The establishment of Taraxacum officinale plants in grassland

Factors involved in the establishment of Taraxacum officinale (dandelion) seedlings in grasslands and plant mortality in the first growing season were studied during 2008–2011. The study was conducted at 11 grassland sites that differed in the quantity of seed rain and the intensity of seedling predation by slugs. In April, of each study year, 10 plots open to the sedimentation of naturally dispersed seeds were established at each site, five plots of which were also sown with 250 T. officinale seeds each. The amount of natural seed rain, slug feeding activity and number of plants in each plot were then recorded at monthly intervals. Seed rain and seedling predation accounted for c. 50% of the variation in seedling establishment. Populations of established seedlings then declined through October, at which point they were at 25% of the original abundance on average. The percentage of plants that survived varied among sites and years. The temporal and spatial variation in T. officinale establishment and survival of young plants was enormous, even within a small area. Predation of seedlings by slugs can effectively prevent the establishment of T. officinale in grassland. This only occurred, however, at slug abundances not acceptable under conditions of public access.     

不同作物类型下蒸散发时间尺度扩展方法对比

该文的目的是评价由瞬时潜热通量经过时间尺度扩展方法计算日蒸散发量的可靠性。为此,采用蒸发比法、改进的蒸发比法、正弦关系法及作物系数法等4种常用的蒸散发时间尺度扩展方法,针对位于华北平原的高营站和位于东北平原的通榆站的5种典型下垫面类型,分别对瞬时潜热通量进行时间尺度扩展,估算日蒸散发量,并与通量站采用涡度相关系统观测的日蒸散发量进行对比。结果表明,尽管4种方法在总体上具有一致性,但改进的蒸发比法的模拟精度最高（相对均方根误差20%左右）,更适合于估算中国北方典型农田的日蒸散发量。然而,4种方法均存在系统误差,从而导致采用上午时段瞬时通量估算的日蒸散发量系统偏小,而采用下午时段估算的日蒸散发量系统偏大。     

居民收入差距对我国经济发展的影响

我国城乡之间、行业之间、区域之间、城镇（或农村）内部的收入差距不断扩大,影响了经济发展。可通过拓宽就业渠道,保障教育公平,深化收入分配制度改革等来缩小收入差距,促进经济发展。     

亚高山针叶林冠下缺苞箭竹的克隆生长

以王朗国家级保护区亚高山针叶林下的缺苞箭竹(Fargesia denudata)为研究对象,比较研究了不同林冠环境下克隆生长特征,及4种林冠环境下克隆繁殖的大小依赖关系.研究结果表明:林冠环境的差异导致了分株平均生物量、基径、高度以及当年生立竹分株密度的显著差异,但对整个无性系种群的分株密度没有影响,缺苞箭竹对不同林冠环境的响应主要体现在分株质量上;间隔子的生物量、直径、分枝强度和比间隔子长等克隆生长特征在各个林冠环境中存在显著差异,间隔子长度只在大林窗环境中显著低于其他林冠环境;缺苞箭竹在4种林冠环境下均表现出克隆繁殖的大小依赖关系,母株大小通过间隔子的作用,对当年生立竹大小有显著影响.缺苞箭竹的克隆生长受到不同林冠环境的影响,在其适宜生境(中等林窗)内种群通过提高分株质量以增强整个种群的生命力,同时克隆生长受到自身母株的制约,林冠环境通过影响母株的质量从而影响克隆繁殖分株.     

不同类型有机物料的有机磷组成及生物有效性

[目的]研究不同有机物料的有机磷组成及其作为磷源施用后的供磷能力,为化肥磷的有机替代奠定理论基础.[方法]供试有机物料包括粪肥类(猪粪、羊粪)、绿肥类(豌豆、苜蓿和绿豆)、秸秆类(小麦秸秆、玉米秸秆和油菜秸秆).分析了8种有机物料的全磷、有机磷含量和C/P值,采用Bowman-Cole方法测定了有机磷中的活性(LOP)...     

椭圆嗜蓝层孔菌子实体化学成分研究

椭圆嗜蓝层孔菌(Phellinus ellipsoidea)子实体甲醇提取物依次用石油醚和乙酸乙酯萃取,其乙酸乙酯分部经柱层析分离得到11个化合物。经鉴定这11个化合物分别为:苯并(1,2-b,5,4-b′)二呋喃-3,5-二酮-8-甲酸甲酯(1)、原儿茶酸(2)、4-(3,4-二羟苯基)-3-丁烯-2-酮(3)、原儿茶醛(4)、Hispidin(5)、Hispolon(6)、Inoscavin A(7)、Phelligridin K(8)、Inoscavin C(9)、Inoscavin E(10)和Inonoblins B(11),其中化合物2、4、7、10为首次从该物种中分离得到。     

细叶旱芹地上部化感物质粗分离物对4种草坪草及5种牧草的化感作用

采用滤纸培养皿法,以发芽率、发芽势、根长和苗长为指标,研究细叶旱芹(Cyclospermum leptophyllum(Pers.) Sprague ex Britton et P. Wilson)地上部化感物质对4种草坪草和5种牧草受体植物的种子萌发和幼苗生长的影响。结果表明,细叶旱芹地上部化感物质对4种草坪草和5种牧草的种子萌发和幼苗生长均有抑制作用,其中对种子发芽势抑制最明显,抑制率最高达96.3%;其次是对幼苗根长的抑制作用,抑制率最高达91.1%。通过比较种子萌发和幼苗生长的测定指标,得出5种馏分对草坪草的化感作用为石油醚相>氯仿相>正丁醇相>乙酸乙酯相>水相,而对牧草的化感作用为石油醚相>乙酸乙酯相>氯仿相>正丁醇相>水相。说明不同受体植物对相同萃取相组分的化感作用强弱存在差异,细叶旱芹地上部化感物质主要存在于石油醚馏分中,可进一步从中分离提取活性物质。     

三峡库区消落带湿地土壤有机碳及其组分特征

湿地生态系统土壤有机碳库的组分变化对于全球碳平衡起着极其重要的作用。本研究选取三峡库区消落带湿地3个海拔梯度的土壤,以从未淹没的样地作为对照,研究消落带湿地不同海拔梯度土壤有机碳组分的特征。结果表明:土壤有机碳、易氧化有机碳、水溶性碳水化合物有机碳和和微生物生物量碳均以消落带小于未淹没样地。在消落带,海拔最低、淹没持续时间较长且正处于水位波动期的样地土壤有机碳、易氧化碳和微生物生物量碳显著低于其他样地,而土壤矿化碳显著高于其他样地。相关性分析表明,土壤有机碳与微生物生物量碳(R~2=0.94)的正相关性显著高于与易氧化有机碳(R~2=0.88)、水溶性有机碳(R~2=0.73)及其水溶性碳水化合物(R~2=0.70)之间的正相关性,但是与矿化碳之间无显著的相关性。因此,土壤微生物生物量碳是消落带湿地土壤有机碳随不同海拔梯度变化的最敏感的组分。     

Cation exchange capacity of density fractions from paired conifer/grassland soils

The cation exchange capacity (CEC) of a soil depends on the type and amount of both mineral and organic surfaces. Previous studies that have sought to determine the relative contribution of organic matter to total soil CEC have not addressed differences in soil organic matter (SOM) composition that could lead to differences in CEC. The objectives of this study were (1) to compare the CEC of two distinct SOM pools, the “light fraction (LF)” composed of particulate plant, animal, and microbial debris, and the “heavy fraction (HF)” composed of mineral-bound organic matter; and (2) to examine the effects of differences in aboveground vegetation on CEC. Soil samples were collected from four paired grassland/conifer sites within a single forested area and density fractionated. LF CEC was higher in conifer soils than in grassland soils, but there was no evidence of an effect of vegetation on CEC for the HF or bulk soil. LF CEC (but not HF CEC) correlated well with the C concentration in the fraction. The mean CEC of both fractions (per kg fraction) exceeded that of the bulk soil; thus, when the LF and HF CEC were combined mathematically by weighting values for each fraction in proportion to dry mass, the resulting value was nearly twice the measured CEC of bulk soil. On a whole soil basis, the HF contributed on average 97% of the CEC of the whole soil, although this conclusion must be tempered given the inflation of CEC values by the density fractionation procedure.     

CO2 emission in an intensively cultivated loam as affected by long-term application of organic manure and nitrogen fertilizer

A long-term field experiment was conducted to examine the influence of mineral fertilizer and organic manure on the equilibrium dynamics of soil organic C in an intensively cultivated fluvo-aquic soil in the Fengqiu State Key Agro-Ecological Experimental Station (Fengqiu county, Henan province, China) since September 1989. Soil CO₂ flux was measured during the maize and wheat growing seasons in 2002-2003 and 2004 to evaluate the response of soil respiration to additions and/or alterations in mineral fertilizer, organic manure and various environmental factors. The study included seven treatments: organic manure (OM), half-organic manure plus half-fertilizer N (NOM), fertilizer NPK (NPK), fertilizer NP (NP), fertilizer NK (NK), fertilizer PK (PK) and control (CK). Organic C in soil and the soil heavy fraction (organo-mineral complex) was increased from 4.47 to 8.61 mg C g⁻¹ and from 3.32 to 5.68 mg C g⁻¹, respectively, after the 13 yr application of organic manure. In contrast, organic C and the soil heavy fraction increased in NPK soil to only 5.41 and 4.38 mg C g⁻¹, respectively. In the CK treatment, these parameters actually decreased from the initial C concentrations (4.47 and 3.32 mg C g⁻¹) to 3.77 and 3.11 mg C g⁻¹, respectively. Therefore, organic manure efficiently elevated soil organic C. However, only 66% of the increased soil organic C was combined with clay minerals in the OM treatment. Cumulative soil CO₂ emissions from inter-row soil in the OM and NPK treatments were 228 and 188 g C m⁻² during the 2002 maize growing season, 132 and 123 g C m⁻² during the 2002/2003 wheat growing season, and 401 and 346 g C m⁻² yr⁻¹ in 2002-2003, respectively. However, during the 2004 maize growing season, cumulative soil CO₂ emissions were as high as 617 and 556 g C m⁻², respectively, due to the contribution of rhizosphere respiration. The addition of organic manure contributed to a 16% increase in soil CO₂ emission in 2002-2003 (compared to NPK), where only 27%, 36% and 24% of applied organic C was released as CO₂ during the 2002 and 2004 maize growing seasons and in 2002-2003, respectively. During the 2002/2003 wheat growing season, soil CO₂ flux was significantly affected by soil temperature below 20 °C, but by soil moisture (WFPS) during the 2004 maize growing season at soil temperatures above 18 °C. Optimum soil WFPS for soil CO₂ flux was approximately 70%. When WFPS was below 50%, it no longer had a significant impact on soil CO₂ flux during the 2002 maize growing season. This study indicates the application of organic manure composted with wheat straw may be a preferred strategy for increasing soil organic C and sequestering C in soil.