调亏灌溉和氮处理对小桐子生长及水分利用的影响

为了研究阶段水分亏缺(亏水+不亏水W_LW_H、不亏水+亏水W_HW_L、亏水+亏水W_LW_L、不亏水+不亏水W_HW_H)和不同施氮量(N_Z:0,N_L:0.2 g/kg,N_H:0.4 g/kg)对小桐子生长、生理指标和灌溉水利用效率的影响,通过盆栽试验,发现W_LW_H的生长和灌溉水利用效率均显著高于W_HW_L;作物的灌溉水利用效率随施氮量的增大而呈现先增大后减小的趋势,在N_L水平下达到最大值;与高水高氮的处理N_HW_HW_H相比,中水低氮处理N_LW_LW_H节约灌溉水27%,节约氮肥使用量50%,小桐子株高减少31%、总干物质量减少35%,灌溉水利用效率减少13%,但茎粗增加13%,根冠比增加20%.可见小桐子在第一阶段处理(40~90 d)幼树期对水分的需求量较小,适度的亏缺灌溉可提高灌溉水利用效率;小桐子在第二阶段处理(90~140 d)处于旺长期,对水分的需求量较大,增大灌水量可大幅度促进小桐子生长及其干物质量的积累.全生育期实施亏缺灌溉,可提高小桐子自身适应外界环境能力,抗干旱胁迫能力也逐渐增强,但W_LW_L水平下的小桐子生长缓慢.经综合分析,认为处理N_LW_LW_H可作为干旱地区条件下的小桐子灌溉和施氮制度.     

Pulverizing Soils for Laboratory Analysis

Soil-testing laboratories utilize a range of grinder types to pulverize soils for laboratory analysis. This study was conducted to evaluate the effects of soil particle diameter and laboratory subsample size on analysis variability on nitrate, Bray 1 extractable phosphorus (P), extractable potassium (K), and soil organic matter (SOM). Four soils collected for the Agricultural Laboratory Proficiency Program were pulverized using four types of commercial grinders and analyzed for particle-size distribution, P, and K. In a second study, soils were pulverized to pass sieves of 2.0, 1.0, and 0.50 mm and subsampled for P, K, and SOM. Results of the commercial grinders indicate a range in mean particle diameters from 0.15 to 0.60 mm, with the lowest for the grinder utilizing a hammer mill design. Sieve-size analysis results indicate that the coarsest 2.0-mm fraction had the largest variability for all soil analyses evaluated. Analyte variability decreased with decreasing sieve size. Mean Bray P, K, and SOM-LOI (Loss-on-Ignition) mean concentrations were not statistically significantly different across the sieve sizes evaluated. Laboratory analysis variability for extractable Bray P increased as subsample size was reduced.     

八个竹种海涂引种试验报告

本文从土壤含盐量着手对八个竹种在引种成活率、新竹抽发数及其质量、角竹笋产量等方面进行了较系统的研究。结果表明,土壤盐分影响竹子的生长发育,此影响一般随含盐量的增加而增加;不同竹种对土壤盐分的适应能力不同;角竹笋能获得高产,单产达20800kg/ha。参照产地母竹和引种地新竹的生长情况,我们建议:海涂地区发展竹子时可选用角竹、桂竹和红竹。     

平原沙土区不同林分类型下土壤有机碳库特征及其影响因子

目的 明晰不同林分类型下土壤有机碳库特征,以期为平原沙土区土壤碳库的提高和生态恢复提供理论依据。 方法 以江苏省平原沙土区丰县16年生杨树纯林、柳树纯林、杨柳混交林3种林分类型及相邻的撂荒地（对照）为对象,测定0～20、20～40、40～60、60～80、80～100 cm等5个土壤层次有机碳及活性组分和土壤酶活性,计算土壤碳库管理指数,并对土壤有机碳库特征和环境因子进行相关性分析。 结果 （1）3种林分类型及对照各土层有机碳含量和储量范围分别为1.03～5.88 g·kg−1和3.53～17.55 t·hm−2。与对照相比,0～100 cm土层,3种林分类型土壤有机碳含量增加了45.2%～82.2%。杨树纯林0～100 cm土层有机碳储量分别是柳树纯林、杨柳混交林和对照的1.23、1.24、1.83倍。（2）与对照相比,0～100 cm土层,3种林分类型的土壤易氧化有机碳、可溶性有机碳和微生物生物量碳含量分别提高了28.6%～48.0%、6.8%～9.7%和21.6%～33.4%。3种林分类型土壤碳库管理指数显著高于100%（P<0.05）。（3）林分类型显著影响土壤蔗糖酶和多酚氧化酶活性（P<0.05）,杨柳混交林0～100 cm土层多酚氧化酶活性显著高于杨树纯林和对照（P<0.05）。（4）相关性分析表明,土壤有机碳库特征受多酚氧化酶和β-葡萄糖苷酶活性显著影响,有机碳含量和储量、易氧化有机碳含量及碳库管理指数受蔗糖酶、过氧化物酶活性显著影响,微生物生物量碳受蔗糖酶活性显著影响。冗余分析表明,土壤碳氮比和细根生物量是土壤有机碳库特征的主要影响因素。 结论 平原沙土区营造人工林提高了土壤有机碳及活性组分和有机碳库稳定性,杨树纯林提高土壤有机碳储量效果最好。     

夏玉米田作物蒸腾与棵间土壤蒸发模拟计算方法研究

本文依据能量平衡原理和质量守恒定律，提出了作物蒸腾与棵间土壤蒸发的估算模式，并对参数的估算做了详细的分析和讨论。最后利用试验区实测资料，通过田间水热耦合运移的数值模拟，对夏玉米田作物蒸腾棵间土壤蒸发模型及其模拟计算方法进行了验证，结果表明，本文提出的模型和模拟计算方法是有效而实用的。     

Lithic soils in the semi-arid region of Brazil: edaphic characterization and susceptibility to erosion

Soils(Leptosols or Epileptic Regosols)with lithic contact at a depth of 50 cm occupy almost 20%of the Brazilian semi-arid region.These lithic soils are susceptible to erosion due to faster saturation of water-holding capacity during rainfall,which accelerates the beginning of runoff.However,erosion traits of lithic soils in the semi-arid region of Brazil are less studied.The aim of this study was to characterize the soil and landscape attributes in areas with Neossolos Litólicos(Entisols)in the Caatinga biome to identify region of high susceptibility to erosion.Results showed that the soils were characterized by a sandy texture,soil structure with poor development and low content of organic carbon.These attributes increase susceptibility to erosion and reduce water storage capacity,especially in the states of Cearáand Sergipe.In these states,the content of rock fragments in the soil reaches 790 g/kg.High contents of silt and fine sand,high silt/clay ratio,predominance of Leptosols and strong rainfall erosivity were observed in Piauíand northwestern Ceará.A very high degree of water erosion was observed in the states of Pernambuco and Paraíba.Despite the low degree of erosion observed in the state of Bahia,it is highly susceptible to erosion due to the predominance of very shallow soils,rugged relief and high values of rainfall erosivity.Lower vulnerability was observed in the state of Alagoas because of its more smoothed relief,greater effective soil depth,thicker A horizon of soil and lower rainfall erosivity.In general,the characteristics that intensify the susceptibility to erosion in the Caatinga biome are those soil structures with poor development or without aggregation,low contents of organic carbon,high contents of silt and fine sand,high values of silt/clay ratio and rugged relief in some regions.This study collected information contributing to a better characterization of soils with lithic contact in the semi-arid region of Brazil.In addition,regions with a higher susceptibility to erosion were identified,revealing insights that could help develop strategies for environmental risk mitigation.     

耕作与施肥模式对渭北旱塬春玉米田蓄水保墒与玉米产量的影响

为揭示渭北旱塬春玉米田休闲期不同保护性耕作模式的蓄水保墒与增产增收效应,寻找适合渭北旱塬春玉米田水肥高效利用的耕作方式和施肥水平,于2013—2014年度在陕西省合阳县甘井镇春玉米田分别设置传统农户模式(翻耕+低肥,S1)、现有高效模式(免耕+高肥,S2)、创新高效模式(深松+平衡施肥,S3)等模式处理,研究各类耕作与施肥相结合保护性耕作模式下春玉米水分利用率、产量和经济效益差异。结果表明,创新模式S3和现有模式S2较农户模式S1播前增加了土壤贮水量;创新模式S3和现有模式S2处理在玉米主要生育期0~200 cm土层平均土壤贮水量分别比农户模式S1增加23.3 mm和18.1 mm,水分利用效率分别提高12.3%和10%,产量增加11.1%、9.2%。创新模式和现有模式均较农户模式能够增加土壤贮水量,提高水分利用效率,增加产量和经济效益,但创新模式蓄水保墒,增产增收优势明显,是适合渭北旱塬地区春玉米生产的水肥管理模式。     

原料表面碱液处理对稻草碎料板力学性能的影响

在实验室条件下探索了稻草原料表面碱液处理对稻草碎料板力学性能的影响.试验表明,处理后的稻草碎料板的内结合强度比处理前有大幅度提高,弯曲弹性模量和静曲强度比处理前则有所下降,但都达到了相关的国家标准;2h吸水厚度膨胀率升高,超过国家标准.因此稻草表面碱液处理提高了稻草原料表面润湿性和胶合强度,但对稻草碎料板的力学性能有影响.     

辽宁营口沿海产业基地民兴河盐碱土对3种引进草种耐盐性的影响

为了确定辽宁省营口沿海产业基地民兴河盐碱地特性,筛选适宜草种,进行盐碱地综合开发和利用.分析测定该地区不同季节不同土层各离子含量,配制土壤盐溶液,测定3种引进草种(NHC牧草、RWW麦草、WAFG 硷草)在不同盐浓度处理下的生理指标.结果显示:该地区土壤含盐量随季节和土层变化而变化,0～60 cm土层,春季含盐量1.42%～1.11%,夏季含盐量1.32%～0.62%.土壤Na 、Cl-与盐度相关系数分别为0.984、0.950,该地区土壤为NaCl型盐土.不同盐处理下, NHC牧草发芽率、种子α-淀粉酶活性、可溶性糖含量、鲜重、成活率均显著高于其他2种试材.NHC牧草萌发的临介土壤盐浓度为200 mmol/L,发芽率为75%,30 d成活率为57%.