保水缓释肥料保水性能及养分释放特性

为了明确添加水溶性保水剂(羧甲基纤维素钠、聚丙烯酰胺、聚丙烯酸钠)肥料的保水缓释效果,利用圆盘造粒工艺制备了保水缓释肥料,通过土壤培养和土柱淋溶试验,研究了保水缓释肥料在土壤中的保水性能和养分缓释效果。结果表明:3种保水缓释肥料均具有一定保水性和养分缓释效果,随保水缓释肥料用量增加,土壤最大持水率逐渐增加,土壤水分蒸发率逐渐减小;其中,以添加聚丙烯酸钠的保水缓释肥料保水性能和养分缓释效果最佳,首次淋溶后氮磷钾养分释放率较普通肥料分别减少了50.38%、55.74%、48.37%,当肥料添加量为2%时,土壤最大持水率较纯土壤提高了43.28%,培养至30 d土壤水分蒸发率较纯土壤降低了22.86%。     

五指山耕地土壤养分现状调查与评价

为了明确海南山区耕地土壤养分空间分布特征，为热带山区耕地土壤养分管理提供思路。以海南五指山市耕地为研究对象，采用野外调查、采样和室内分析相结合的方法，阐述土壤养分现状，探讨其土壤养分分布规律。结果表明：五指山耕地土壤总体呈酸性，其pH值为5.1；土壤有机质、有效磷、速效钾和中量元素(钙、镁、硫)含量均为中等或偏下水平，土壤有效铜和有效锌含量较为丰富。五指山耕地土壤酸化和养分含量分布不均主要与气候、母质分布和施肥不平衡有关。     

Effect of the addition of Chaetoceros calcitrans,Navicula sp. and Phaeodactylum tricornutum (diatoms) on phytoplankton composition and growth of Litopenaeus vannamei (Boone) postlarvae reared in a biofloc system

The aim of this study was to evaluate the effect of the addition of Chaetoceros calcitrans, Navicula sp. and Phaeodactylum tricornutum (diatoms) on phytoplankton composition and the growth of Litopenaeus vannamei postlarvae reared in a biofloc system . Four treatments were used: BFT (biofloc system without feed and no addition of diatoms); BFT‐F (biofloc system with feed and no addition of diatoms); BFT‐D (biofloc system with the addition of diatoms and no feed); and BFT‐FD (biofloc system with the addition of feed and diatoms), all in triplicate. The shrimp (16 ± 0.02 mg) were stocked at 2500 postlarvae m^?3 and fed a commercial feed. Diatoms were added on the 1st, 5th, 10th and 15th day at a density of 5 × 10⁴ cells mL^?1 for each species. No significant differences (P > 0.05) between treatments were observed for gross primary production, net ecosystem production and water column respiration rate. However, significant differences (P < 0.05) were observed for nitrite, orthophosphate, alkalinity, final weight, weight gain, yield, feed conversion ratio (FCR), phytoplankton and cyanobacteria composition. The BFT‐FD treatment had better performance parameters for final weight (270 mg), weight gain (254 mg), yield (0.67 Kg m^?3) and FCR (0.61), indicating the benefits of the diatoms C. calcitrans, Navicula sp. and P. tricornutum for decreasing cyanobacteria and improving growth of L. vannamei postlarvae reared in biofloc systems.     

氢氧化镁对水质、底质改良的研究与应用

近年,沿海各地区水产养殖业发展迅速。由于内湾海区海水循环交换能力较弱,黑臭底泥的长期堆积,导致养殖水体水质和底质进一步恶化,然而这种问题普遍存在于封闭式或半封闭式水域环境中。对此,氢氧化镁作为水质、底质改良剂被应用于水环境的治理。本文概述了氢氧化镁的作用机理,包括氢氧化镁与悬浮颗粒物的静电、对氮磷的降解及对硫化氢的降解等作用;同时介绍了氢氧化镁在海水养殖场、淡水湖泊和水库、水华防控、赤潮防控及废水处理中的研究与应用;展望了氢氧化镁和纳米级氢氧化镁在水体环境领域的应用前景。     

外源溶磷菌对不同土壤条件下大豆生长特性的影响

为了明确溶磷菌在多种土壤中的应用效果,探讨了两株溶磷菌对黑土及盐碱土种植大豆的促生效应。采用盆栽试验分析了不同处理对大豆光合作用、渗透调节物质含量、生物量、氮磷吸收及产量的影响。结果表明:加菌处理可增加植株Pn,显著降低R6、R8两时期叶片可溶性蛋白、可溶性糖及游离氨基酸含量,增加R2~R8时期大豆株高和根干重,混合土壤中加菌处理也可提高植株地上部分氮、磷及植株全磷、全氮含量。添加wj1和混合菌处理的植株干重优于添加wj3的处理。黑土加混合菌可显著提高大豆R2期叶片WUE,增加V3、R2和R8这3个时期大豆地上、地下部分氮、磷及植株全氮、全磷的含量。黑土加wj1与混合土壤加菌处理的大豆株荚数、总粒数、单株粒重及百粒重均高于未加菌处理。添加外源溶磷菌,对黑土及盐碱土栽培大豆均有不同程度的促生效果,能明显增强大豆在混合盐碱土壤中的适应性,增加植株生物量、氮磷吸收量和产量,且混合菌处理对大豆的促生效应优于wj1及wj3单一菌株处理。     

黔东南州天柱县植烟土壤保育与改良研究

植烟土壤是确保烤烟优质高产的关键因素之一,通过对天柱县植烟土壤烟田基本情况、土壤退化情况、土壤保育与改良情况、土地整理情况等进行调查,结果表明:该烟区地块比较破碎,有便利的排水条件或健全的排水设施,无洪涝灾害的烟田面积为420.00 hm~2,占63.0%;土壤板结发生面积为136.00 hm~2,占基本烟田的20.4%;有机质含量下降发生面积为208 hm~2,占基本烟田的31.2%;水土流失发生面积为169.33 hm~2,占基本烟田的25.4%。为此,应采取土壤改良措施,以促进天柱特色优质烤烟的发展。     

土壤有机碳对沼渣或牛粪施用后温室气体排放潜力的影响—盆栽试验结果

A change in the European Union energy policy has markedly promoted the expansion of biogas production.Consequently,large amounts of nutrient-rich residues are being used as organic fertilizers.In this study,a pot experiment was conducted to simulate the high-risk situation of enhanced greenhouse gas (GHG) emissions following organic fertilizer application in energy maize cultivation.We hypothesized that cattle slurry application enhanced CO2 and N2O fluxes compared to biogas digestate because of the overall higher carbon (C) and nitrogen (N) input,and that higher levels of CO2 and N2O emissions could be expected by increasing soil organic C (SOC) and N contents.Biogas digestate and cattle slurry,at a rate of 150 kg NH4+-N ha-1,were incorporated into 3 soil types with low,medium,and high SOC contents (Cambisol,Mollic Gleysol,and Sapric Histosol,termed Clow,Cmedium,and Chigh,respectively).The GHG exchange (CO2,CH4,and N2O) was measured on 5 replicates over a period of 22 d using the closed chamber technique.The application of cattle slurry resulted in significantly higher CO2 and N2O fluxes compared to the application of biogas digestate.No differences were observed in CH4 exchange,which was close to zero for all treatments.Significantly higher CO2 emissions were observed in Chigh compared to the other two soil types,whereas the highest N2O emissions were observed in Cmedium.Thus,the results demonstrate the importance of soil type-adapted fertilization with respect to changing soil physical and environmental conditions.     

Soil water response to precipitation in different microtopographies on the semi-arid Loess Plateau,China

Soil water is an important factor restricting afforestation on the semi-arid Loess Plateau.The microtopography of the loess slope has changed the distribution pattern of soil water on the slope.To improve water utilization efficiency and optimize afforestation configuration patterns,the relationship between soil water and precipitation at micro-topographic scale must be studied.We used time series analysis to study the temporal variation of soil water and its response to precipitation in four kinds of micro-topographies and undisturbed slope on loess slopes.Micro-topographies significantly influenced soil water distribution and dynamics on the slopes.Soil water stored in the platform,sinkhole,and ephemeral gully influenced subsequent soil water for 4 weeks,whereas soil water stored in the scarp and undisturbed slope could influence soil water for 2 weeks.It took 12 weeks,10 weeks,18 weeks,6 weeks,and 12 weeks for precipitation to reach the deeper soil layer in the platform,sinkhole,scarp,ephemeral gully,and undisturbed slope,respectively.These soil water characteristics in different micro-topographies are vital factors that should be taken into consideration when undertaking afforestation on the Loess Plateau.     

开垦年限对黑土氮初级转化速率和净转化速率的影响

以东北黑土区开垦2 a和开垦30 a的典型旱作土壤为研究对象,采用15N同位素成对标记技术开展室内培养试验,利用数值计算模型(FLUAZ)计算不同开垦年限土壤的氮初级转化速率,以比较不同开垦年限黑土氮初级转化速率和净转化速率的差异,明确开垦年限对黑土氮转化过程的影响。结果表明,与开垦2a土壤相比,开垦30a土壤的有机碳和水溶性有机碳含量显著降低,导致土壤氮初级矿化速率和初级固定速率也显著降低。但开垦30a土壤的初级硝化速率、净硝化速率和净氮矿化速率却显著高于开垦2a土壤。两个开垦年限土壤的初级硝化速率分别为净硝化速率的1.15倍和1.02倍,说明土壤微生物对硝态氮的固定很少。开垦30a土壤的m/i值(氮初级矿化速率与初级固定速率之比)和n/ia值(初级硝化速率与初级铵态氮固定速率之比)均显著大于1,而开垦2 a土壤的m/i值和n/ia值均接近1。表明开垦2 a土壤的氮矿化与固定过程紧密偶联,氮素损失的风险较小,而开垦30 a土壤中氮矿化量超过了固定量,这为硝化作用的进行提供了底物,增加了硝酸盐反硝化和淋溶风险。     

森林土壤动物生态功能研究进展

森林土壤动物是森林土壤生态系统中不可分割的重要组成部分，对森林土壤生态系统的物质循环和能量流动起着重要作用。文中综述了近10年森林土壤动物生态功能的相关研究进展，包括森林土壤动物对土壤理化性质、微生物、植物的影响以及外来土壤动物入侵对土壤生态系统的影响等；展望了我国森林土壤动物的未来研究方向，未来研究应多关注森林土壤动物生态功能的作用机制、森林土壤动物对全球变化的响应、外来土壤动物入侵对森林生态系统的影响、森林土壤动物种类的研究范围以及新技术的应用，以期为我国森林土壤动物生态功能、土壤动物与生态系统、可持续利用土壤动物等领域研究提供科学参考。