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1.
以围封保护和自由放牧油蒿草场为研究对象,通过野外调查与室内分析,研究了围封和放牧条件下沙地草场生物量和植被-土壤碳密度。结果表明:(1)自由放牧使油蒿群落中植物种类增加,但降低了植物群落盖度。自由放牧不仅导致油蒿草场地上、地下总生物量降低,也使得油蒿地上、地下生物量占群落地上、地下总生物量的比例减小。生长季自由放牧样地凋落物生物量显著大于围封保护样地(P0.05);(2)围封保护样地植被碳密度大于自由放牧样地,土壤碳密度却小于自由放牧样地,但两个样地间差异不显著(P0.05);(3)油蒿草场90%以上的碳储存于土壤中,围封保护样地和自由放牧样地油蒿草场土壤碳密度占植被-土壤系统碳密度的91%、93%;(4)围封保护油蒿草场碳密度为2.29 kg/m2,自由放牧油蒿草场碳密度为2.68 kg/m2,两个样地间差异不显著,自由放牧对油蒿草场碳密度影响不大。  相似文献   
2.
Abstract Endozoochory has proven to be a highly effective mechanism in the dispersal of viable seeds in Mediterranean grasslands. We studied the effect of cattle dung application on species richness, particularly on the reintroduction of species lost after abandonment. Sown and control plots were monitored for 3 years after dung sowing. We found a significant increase in small‐scale richness, which may be attributed to the treatment, with the inclusion of species detected in the dung and in the grazed pasture. The differences in richness and floristic composition diminished over time. This experiment proves the potential utility of this treatment for the restoration of species richness in abandoned pastures, although supplementary steps are necessary, including further sowing and/or shrub cutting in subsequent years.  相似文献   
3.
Heterotrophic decomposition of organic matter dictates that substrate supply rate, including energy and nutrients, can limit soil microbial activity. In New Zealand, soils are naturally deficient in nitrogen and phosphorus. Fertiliser application is a part of pastoral agriculture, the countrys most widespread land use. We postulated that organic soils under grazed pasture and pristine forest would be at the extremes of substrate quality and supply rate, and thus potential microbial response to food opportunities. Soil microbial responses to the addition of fresh energy (sucrose) were determined by laboratory experiments with root-free samples and intact cores including roots. Responses were quantified by respiration and respired carbon (C) isotope (13C) enrichment measurements. A supra-trace sucrose dose (0.002 mol kg–1 (soil)) caused the forest soils microbial respiration rate to nearly double within 2 h. The peak response took 20 h, and saturation occurred beyond a sucrose dose of 0.05 mol kg–1 (soil). Intact soil cores from the forest had similar respiration rates and responses. For root-free soil samples from the grazed pasture, respiration response to sucrose was nearly immediate, dose dependent, and there was up to a 9-fold increase in the rate. Intact cores from the pasture had much higher respiration rates, but a similar response to sucrose. For both soils, the similarity of sucrose application effects on respiration and relative 13C enrichment of the respired carbon was striking.  相似文献   
4.
Low input legume-based agriculture exists in a continuum between subsistence farming and intensive arable and pastoral systems. This review covers this range, but with most emphasis on temperate legume/grass pastures under grazing by livestock. Key determinants of nitrogen (N) flows in grazed legume/grass pastures are: inputs of N from symbiotic N2 fixation which are constrained through self-regulation via grass/legume interactions; large quantities of N cycling through grazing animals with localised return in excreta; low direct conversion of pasture N into produce (typically 5–20%) but with N recycling under intensive grazing the farm efficiency of product N: fixed N can be up to 50%; and regulation of N flows by mineralisation/immobilisation reactions. Pastoral systems reliant solely on fixed N are capable of moderate-high production with modest N losses e.g. average denitrification and leaching losses from grazed pastures of 6 and 23 kg N ha–1 yr–1. Methods for improving efficiency of N cycling in legume-based cropping and legume/grass pasture systems are discussed. In legume/arable rotations, the utilisation of fixed N by crops is influenced greatly by the timing of management practices for synchrony of N supply via mineralisation and crop N uptake. In legume/grass pastures, the spatial return of excreta and the uptake of excreta N by pastures can potentially be improved through dietary manipulation and management strategies. Plant species selection and plant constituent modification also offer the potential to increase N efficiency through greater conversion into animal produce, improved N uptake from soil and manipulation of mineralisation/immobilisation/nitrification reactions.  相似文献   
5.
Bei den jüngsten Ausgrabungen am hallstattzeitlichen Fürstengrabhügel Magdalenenberg bei Villingen wurden vorzüglich erhaltene und autochthone Pflanzenreste geborgen, darunter 30 Arten von Bryophyten. Diese ließen sich folgenden rezenten ökologischsoziologischen Gruppen zuordnen: Halbtrockenrasen-Arten, Arten verdichteter Erdblößen, Waldboden-Bewohner, Arten frischer bis nasser Standorte, Euryöke. Durch aktualistischen Vergleich der Moos-Synusien mit heutigen Pflanzengesellschaften im gleichen Naturraum ließ sich entschlüsseln, daß das Gelände damals mit extensiv beweideten Halbtrockenrasen bewachsen war; die Tätigkeit der Hügelbauer spiegelt sich in einer Überlagerung mit “Ruderalmoosen” wider. Durch Samenpflanzen-Funde konnte die Rekonstruktion weiter präzisiert und abgesichert werden.  相似文献   
6.
Factors influencing the seasonal and daily variation in denitrification rates in grazed swards were examined at 5 experimental sites in England with wide ranging environmental/geographic conditions. There was a wide range of fertilizer inputs at each site. Rates of denitrification were estimated by a coring and field incubation technique using acetylene to inhibit the reduction of N2O to N2. Major features of the detailed results from two of the sites were: (i) the large ranges in rates of loss, (ii) the relatively low contributions to total annual loss during autumn and winter, (iii) the apparent association of high rates of loss with fertilizer additions made when the soil was wet or immediately preceding a rainfall event, and (iv) significant losses from soil at 10–30 cm in the profile. Multiple quadratic regression analysis of the effects of soil NO3 --N, soil temperature and water was used to explain variability in rates of loss. When separate regressions were fitted within each site × year × season × fertilizer level subset, 51% of the variation in loss was explained on a poorly drained fine loam/silt but only 38% on a freely drained loam.  相似文献   
7.
Measurements of net mineralization using a field incubation method were made over a full growing season (180 d). Soil cores, taken from cut swards which for many years had been previously grazed by cattle, were placed in jars in the field for successive incubation periods of 14 d. Acetylene was added to the incubation jars to inhibit nitrification in the soil cores and thereby prevent losses of N through denitrification. Net mineralization over 180 d amounted to 415, 321 and 310 kg N ha–1 under grass/clover, unfertilized grass and grass receiving 420 kg N ha–1 y–1, respectively. At the start of the growing season, an index of potentially mineralizable N in the soil was estimated by a chemical extraction method, but this index was <50% of the estimates obtained by field incubation. The amount of N in herbage harvested regularly from the swards also under-estimated the supply of N from the soil, with apparent recoveries of 53, 82 and 74% and total yields of N of 240, 263 and 538 (kg N ha–1) from grass/clover, unfertilized grass and fertilized grass, respectively. Mineralization rates varied significantly with seasonal soil temperature fluctuations, but the incubation method was apparently less sensitive in relation to changes in soil water content. Rates of N-turnover (as % of total soil N) were highest under grass/clover (9%), but similar under fertilized and unfertilized grass swards (approximately 5%).  相似文献   
8.
黄土高原围封与自然放牧草地碳交换特征   总被引:1,自引:0,他引:1  
用静态箱法于2012年3月~2013年2月对黄土高原自然放牧及其围封6年的草地土壤呼吸和净生态系统CO2交换速率进行为期1年的实地观测。结果表明:(1)围封和自然放牧草地全年的碳交换总量均表现为碳汇,即CO2净吸收;围封草地全年净生态系统碳交换量为(-58.0±14.5)g·m-2,其中生长季和非生长季交换量分别为(-70.3±11.4)g·m-2和(12.4±3.1)g·m-2;自然放牧草地生态系统全年碳交换量为(-48.7±14.0)g·m-2,其中生长季和非生长季交换量分别为(-56.9±10.6)g·m-2和(8.1±3.3)g·m-2。(2)草地净生态系统CO2交换速率生长季主要受土壤含水量的控制,而在非生长季则主要受土壤温度的控制;草地土壤呼吸速率主要受土壤温度和土壤含水量共同影响,其中在生长季受土壤含水量的影响作用更大,而在非生长季则受土壤温度的影响作用更大。(3)土壤有机质含量的差异是造成围封草地土壤呼吸速率大于自然放牧草地的主要原因。(4)研究区草地存在土壤呼吸负通量现象,样地灰钙土偏高的碱性条件(pH8.2)促进了土壤次生碳酸盐的淀积可能是造成这一现象的主要原因。  相似文献   
9.
Alterations to ecosystem nitrogen (N) cycling by introduced plant species may increase the invasibility of habitat providing a positive feedback for the introduced species to become invasive. Spatial patterns of foliar and soil δ15N ratios reflect variation in rates and process of N‐cycling across invaded landscapes and provide insight into N‐source uptake and utilization strategies of invasive plant species. To evaluate invasion‐associated changes in soil and foliar δ15N at different scales: regional (among different sites), local (between north‐ and south‐facing aspect at the same site), and microsite (within populations in the same community), we measured foliar and soil δ15 N, animal faeces cover (as a proxy for grazing intensity) and N2‐fixing species cover from inside to outside Thymus vulgaris L. (thyme)‐invaded lightly grazed pastoral communities in Central Otago, southern South Island, New Zealand. Mean thyme foliar δ15N were near‐zero across the invaded landscape, and did not change across the advancing edge of invasion or with aspect. There was no evidence that associations with N2‐fixing species provide a potential N source. Soil δ15N was lower inside of thyme compared to at the edge or outside of thyme and was varied between aspects at some sites. Animal faeces cover as a proxy for grazing intensity explained only 23% of this observed variation of soil δ15N. Thyme invasion may result in lowered soil δ15N reflecting alterations to N dynamics. Associated invasion‐related impacts of animal grazing may also impact soil δ15N. Further studies are required to distinguish the underlying mechanism responsible for the observed patterns of foliar and soil δ15N values across thyme‐invaded Central Otago landscapes.  相似文献   
10.
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