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91.
干旱是影响宁夏东部沙化区荒漠草地退化的主要自然因素,也是天然草地补播成功率低的主要原因,该地区大面积种植的柠条是土壤覆盖保水的丰富资源,但是缺乏相关研究。选择平坦的、未生长柠条的退化天然补播草地作为研究对象,在临近有柠条生长的草地平茬其柠条枝条用于试验覆盖,研究不同柠条覆盖厚度(TSM0,覆盖0 cm;TSM1,覆盖1 cm;TSM2,覆盖2 cm;TSM3,覆盖3 cm)对该地区荒漠草地0~40 cm土壤水热以及补播牧草地上生物量的影响。结果表明,柠条枝条覆盖显著提高了土壤含水量,并且随着覆盖厚度的增加逐渐增大,但2018和2019年间所有覆盖处理下0~20 cm土壤水分平均值与TSM0之间差异不显著(P>0.05);在20~40 cm土层,3种柠条枝条覆盖厚度明显较对照提高了土壤水分含量,表现出TSM3>TSM2>TSM1>TSM0的趋势。结果还表明,柠条枝条覆盖还具有降低草地0~10 cm温度的作用,生长季8:00、14:00和18:00的土壤温度总体均随着柠条枝条覆盖厚度的增加出现降低趋势,且2019年土壤温度随着覆盖厚度的增加,变异系数也在减小,依次为4.6%、2.3%、1.7%,表明覆盖对土壤温度的变化具有缓冲作用。补播牧草地上生物量亦随着覆盖厚度的增加而增大,蒙古冰草、沙打旺及补播的3种牧草的总生物量均与草地20~40 cm土壤水分呈显著正相关(P<0.05)。本研究表明,柠条枝条覆盖有效地改善了荒漠草地土壤的水热,提高了土壤墒情,为牧草种植提供了良好的生长环境,可为该地区及类似地区退化草地的补播改良提供技术借鉴。  相似文献   
92.
阐明长期有机物料施肥下土壤CO2排放特征及其影响机制以及碳库管理指数对黄土高原旱作农业区固碳减排及施肥模式选择的影响尤为重要。基于2012年设置在陇中黄土高原旱作区的长期定位试验,通过不施肥(CK)、氮肥(NF)、有机肥(OM)、秸秆(ST)、有机肥结合无机肥(OMNF)5个处理,测定并计算了2018年不同施肥措施下全年土壤CO2排放、作物碳排放效率和碳库管理指数的变化,并运用结构方程模型分析了0~30 cm土壤温度、水分、微生物量碳氮、易氧化有机碳、蔗糖酶、脲酶与土壤CO2排放速率的关系。结果表明:1)与不施肥相比,秸秆、有机结合无机肥和有机肥处理使生育期土壤CO2排放平均速率提高了42.72%、30.82%和29.79%,秸秆、有机肥处理分别使生育期土壤CO2排放量显著提高36.35%、32.45%(P<0.05),有机结合无机肥处理使碳排放效率显著降低41.10%(P<0.05);2)有机物料处理均能显著提高0~5 cm土层易氧化有机碳、微生物量碳氮、蔗糖酶活性和碳库管理指数,相比不施肥和氮肥处理,有机结合无机肥处理分别使0~30 cm土壤碳库管理指数提高127.41%,99.33%(P<0.05);3)结构方程模型表明,环境因子对土壤CO2排放速率的总解释度为53%,对土壤CO2排放速率总效应较大的影响因素包括土壤温度(2.36)、微生物量碳(1.59)和土壤水分(1.18),且均间接地影响着土壤CO2排放速率,土壤温度促进了微生物量碳和蔗糖酶活性的提高,微生物量碳促进了微生物量氮和易氧化有机碳的增加。综合来看,有机结合无机肥处理可以提升土壤碳库管理指数,保持微生物活性,增加作物产量,降低土壤碳排放效率,是陇中黄土高原旱作农业区比较适宜的农田培肥措施。  相似文献   
93.
新疆草地优势种植物相对生物量沿海拔梯度变化特征   总被引:1,自引:0,他引:1  
优势种作为草地生态系统中地上生物量的主要贡献者,其生物量既受到环境因素的影响,也受到共存种种间关系的影响。然而,由于物种的不同和环境梯度的差异,目前有关优势种生物量与环境因素关系的研究,尚未获得一致性的结论。基于此,本研究以2011-2013年对新疆9种草地类型397个样地中优势种相对生物量的调查数据为基础,首先统计了不同草地类型中优势种组成,其次通过一般线性模型分析了优势种相对生物量随海拔梯度变化特征,以及共存优势种相对生物量之间的关系。结果显示:1)新疆草地共有169个优势种,隶属31科120属。这些优势种主要以禾本科植物为主,占据了优势种的19.53%。其中,高寒草原、温性草甸草原、温性草原、温性荒漠草原和温性草原化荒漠中,最主要的优势种均为针茅。而在高寒草甸、山地草甸和温性荒漠中,最主要的优势种则分别为珠芽蓼、千叶蓍和角果藜;2)优势种相对生物量与海拔的关系可以归为5类,分别呈现无显著关系、先降低后升高的U型变化趋势、显著正相关关系、显著负相关关系和先增加后降低的单峰型关系。这5类关系所对应的优势种数量分别为50、9、8、6和4个,分别占优势种总数的64.9%、11.7%、10.4%、7.8%和5.2%;3)24个共存优势种之间,其相对生物量共存在19对显著关系,且大多数共存优势种相对生物量之间主要表现为负相关关系。本研究表明,优势种相对生物量与海拔的关系,因物种不同呈多种变化格局且受到共存优势种的影响,结果可对未来新疆草地地上生物量的维持和管理,提供一定的参考依据。  相似文献   
94.
Soil aggregate (SA) can be formed and stabilized when soil organic matter (SOM) is decomposed in the soil. However, the relationships between the SA dynamics and SOM with different decomposition rates have not been clarified. Therefore, this study examined the effects of the addition of polysaccharides to soil on SA formation and stability. A Japanese tropical soil was incubated for 99 d at 30 °C in a dark environment following the addition of 0.5% (w/w) starch or cellulose. The decomposition rates of the amendments, and SA formation and stability were evaluated by measuring soil respiration rates, and distribution fractions of soil aggregate sizes and mean weight diameter (MWD) of SA, respectively. The cumulative soil respirations with all treatments rapidly increased until Day 12 of the incubation. The initial slope of the cumulative soil respiration in the soil with starch was significantly higher than that in the soil with cellulose. In either soil with starch or cellulose, the fractions of macro-aggregates (>1000 μm in diameter) significantly increased, respectively, compared with control soil. However, the fractions of meso-aggregates (250–1000 μm) and nano-aggregate (<20 μm) in the soil with starch significantly decreased, while those fractions in the soil with cellulose fluctuated until Day 6. The MWDs reached the maximum on Day 6, indicating the SA formation in the soils with starch or cellulose. The increasing rate of the SA formation in the starch-amended soil was greatly higher than that in the cellulose-amended soil. After Day 6, the MWDs in the soils with either polysaccharide decreased with similar trends with no significant differences between treatments, indicating similar stability of the SA in both treatments. This study showed that the different decomposability of the organic amendments might influence the SA formation differently, but not the SA stability.  相似文献   
95.
Several studies have reported how tillage and cropping systems affect quantity, quality, and distribution of soil organic matter (SOM) along the profile. However, the effect of soil management on the chemical structure of SOM and on its hydrophobic and hydrophilic components has been little investigated. In this work, the long‐term (19 years) effects of two cropping systems (wheat monoculture and wheat/faba bean rotation) and three tillage managements (conventional, reduced, and no tillage) on some chemical characteristics of SOM and their relationships with labile carbon (C) pools were evaluated. Soil samples were taken from the topsoil (0–15 cm) of a Chromic Haploxerert (central Sicily, Italy). After 19 years of different tillage and cropping systems management, total organic C significantly differed among treatments with the labile organic C pools showing the greater amount in no till and in wheat/faba bean plots. Hydrophobic and hydrophilic components of SOM, determined by diffuse reflectance infrared Fourier transform spectroscopy, were mainly affected by cropping system, whereas aromatic components of SOM by tillage. Soil organic matter components and characteristics showed significant correlations with the soil biochemical parameters, confirming the expected synergism between chemical and biochemical properties. This study demonstrated that (i) no tillage and crop rotation improve the chemical and biochemical properties of SOM of Vertisols under semiarid environment; and (ii) tillage management and cropping systems have affected, after 19 years, more the chemical and biochemical properties of SOM than its quantity. Copyright © 2014 John Wiley & Sons, Ltd.  相似文献   
96.
The continuous use of plowing for grain production has been the principal cause of soil degradation. This project was formulated on the hypothesis that the intensification of cropping systems by increasing biomass‐C input and its biodiversity under no‐till (NT) drives soil restoration of degraded agro‐ecosystem. The present study conducted at subtropical [Ponta Grossa (PG) site] and tropical regions [Lucas do Rio Verde, MT (LRV) site] in Brazil aimed to (i) assess the impact of the continuous plow‐based conventional tillage (CT) on soil organic carbon (SOC) stock vis‐à‐vis native vegetation (NV) as baseline; (ii) compare SOC balance among CT, NT cropping systems, and NV; and (iii) evaluate the redistribution of SOC stock in soil profile in relation to soil resilience. The continuous CT decreased the SOC stock by 0·58 and 0·67 Mg C ha−1 y−1 in the 0‐ to 20‐cm depth at the PG and LRV sites, respectively, and the rate of SOC sequestration was 0·59 for the PG site and ranged from 0·48 to 1·30 Mg C ha−1 y−1 for the LRV site. The fraction of C input by crop residues converted into SOC stock was ~14·2% at the PG site and ~20·5% at the LRV site. The SOC resilience index ranged from 0·29 to 0·79, and it increased with the increase in the C input among the NT systems and the SOC sequestration rates at the LRV site. These data support the hypothesis that NT cropping systems with high C input have a large potential to reverse the process of soil degradation and SOC decline. Copyright © 2013 John Wiley & Sons, Ltd.  相似文献   
97.
During the last few decades, land use changes have largely affected the global warming process through emissions of CO2. However, C sequestration in terrestrial ecosystems could contribute to the decrease of atmospheric CO2 rates. Although Mediterranean areas show a high potential for C sequestration, only a few studies have been carried out in these systems. In this study, we propose a methodology to assess the impact of land use and land cover change dynamics on soil organic C stocks at different depths. Soil C sequestration rates are provided for different land cover changes and soil types in Andalusia (southern Spain). Our research is based on the analysis of detailed soil databases containing data from 1357 soil profiles, the Soil Map of Andalusia and the Land Use and Land Cover Map of Andalusia. Land use and land cover changes between 1956 and 2007 implied soil organic C losses in all soil groups, resulting in a total loss of 16·8 Tg (approximately 0·33 Tg y−1). Afforestation increased soil organic C mostly in the topsoil, and forest contributed to sequestration of 8·62 Mg ha−1 of soil organic C (25·4 per cent). Deforestation processes implied important C losses, particularly in Cambisols, Luvisols and Vertisols. The information generated in this study will be a useful basis for designing management strategies for stabilizing the increasing atmospheric CO2 concentrations by preservation of C stocks and C sequestration. Copyright © 2012 John Wiley & Sons, Ltd.  相似文献   
98.
基于目前现有生物质燃烧炉的燃烧效率低,且燃烧过程中焦油生成过多等问题。以高效率燃烧方式的薄层燃烧为该小型生物质直燃炉的主要燃烧方式,大大提高燃烧效率的同时,有效较低焦油与烟尘的产生,并且采用螺杆输送装置对炉膛进行持续供料,实现稳定的不间断燃烧,为成功解决农村生物质燃料浪费及环境污染起到积极作用,为新形势下的能源可持续发展提供思路。  相似文献   
99.
机电产品的包装需要耗费大量的原木,对环境造成了极大的影响,也增加了机电产品的生产经营成本。文章从低碳和成本约束的角度,对机电产品包装概念设计的模型进行了分析和探讨。  相似文献   
100.
6种灌木不同器官生物量及其碳、氮含量的分配特征   总被引:1,自引:0,他引:1  
通过研究晋北地区草地黄刺玫、沙棘、荆条、酸枣、绣线菊和柠条等6种常见灌木的叶片、新生枝、老龄枝生物量及其碳、氮含量的分配特征,旨在为草地准确估算草地植物碳、氮循环提供依据。结果表明:黄刺玫的地上生物量最大,是酸枣的7倍。沙棘叶片生物量占地上生物量的比例最大;黄刺玫新生枝生物量占地上生物量的比例最大;柠条老龄枝生物量占地上生物量的比例最大。黄刺玫、沙棘和荆条的地上部分各器官生物量分配特征相似,由高到低表现为叶片、老龄枝、新生枝;绣线菊、酸枣和柠条的地上部分各器官生物量分配特征相似,由高到低表现为老龄枝、叶片、新生枝。6种灌木地上部分各器官碳含量差异不显著,氮含量分布由高到低为叶片、新生枝、老龄枝。  相似文献   
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