 97.7% with the West Buxton strain of serotype A1. The isolate from mummichog exhibited deduced amino acid sequence similarities of 99.1% with the West Buxton strain of Serotype A1 and 94.8% with the Jasper isolate of Serotype A9. Similarities of deduced amino acid sequences ranged from 79.9 to 86.9%, with representatives of the other 7 serotypes. This is the first report of an aquabirnavirus from mummichog F. heteroclitus and only the fifth report of an aquabirnavirus from a flounder species.     

Recovery of novel bacterial diversity from a forested wetland impacted by reject coal

Sulphide mineral mining together with improperly contained sulphur-rich coal represents a significant environmental problem caused by leaching of toxic material. The Savannah River Site's D-area harbours a 22-year-old exposed reject coal pile (RCP) from which acidic, metal rich, saline runoff has impacted an adjacent forested wetland. In order to assess the bacterial community composition of this region, composite sediment samples were collected at three points along a contamination gradient (high, middle and no contamination) and processed for generation of bacterial and archaeal 16S rDNA clone libraries. Little sequence overlap occurred between the contaminated (RCP samples) and unimpacted sites, indicating that the majority of 16S rDNAs retrieved from the former represent organisms selected by the acidic runoff. Archaeal diversity within the RCP samples consisted mainly of sequences related to the genus Thermoplasma and to sequences of a novel type. Bacterial RCP libraries contained 16S rRNA genes related to isolates (Acidiphilium sp., Acidobacterium capsulatum, Ferromicrobium acidophilium and Leptospirillum ferrooxidans) and environmental clones previously retrieved from acidic habitats, including ones phylogenetically associated with organisms capable of sulphur and iron metabolism. These libraries also exhibited particularly novel 16S rDNA types not retrieved from other acid mine drainage habitats, indicating that significant diversity remains to be detected in acid mine drainage-type systems.     

Morphological and Molecular Characterization of Punctodera Stonei Brzeski, 1998 (Nematoda: Heteroderidae) from Virginia,USA

In August of 2021, several cysts with juveniles and eggs were discovered during a vegetation survey conducted at the Arlington National Cemetery, Virginia. Eight soil samples were collected from the rhizosphere region of the common grass (Festuca arundinacea L.) and processed at the Mycology and Nematology Genetic Diversity and Biology Laboratory (MNGDBL). Cysts were light to dark brown in color, and oval to pear-shaped without bullae in young cysts but present in older cysts and with prominent vulval cone. The juveniles had slightly concave stylet knobs projecting sometimes anteriorly, tail tapering gradually to a narrowly rounded terminus, and hyaline tail terminus conspicuous at least twice the length of stylet. The molecular analysis included the analysis of three gene sequence fragments: D2–D3 of 28S rRNA, ITS rRNA, and COI. The nematode species was identified by both morphological and molecular means as Stone''s cyst nematode, Punctodera stonei. Detection of P. stonei in Virginia represents a new record of this species in the United States, and a second report after Canada in North America.     

Field-based assessment of wetland condition,wetland extent,and the National Wetlands Inventory in Kentucky,USA

The economic and ecological importance of wetlands is well documented, but there are few studies that have assessed wetland condition and extent for the United States. Many states, including Kentucky, have had no statewide field evaluation of wetlands of any kind. The National Wetland Inventory (NWI) is the largest database for mapped wetlands in the United States and the most comprehensive source of wetland information for Kentucky, but its value for determining wetland condition is limited. Therefore, our objectives were to document wetland extent and condition and assess the agreement between the NWI and field-based wetland characteristics in Kentucky. We conducted field and remote-sensing based assessments of 352 wetlands across the state. NWI-mapped and field-assessed wetlands had similar large-scale patterns; however, for individual wetlands, classification often disagreed. Based on our wetland assessment method, wetlands appear to be of moderate condition, although we found differences among basins, dominant vegetation types, and landscape positions and much variation as many sites scored very low and high. Our findings support previous work showing that rapid assessments are valuable for determining wetland condition for ambient monitoring and other applications. Also, our results provide the foundation for future status and trends studies and suggest an urgent need to update the NWI in Kentucky and elsewhere. We suggest that the NWI could be improved by using newer technology that increases wetland mapping accuracy and including predictions of wetland condition using the enhanced NWI approach.     

美国俄亥俄州人工河滨湿地甲烷排放

2008年11月-2009年10月,在美国俄亥俄州哥伦布市Olentangy河河滨湿地,运用静态箱·气相色谱法对比研究了不同水文模式和植被生长状况下2种植被类型(人工植被和自然植被)淡水河滨恢复湿地甲烷(CH4)排放的时空规律,探讨了湿地土壤温度、水文条件、植被和土壤碳含量等因子对CH4排放的影响.结果表明,人工植被和自然植被湿地CH4排放通量均有明显的季节变化规律,但自然植被的淡水湿地CH4排放量仍明显高于人工植被湿地的排放量,其年排放量分别为68和114gCH4-C· m-2·a-1(P＜0.05),这是由于自然植被湿地相对于人工植被湿地有着更高的累积生产力.在2个实验湿地中,淹没深水区比干湿交替区有更高的CH4排放量,CH4排放通量的中值(平均值)分别为4.7(59.9)和0.09( 1.17)mg·m-2·h-1(P＜0.01),波动的水文相对于静止水文条件可减少CH4排放量.并且,实验湿地CH4排放通量与土壤温度和土壤有机碳含量有一定的相关性.因此,可通过对湿地进行适当的植物配置和水文条件等设计和管理措施有效地减少CH4排放.     

Litter decomposition in created and reference wetlands in West Virginia,USA

Large amounts of resources have gone into wetland mitigation in recent years; however, it is still unclear whether wetland function is being replaced along with wetland area. Litter decomposition is linked to numerous wetland functions. In this study, we measured plant litter decomposition potential over 12 months in 8 created and 8 reference wetlands located in the Allegheny Mountains of West Virginia, USA. Broadleaf cattail (Typha latifolia L.) litter bags were placed in each wetland and collected at 3 month intervals. Linear decomposition rate constants and percent mass remaining were similar between wetland types (created and reference) and among Cowardin classifications (palustrine: unconsolidated bottom, aquatic bed, emergent, and scrub/shrub). Created wetland age was not correlated with decomposition potential. Our study found that created wetlands had similar litter decomposition potential as reference wetlands indicating that similar processes are likely acting upon litter decomposition within both natural and created wetlands.     

Hydrochory,seed banks,and regeneration dynamics along the landscape boundaries of a forested wetland

Following the environmental sieve concept, the setting in which the recruitment of Taxodium distichum occurs in, becomes increasingly restrictive from the seed to seedling stage in an impounded forested wetland. Although a wide elevational band of dispersing seed moves across the boundary of a swamp-field in the water sheet, the zone of germination is relegated to that portion of the forested wetland that draws down during the growing season. Seedling recruitment is further restricted to the uppermost zone of the winter water sheet. These patterns are likely applicable to other species of dominant swamp species, e.g., Cephalanthus occidentalis crossed the boundary of a forested wetland and abandonded field in winter flooding (November–December and November–March, respectively) in Buttonland Swamp. The elevation of the boundary was 101.3 m NGVD. While the seeds of at least 40 swamp species were dispersed across the boundary, few viable seeds were dispersed after the winter season. Kriged maps showed seeds of T. distichum and C. occidentalis dispersed in patches in the water depending on the position of the water sheet. Most species of both water- and gravity-dispersed species had a localized pattern of seed distribution (either spherical or exponential) and this indicated that seeds may not be dispersed for great distances in the swamp. Water-dispersed T. distichum and C. occidentalis had larger dispersal ranges (A ₀=225 and 195 m, respectively) than Bidens frondosa and B. discoidea (A ₀=14 and 16 m, respectively). Seed dispersal varied with season depending on the availability of seeds. In Buttonland Swamp, viable seeds typically were dispersed for T. distichum in November–June, and for C. occidentalis in November-July. Low water occurred in August 1993 and high in February 1994 (99.8 and 101.6 m NGVD, respectively). The seed banks along the landscape boundary varied in species composition according to elevation (r ² = 0.996). While the similarity of species richness between water-dispersed seeds and the seed bank at elevations that flooded (during June 1993 through May 1995) was high (10–17%), it was low between water-dispersed seeds and the seed bank at elevations that did not flood (5%). T. distichum seeds had a short germination window in that seeds germinated within a year following their production in zones that were flooded in the winter followed by drawdown during the next growing season. After 1 year, less than 5% of the T. distichum seeds remained viable on the surface of the soil. Germination of T. distichum was confined to specific elevations (above 99.3 but below 101.6 m NGVD) during this study with 4.1% of the seedlings surviving for more than 2 years at a mean of 101.4 m NGVD. All seedlings below this elevation died. To maximize natural regeneration along the boundaries of swamps in abandoned farm fields targeted for restoration, this study suggests a flood pulse regime consisting of high water in the winter to maximize dispersal of live seeds followed by low water in the summer to facilitate seed germination and seedling recruitment. Hydrologic restoration could assist in the natural recovery of damaged wetlands if a seed source exists nearby.     

Primary production, nutrient dynamics, and accretion of a coastal freshwater forested wetland assimilation system in Louisiana

This study reports on the response of a tidal, freshwater forested wetland ecosystem to long-term input of secondarily treated municipal effluent from the City of Mandeville, LA. Measurements of hydrology, nutrients, and aboveground net primary productivity were made from September 1998 through March 2002. Accretion measurements were made in October 2000 and October 2004. The major hydrologic inputs to the system were the effluent, precipitation, and back water flooding from Lake Pontchartrain. Nutrient levels were generally low except in the immediate vicinity of the outfall. Mean net primary production of the freshwater forest system was significantly higher downstream of the effluent discharge (1202 g m⁻² yr⁻¹) compared to the control site (799 g m⁻² yr⁻¹). Downstream of the outfall, accretion rates were double the rate of relative sea level rise in the area. Removal efficiencies of N and P were as high as 75% and 95%, respectively. The relatively constant flow of secondarily treated municipal effluent buffered the downstream area from salinity intrusion during a region-wide drought. Re-direction of nutrient-enhanced effluents from open water bodies to wetland ecosystems can maintain plant productivity, sequester carbon, and maintain coastal wetland elevations in response to sea-level rise in addition to improving overall surface water quality, reducing energy use, and increasing financial savings.     

The contribution of trees to ecosystem methane emissions in a temperate forested wetland

Wetland‐adapted trees are known to transport soil‐produced methane (CH₄), an important greenhouse gas to the atmosphere, yet seasonal variations and controls on the magnitude of tree‐mediated CH₄ emissions remain unknown for mature forests. We examined the spatial and temporal variability in stem CH₄ emissions in situ and their controls in two wetland‐adapted tree species (Alnus glutinosa and Betula pubescens) located in a temperate forested wetland. Soil and herbaceous plant‐mediated CH₄ emissions from hollows and hummocks also were measured, thus enabling an estimate of contributions from each pathway to total ecosystem flux. Stem CH₄ emissions varied significantly between the two tree species, with Alnus glutinosa displaying minimal seasonal variations, while substantial seasonal variations were observed in Betula pubescens. Trees from each species emitted similar quantities of CH₄ from their stems regardless of whether they were situated in hollows or hummocks. Soil temperature and pore‐water CH₄ concentrations best explained annual variability in stem emissions, while wood‐specific density and pore‐water CH₄ concentrations best accounted for between‐species variations in stem CH₄ emission. Our study demonstrates that tree‐mediated CH₄ emissions contribute up to 27% of seasonal ecosystem CH₄ flux in temperate forested wetland, with the largest relative contributions occurring in spring and winter. Tree‐mediated CH₄ emissions currently are not included in trace gas budgets of forested wetland. Further work is required to quantify and integrate this transport pathway into CH₄ inventories and process‐based models.     

Diatoms as indicators of isolated herbaceous wetland condition in Florida,USA

Benthic, epiphytic, and phytoplanktonic diatoms, as well as soil and water physical–chemical parameters, were sampled from 70 small (average 0.86 ha) isolated depressional herbaceous wetlands located along a gradient of human disturbance in peninsular Florida to (1) compare diatom assemblage structure between algal types; (2) develop biological indicators of wetland condition; (3) examine synecological relationships between diatom structure and environmental variables, with the ultimate goal of developing an index of biological integrity using a single assemblage. Collected diatom samples were enumerated to 250 valves and identified to species or subspecies. An assessment of wetland condition was made using a landscape-scale human disturbance score (Landscape Development Intensity index, LDI), calculated for each site using land use maps and GIS.Assemblages from both impaired and reference sites were compared using blocked multi-response permutation procedures, the percent similarity index, and visually examined using non-metric multidimensional scaling (NMDS). No ecologically significant compositional differences were found within sites. Mantel's test (Mantel's r = 0.29, p < 0.0001) and NMDS (stress: 14.52, variance: 78.5%) identified epiphytic diatoms as the most responsive to human disturbance. Strong significant correlations (|r_s| > 0.50, p < 0.05) were found between epiphytic NMDS site scores and soil pH, specific conductivity, water total phosphorous, and LDI, while soil pH, water color, soil TP, and turbidity were also significantly correlated (p < 0.05).Metrics to assess wetland condition were developed using epiphytic abundance data. Epiphytic taxa sensitive or tolerant to human landscape modification were identified using Indicator Species Analysis, and autecological indices relating diatom sensitivity to nutrients, pH, dissolved oxygen levels, saprobity, salinity, and trophic status were calculated. Fourteen final metrics were identified, scored on an ordinal scale, and combined into the Diatom Index of Wetland Condition (DIWC). The DIWC was highly correlated with the disturbance score (Spearman's r_s = −0.71, p < 0.0001), although the results need to be validated.     

Dominant environmental factors in wetland plant communities invaded by Phragmites australis in East Harbor, Ohio, USA

Elevation, standing crop, disturbance and soil fertility often emerge from studies of freshwater plant communities as the dominant environmental factors determining both species richness and species composition. Few studies in North America have investigated the relationship between these factors and species abundance (standing crop) and species composition in the context of invasion by Phragmites australis. This study explores the influence of key abiotic and biotic variables on species abundance and composition across three Lake Erie wetlands differing in hydrology and Phragmites abundance in East Harbor, Ohio, USA. Standing crop for 92 species was related to standard sediment analyses, wave exposure, distance to shoreline, elevation, light interference, species density, and Phragmites standing crop in each of 95 1 × 1 m quadrats by using canonical correspondence analysis (CCA). Elevation (Axis I) and Phragmites standing␣crop-soil fertility (Axis II) explained 35.7 and 26.2%, respectively, of the variation in the species–environment relationships. Wave exposure was not a primary component of the first four canonical axes. Axis I was instrumental in describing species composition, separating wet meadow species from marsh species. Axis II was inversely related to species density for both wet meadow and marsh species. These findings generally support prevailing models describing the distribution of wetland plants along environmental gradients. Two discrepancies were noted, however: (1) species density was highest in the most sheltered sites and (2) wave exposure was directly associated with Phragmites standing crop-soil fertility gradient. The structural integrity of Phragmites stems, topographic heterogeneity and differential responses to anthropogenic disturbance may contribute to departure from prevailing multivariate models. This information has direct implications for local and regional wetland managers.     

Reproductive Ecology of American Black Bears in the Alleghany Mountains of Virginia,USA

We studied reproduction of American black bears (Ursus americanus) in western Virginia from 1994 to 2003. We handled 326 ≥2-year-old female black bears 672 times during summer trapping and followed 176 of these individuals through 424 winter den seasons. We examined 183 litters consisting of 455 cubs. Primiparity occurred at mean and modal ages of 3.8 and 3 years, respectively. Composite mean litter size was 2.49 (SE = 0.06) cubs/litter; 3- and 4-year-olds had smaller litters than older bears. We tracked reproductive synchrony using 5 indices and documented a resetting of this synchrony, likely in response to hard-mast failure. The amplitude of oscillations in synchrony indices dampened through time after the synchronizing events. Documentation and quantification of relationships between nutrient availability, reproduction and population dynamics can be used to inform population modeling efforts and more accurately forecast harvest. © 2011 The Wildlife Society.     

小兴安岭天然森林沼泽湿地生态系统碳源/汇

采用静态箱-气相色谱法与相对生长方程法,同步测定小兴安岭7种天然沼泽湿地(草丛沼泽-C、灌丛沼泽-G、毛赤杨沼泽-M、白桦沼泽-B、落叶松苔草沼泽-L-T、落叶松藓类沼泽-L-X、落叶松泥炭藓沼泽-L-N)的土壤呼吸(CO_2、CH_4)净碳排放量、植被年净固碳量,并依据生态系统净碳收支平衡,揭示温带天然沼泽湿地的碳源/汇作用规律。结果表明:(1)7种天然沼泽CH_4年通量(0.006—7.756 mg m~(-2)h~(-1))呈M(高于其他类型1.0—1291.7倍,P0.05)C、G、B(高于针叶林沼泽17.7—649.0倍,P0.05)针叶林沼泽变化趋势,其季节动态存在3种类型(C、G单峰型、M、B多峰型及针叶林沼泽排放与吸收交替型);(2)其CO_2年通量(157.40—231.06 mg m~(-2)h~(-1))呈G(高于森林沼泽28.7%—46.8%,P0.05)C(高于森林沼泽7.4%—22.5%,P0.05)森林沼泽的变化趋势,其季节动态存在2种类型(C、G、L-X和L-N双峰型和M、B、L-T单峰型);(3)C、G、M、B、L-N CH_4排放仅受0—40 cm不同土壤层温度所控制;7种天然沼泽土壤CO_2排放均受气温及0—40 cm不同土壤层温度所控制,但B、L-X、L-N受温度与水位综合控制;(4)其植被年净固碳量((2.05±0.09)—(6.75±0.27)t C hm-2a-1)呈C(高于其他类型65.4%—229.3%,P0.05)G、B、L-T、L-X、L-N(高于M 80.0%—99.0%,P0.05)M变化趋势;(5)7种天然沼泽的碳源/汇(-2.32—2.09 t C hm-2a-1)作用不同,C、B和L-N为碳吸收汇(C强汇、B和L-N弱汇),M、G、L-T和L-X则为碳排放源(M、G强源、L-T和L-X弱源)。因此,温带小兴安岭草丛沼泽为碳强汇、灌丛沼泽为碳强源、森林沼泽基本维持碳平衡(除M外)。     

Spatial and temporal simulation of soil CO2 concentrations in a small forested catchment in Virginia

The question of how to extrapolate point measurements of soil CO₂ processes to coarser scales remains unanswered because we know little about the spatial and temporal variability in the CO₂ concentration of soil air. In this work, we describe a series of simple physically-based models that simulate soil temperature, soil tension, and soil CO₂ processes. We apply these models to simulate the spatial and temporal dynamics of soil CO₂ concentrations throughout a small catchment in the Virginia Blue Ridge. Output from the simulations is compared with field measurements. We find that despite some model deficiencies, we are able to simulate the gross patterns through space and time of soil air CO₂ concentration. During the growing season when soil temperature is high, we find that soil water status is the limiting control on soil respiration and CO₂ concentration. We also find that soil CO₂ concentration can be high despite low respiration values due to decreased soil diffusivity as moisture fills pore spaces.