运材汽车后桥的使用与修理

介绍了运材汽车后桥的使用和修理方法,对提高运材汽车的使用寿命具有一定的参考价值。     

Recovery of saturated hydraulic conductivity under secondary succession on former pasture in the humid tropics

Landscapes in the humid tropics are undergoing a continuous change in land use. Deforestation is still taking its toll on forested areas, but at the same time more and more secondary forests emerge where formerly agricultural lands and pastures are being abandoned. Regarding soil hydrology, the extent to which secondary succession can recover soil hydrological properties disturbed by antecedent deforestation and pasture use is yet poorly understood. We investigated the effect of secondary succession on saturated hydraulic conductivity (Ks) at two soil depths (0-6 and 6-12 cm) using a space-for-time approach in a landscape mosaic in central Panama. The following four land-use classes were studied: pasture (P), secondary forest of 5-8 years of age (SF5), secondary forest of 12-15 years of age (SF12) and secondary forest of more than 100 years of age (SF100), each replicated altogether four times in different micro-catchments across the study region. The hydrological implications of differences in Ks in response to land-use change with land use, especially regarding overland flow generation, were assessed via comparisons with rainfall intensities.Recovery of Ks could be detected in the 0-6 cm depth after 12 years of secondary succession: P and SF5 held similar Ks values, but differed significantly (α = 0.05) from SF12 and SF100 which in turn were indistinguishable. Variability within the land cover classes was large but, due to sufficient replication in the study, Ks recovery could be detected nonetheless. Ks in the 6-12 cm depth did not show any differences between the land cover classes; only Ks of the uppermost soil layer was affected by land-use changes. Overland flow - as inferred from comparisons of Ks with rainfall intensities - is more likely on P and SF5 sites compared to SF12 and SF100 for the upper sample depth; however, generally low values at the 6-12 cm depth are likely to impede vertical percolation during high rainfall intensities regardless of land use.We conclude that Ks can recover from pasture use under secondary succession up to pre-pasture levels, but the process may take more than 8 years. In order to gain comprehensive understanding of Ks change with land use and its hydrological implications, more studies with detailed land-use histories and combined measurements of Ks, overland flow, precipitation and throughfall are essential.     

Sitka spruce site index in response to varying soil moisture and nutrients in three different climate regions in Ireland

We examined the relationships between Sitka spruce (Picea sitchensis (Bong.) Carr.) site index, windspeed, former land use, soil moisture and soil nutrients with a view to identifying factors limiting the growth potential of the species in three climate regions in Ireland. We selected plantations covering three climate regions (delineated on the basis of ‘growing season’ balance of precipitation and potential evapotranspiration; representing dry, moist and wet climate regions) located on sites representing the range of soil moisture regimes (SMR), soil nutrient regimes (SNR), and land use types found throughout Ireland. Site index of Sitka spruce varied among climate region, with significantly lower site index associated with the wet climate region mainly due to the deterioration in edaphic conditions and adverse climatic conditions. The effect of edaphic variables (SMR, SNR) on site index was consistent across climate regions, site index increasing with increasing SNR, and decreasing with excess moisture or moisture deficit. Site index reached a maximum on fresh/very rich sites in the dry and moist climate regions and on moist/rich sites in the wet climate region. In the dry climate region, water supply (SMR) was the most important variable regulating growth, in wetter windier climates nutrient supply (SNR) was the most important factor, accounting for 69% of the variation in site index. The study has allowed region-specific recommendations to be made for successful plantation establishment in Ireland and for countries with similar climatic regions.     

Coast live oak, Quercus agrifolia, susceptibility and response to goldspotted oak borer, Agrilus auroguttatus, injury in southern California

Oak mortality is often associated with a complex of decline factors. We describe the morphological and physiological responses of coast live oak, Quercus agrifolia Née, in California to an invasive insect, the goldspotted oak borer (GSOB), Agrilus auroguttatus Schaeffer (Coleoptera: Buprestidae), and evaluate drought as a potential inciting factor. Morphological traits of 356 trees were assessed and physiological traits of 70 of these were monitored intensively over one growing season. Morphological characteristics of tree health included crown thinning and dieback; bole staining resulting from larval feeding; density of GSOB adult exit holes; and holes caused by woodpecker feeding. These characteristics were used to rank GSOB infestation/injury into four classes, and taken together, they explained 87% of the variation in a principal component analysis. Drought stress on various size/age and infestation classes of Q. agrifolia was measured by assessing branchlet pre-dawn and solar noon xylem water potential, leaf cell turgor potential, and water use efficiency over one growing season. Both morphological and physiological traits were highly variable in mature and old growth trees. Early summer plant water status (branchlet xylem water potential and water use efficiency) was similar between uninfested and newly colonized trees, suggesting that GSOB are not pre-selecting drought-stressed Q. agrifolia for oviposition. By late summer, leaf water and cell turgor potentials were lower in infested than in uninfested mature trees, suggesting that GSOB infestation causes drought stress in these trees. Among the tree size/age classes, infested old growth trees exhibited the greatest change in water use efficiency over the growing season, and showed greater morphological injury symptoms of decline than infested mature trees. Morphological attributes of decline in Q. agrifolia associated with GSOB were correlated weakly with increasing physiological drought stress among infestation classes of trees. We propose that the collection of morphological responses of Q. agrifolia to GSOB described here can be used to monitor the future expansion of the GSOB distribution as well as the GSOB-induced decline of Q. agrifolia in California.     

信宜市土地利用景观格局研究

以广东省信宜市为研究区,利用patch analyst景观格局分析软件,选取斑块数目、斑块面积、斑块密度、平均斑块大小、斑块面积标准差、斑块面积变异系数、平均斑块形状指数、面积加权平均斑块形状指数、平均斑块分维数、面积加权平均斑块分维数、破碎度、均匀度和多样性指数等指标,对信宜市土地利用景观格局进行分析.结果表明:各类...     

不同利用方式红壤反硝化势和气态产物排放特征

采用厌氧培养-乙炔抑制法测定了4种不同利用方式红壤的反硝化势和气态产物N₂O和N₂的排放速率。结果表明，不同利用方式红壤反硝化势和N₂O和N₂的排放速率差异明显，土壤反硝化势强弱顺序依次为：竹林>茶园>林地>旱地。反硝化势与土壤有机碳(P<0.05)、厌氧培养期间土壤CO₂累积排放量(P<0.01)、nirS基因丰度( P<0.05)和nirK基因丰度(P<0.05) 呈显著正相关关系。逐步回归分析结果表明，CO₂累积排放量表征的易矿化碳是造成不同利用方式红壤反硝化势差异的主要原因，可以解释反硝化势变化的66%(P<0.01)。不同利用方式红壤N₂O和N₂排放速率差异明显，旱地红壤N₂O和N₂排放速率均最低，表明土壤pH的提升并没有增加旱地红壤的反硝化损失风险和N₂O排放速率。土壤易矿化有机碳含量也是影响不同利用方式红壤N₂O和N₂排放速率的主要因素。反硝化功能基因nirS、nirK和nosZ的丰度均与CO₂累积排放量呈显著正相关关系，进一步支持了土壤易矿化有机碳含量是影响不同利用方式红壤反硝化势和气态产物排放的主要因子。土壤pH是影响不同利用方式红壤反硝化气态产物N₂/N₂O的主要因素，但是pH影响红壤N₂/N₂O的微生物机制仍需要进一步研究。     

陕北"一户一田"和"一组一田"耕地细碎化整治模式与绩效评价

耕地细碎化是当前制约中国农业现代化发展的重要因素,如何解决耕地细碎化问题已经成为推动小农户和现代农业有机衔接的必然路径。该研究基于实地农户调研数据和半结构访谈内容,对陕北榆林市榆阳区首创的"一户一田"和"一组一田"2种耕地细碎化整治模式进行系统剖析,并采用双重差分(Difference-in-difference, DID)模型定量分析2种模式的绩效差异。研究发现:1)"一户一田"模式是农民自发的产权重组和分散流转,并与政府支持的土地整治项目叠加与综合;"一组一田"模式是一种"以家庭承包经营为基础、统分收放自如的双层经营体制"创新模式,也是产权改革、统分流转、土地整治与统分经营管理的有机结合。2)"一户一田"和"一组一田"两种模式均能有效解决耕地细碎化问题,显著增加耕地面积,实施后耕地面积增加率分别为6.02%和57.58%;同时也使得农业机械化水平有所提高,显著提升农业生产效率与作物产量,作物产量增加率分别为12.54%和19.87%,"一组一田"提升更为明显。3)2种模式均有利于提高农户收入,"一户一田"主要是通过增加农业种植收入来提高总收入;"一组一田"对农户收入提升更加显著,除增加农业收入外,也通过产业转型增加了务工收入。与"一户一田"模式相比,"一组一田"模式更能够促进集中连片、规模扩大、设施完善、经营现代化的高标准农田建设。为解决耕地细碎化问题,应加强政策引导和支持,挖掘村内能人价值,明晰合作社、分社和农民的责、权、利关系等,促进小农户和现代农业发展有机衔接。     

滴灌条件下冬小麦施氮增产的光合生理响应

小麦籽粒产量与抽穗期之后的旗叶光合能力密切相关。为明确冬小麦施氮增产的光合生理响应,该文以充分滴灌不同N追肥量处理的冬小麦田为研究对象,抽穗期后进行3次旗叶光合-光响应曲线测定,量化并比较了旗叶光合能力(Amax)和表观光量子羧化效率(α)等参数及产量(Y)和水分利用效率(WUEa),并确定了旗叶比叶重(SLA)、N含量(N-mass和N-area)和13C同位素甄别率(Δ)对光合参数及产量的影响。分析表明:充分滴灌条件下,增施N肥能延长旗叶光合功能持续期,提高Amax和α,以高N处理(N3,207kg/hm2)处理最为显著(P=0.046),在生育中后期仍能保持较高的Amax,这也是N3处理Y较高的主要原因。而N肥对农田耗水影响不显著,高N处理的WUEa也较高。Amax的提高和维持与旗叶SLA、N-mass、N-area和Δ的变化有关,N肥处理也显著影响了Amax与SLA、N-mass、N-area和Δ之间的线性相关关系。该结果从光合生理角度阐明了冬小麦施氮增产的生理因素,可为该地区冬小麦滴灌施肥管理提供参考。     

中国中东部农田作物水分利用效率时空分布及影响因子分析

为研究中国中东部地区农田生态系统水分利用效率时空分布特征,该文利用遥感数据、气象数据以及国家分省区农业统计数据,基于农作物种植结构所划分的地区,通过趋势分析方法,分析了2003-2012年10 a间农田水分利用效率的时空分布特征。结果发现:华北地区农田多年平均水分利用效率(water use efficiency,WUE)高于南方水田区,山东半岛、辽东半岛以及江苏沿海地区农田WUE最高,多年农田WUE均值高达2.0 g/kg,而东北平原及东南丘陵地区农田WUE多年均值则较低,平均在1.5 g/kg以下。中国中东部农田WUE总体上呈上升趋势。其中,华北平原以及松嫩平原农田WUE增加趋势明显,最大年均增幅达0.02 g/(kg·a),而东南丘陵、江淮以及三江平原等地,农田WUE则呈减小趋势,最大年均降幅达-0.007 g/(kg·a)。整体上看,北方地区农田WUE的涨幅高于南方。考虑气候变化后,灌溉和施肥对中国中东部农田WUE的影响较小。气候变化则是影响中东部农田WUE的主要因素。在北方地区,对农田WUE变化有显著影响的因子为年降水量,而在南方地区,年均温的影响则更显著。相比于在中东部北方地区农田WUE年际变化主要受到年降水量对农田蒸散发(evapotranspiration,ET)的影响,在南方地区,农田WUE年际变化则主要受到年均温对农作物总初级生产力(gross primary productivity,GPP)的影响。该研究可为农田区水资源合理利用以及中东部农田生态环境持续发展提供参考。     

早稻施氮对连作晚稻产量和氮肥利用率及土壤有效氮含量的影响

于20022～005年,在湖南长沙采用连续定位试验,研究了早稻施氮对连作晚稻产量、氮肥利用率、土壤有效氮含量的影响。试验设早稻施氮/晚稻不施氮、早稻施氮/晚稻施氮、早稻不施氮/晚稻不施氮、早稻不施氮/晚稻施氮4个处理。结果表明,在连续4年早季施氮的条件下,连作晚稻施氮处理的平均产量为6.45.t/hm2,地上部干物质重12.13.t/hm2,氮素吸收量183.6.kg/hm2,分别比连作晚稻不施氮处理增加28.4%、35.1%和103.5%,均达到显著水平;在连续4年早季不施氮的条件下,连作晚稻施氮处理的平均产量为6.61.t/hm2,地上部干物质重12.14.t/hm2,氮素吸收量165.6.kg/hm2,分别比不施氮处理增加33.4%、37.6%和95.6%,均亦达到显著水平。连作晚稻在早季不施氮和早季施氮两种情况下氮肥利用率不同,前者的氮肥生理利用率显著高于后者,增幅为37.8%,两者的氮肥农学利用效率、吸收利用率差异不显著,但前者4年氮肥农学利用效率平均值比后者高18.1%,吸收利用率低6.8个百分点。早晚两季均不施氮小区土壤碱解氮含量均明显低于其他施氮小区,但没有出现随试验年度加长而连续下降的趋势;当早稻或晚稻其中有一季施用了氮肥,或者两季均施用了氮肥的小区,土壤碱解氮含量差异不显著。说明连作晚稻产量主要受当季施氮量的影响,而受早季施氮量的影响较小;早季不施氮小区的连作晚稻氮肥的农学利用效率、生理利用率比早季施氮小区高;在一定程度上降低稻田氮肥用量不会导致土壤背景氮含量的下降。