石灰联合碳铵熏蒸对连作香蕉生长和根际微生物群落结构的影响

摘 要：由于长期连作导致香蕉枯萎病大量爆发，造成香蕉种植面积锐减，已严重影响海南香蕉产业的发展，因而急需寻求能够缓解或克服香蕉连作障碍的有效措施。本实验旨在探究使用绿色土壤熏蒸剂对长期连作蕉园的香蕉枯萎病的防控效果，特别是对植株生长发育、土壤化学性质和根际微生物区系的影响。田间试验共设置两个处理：石灰碳铵熏蒸处理（LAB）和对照处理（CK）。结果表明: LAB处理可以显著降低香蕉枯萎病发病率，与CK处理相比两季分别降低40%和46.62%，显著增加香蕉亩产量，与CK处理相比两季分别增产45.56%和75.99%。LAB处理可以显著提高土壤pH，改善土壤酸化，使酸性土壤维持中性水平，同时，增加土壤有机质含量，并且显著提高土壤速效磷（两季分别提高28.33%和89.14%）和速效钾含量（23.92%和38.67%）。并且LAB处理明显改变香蕉根际微生物群落结构，可以显著降低变形菌门和子囊菌门相对丰度，显著增加放线菌门等相对丰度，同时显著降低病原菌镰刀菌属相对丰度，并且显著提高部分土壤拮抗菌属的相对丰度，如链霉菌属、红球菌属和曲霉属。因此，石灰碳铵熏蒸有效改善香蕉根际微生物群落结构，有效防控香蕉枯萎病的发生并促进其植株生长。     

科尔沁草甸湿地土壤碳氮剖面分布及生长季动态特征

采用定位观测的试验方法,于2016年5-10月及2017年8月对科尔沁草甸湿地0~100 cm土层土壤有机碳、全氮剖面分布及生长季动态特征进行了实验分析,旨在为科尔沁草甸湿地保护提供科学指导并为干旱半干旱地区湿地土壤碳氮储量估算提供借鉴。结果表明:1)科尔沁草甸湿地土壤有机碳、全氮含量整体随土层深度下降,0~20 cm土层间下降显著,20 cm以下趋于相对稳定,范围分别为11.9~23.5 g·kg^-1和0.66~1.50 g·kg^-1。2)各土层土壤碳氮含量月间差异显著(全氮40~60 cm土层除外),变化幅度随土层深度先减小后增大;土壤碳氮密度(100 cm)生长季变化大于年际变化,有机碳密度全生长季呈上升趋势,范围为15.44~20.82 kg·m^-2,全氮密度生长初期明显下降,之后趋于相对稳定,范围为1.01~1.16 kg·m^-2。3)土壤有机碳含量与全氮含量呈极显著正相关;植被和水文是影响其分布、变化的关键因子。科尔沁草甸湿地生长季土壤有机碳、全氮密度变化较大,且表现为潜在的碳汇和氮源,但年际间碳汇潜力未充分发挥,本研究建议禁牧力度应加大并增加氮肥投入以提高科尔沁草甸湿地生态系统功能。     

Influence of soil phosphorus status,texture, pH and metal content on the efficacy of amendments to pig slurry in reducing phosphorus losses

Cost‐effective strategies for using chemically amended organic fertilizers need to be developed to minimize nutrient losses in surface and groundwater. Coupling specific soil physical and chemical characteristics with amendment type could increase their effectiveness. This study investigated how water‐extractable phosphorus (P) was affected by chemical amendments added to pig slurry and how this effect varied with soil properties. A 3‐month incubation study was conducted on 18 different mineral soils, stored at 10 °C and 75% humidity and treated with unamended and amended slurry which was incorporated at a rate equivalent to 19 kg total P (TP )/ha. The amendments examined were commercial‐grade liquid alum, applied at a rate of 0.88:1 [Al:TP ], and commercial‐grade liquid poly‐aluminium chloride (PAC ), applied at a rate of 0.72:1 [Al:TP ]. These amendments were previously identified by the authors as being effective in reducing incidental losses of P. The efficacy of the amendments varied with the soil test P, the degree of P saturation (DPS ) and the Mehlich aluminium, iron and calcium, but not soil texture. Chemical amendments were most effective in soils with DPS over approximately 20%. Due to their high cost, the incorporation of amendments into existing management practices can only be justified as part of a holistic management plan where soils have high DPS .     

Do cover crops change the lability of phosphorus in a clayey subtropical soil under different phosphate fertilizers?

Plants have developed different mechanisms to absorb and solubilize phosphorus (P) in the soil, especially in environments with low P availability. This study evaluated the effects of different winter cover crops on soil P availability in a clayey subtropical (Hapludox) soil receiving soluble P fertilizer and a rock phosphate applied to the summer crop, under no‐tillage. The experiment was carried out over 3 yrs (2009–2011) with five different cover crop species: common vetch, fodder radish, ryegrass, black oat, white clover and fallow as control. The soil was sampled after the third year of cover crop cultivation and analysed for inorganic and organic P forms according to the well‐established Hedley fractionation procedure. Phosphate fertilizers promoted accumulation of both labile and nonlabile P pools in soil in the near surface layer, especially under rock phosphate. Fertilizer applications were not able to change P fractions in deeper layers, emphasizing that the Brazilian clayey soils are a sink of P from fertilizer and its mobility is almost nil. Although the cover crops recycled a great amount of P in tissue, in a short‐term evaluation (3 yrs) they only changed the content of moderately labile P in soil, indicating that long‐term studies are needed for more conclusive results.     

甘蔗叶不同还田方式对土壤养分的影响

为减轻秸秆焚烧所带来的环境问题和充分利用甘蔗叶资源,在大田环境下动态监测甘蔗叶粉碎、焚烧和深埋3种还田方式对土壤养分的影响。结果表明:甘蔗叶粉碎还田和深埋还田有利于甘蔗叶中有机碳及氮、磷、钾养分的缓慢释放;甘蔗叶焚烧还田提高了土壤碱解氮含量5.6~20.9 mg/kg和速效磷含量0.8~4.0 mg/kg,促进土壤中氮磷向有效态转化,焚烧还田初期显著增加了土壤速效钾的含量12.3~18.3 mg/kg,但焚烧会损失部分甘蔗叶中碳氮元素,也造成环境污染。综合分析认为甘蔗叶粉碎还田是比较省工、方便的处理方式。     

水稻均衡营养肥对杂交稻生长发育的影响及养分吸收特性

研究了水稻均衡营养肥对杂交稻生长发育的影响及养分吸收特性,以为精准施肥及秸秆还田养分循环利用提供必要的科学参数。结果表明,水稻均衡营养肥处理的株高、总粒数、实粒数、结实率、穗质量和产量均高于常规施肥处理,稻谷中的总钾、S~(6+)和Fe~(2+)含量均高于常规施肥处理,但总磷、Ca~(2+)和Mg~(2+)的含量低于常规施肥处理,总氮含量则基本相同;常规施肥处理的秸秆中总氮、总钾、Mg~(2+)和S~(6+)含量均高于水稻均衡营养肥处理,总磷、Ca~(2+)和Fe~(2+)含量基本相同。均衡营养肥处理氮、磷、钾利用率分别为67.8%、60.0%和95.5%,农民常规施肥处理分别为32.3%、86.0%和100%。可见,水稻均衡营养肥能均衡的为杂交稻生长提供必需的养分,大幅度提高肥料利用率。     

Utilizing a DUALEM‐421 and inversion modelling to map baseline soil salinity along toposequences in the Hunter Valley Wine district

In the oldest commercial wine district of Australia, the Hunter Valley, there is the threat of soil salinization because marine sediments underlie the area. To understand the risk requires information about the spatial distribution of soil properties. Electromagnetic (EM) induction instruments have been used to identify and map the spatial variation of average soil salinity to a certain depth. However, soils vary with depth dependent on soil forming factors. We collected data from a single‐frequency and multiple‐coil DUALEM‐421 along a toposequence. We inverted this data using EM4Soil software and evaluated the resultant 2‐dimensional model of true electrical conductivity (σ – mS/m) with depth against electrical conductivity of saturated soil pastes (EC_p – dS/m). Using a fitted linear regression (LR) model calibration approach and by varying the forward model (cumulative function‐CF and full solution‐FS), inversion algorithm (S1 and S2), damping factor (λ) and number of arrays, we determined a suitable electromagnetic conductivity image (EMCI), which was optimal (R² = 0.82) when using the full solution, S2, λ = 3.6 and all six coil arrays. We conducted an uncertainty analysis of the LR model used to estimate the electrical conductivity of the saturated soil‐paste extract (EC_e – dS/m). Our interpretation based on estimates of EC_e suggests the approach can identify differences in salinity, how these vary with parent material and how topography influences salt distribution. The results provide information leading to insights into how soil forming factors and agricultural practices influence salinity down a toposequence and how this can guide soil management practices.     

施石灰和秸秆还田对双季稻产量和氮素吸收的互作效应

红壤稻田面临土壤酸化和肥力偏低的双重挑战。施石灰和秸秆还田分别是稻田土壤酸化改良和培肥的有效措施,但二者的互作效应尚不清楚。本研究连续4年(2015—2018年)在江西省开展施石灰和秸秆还田双因素田间定位试验,旨在探明施石灰和秸秆还田对红壤双季稻田水稻产量和氮素吸收的互作效应。结果表明,施石灰和秸秆还田均显著提高了早、晚稻的产量和氮素吸收,且二者具显著的协同促进效应。秸秆还田下,施石灰使早稻产量和氮素吸收分别增加10.7%和15.5%;而在秸秆不还田下,增幅仅分别为4.4%和9.7%。秸秆还田下,石灰使晚稻产量和氮素吸收分别提高18.7%和24.6%;但在秸秆不还田下,增幅则分别为10.5%和5.7%。施石灰对早、晚稻产量和氮素吸收的促进效应随试验年限的增加而减弱。石灰对土壤pH值的提升效应随试验年限的延长显著降低。试验4年后,石灰对土壤有机质和全氮含量均无显著影响;秸秆还田显著提高了土壤有机质含量,而对全氮含量无显著影响。因此,秸秆还田配施石灰能够协同实现双季稻增产、土壤酸化改良与培肥。本研究表明在此酸性的红壤双季稻田上每4年左右施用一次石灰为宜。     

Soil risk maps – Interpreting soils data for policy makers,agencies and industry

Surface runoff, erosion, compaction and the leaching of potential pollutants from land can degrade the soil resource and damage the water environment, reducing crop yields, causing loss of valuable nutrients and organic matter, together with increasing flood risk. Increasingly, it is recognized that scientific information must be translated into practical tools to change practices and protect the soil and water resource. Working alongside agencies in Scotland, we applied a suite of simple, transparent, rule-based models to identify areas most at risk of exporting sediment and pollutants that may degrade water quality based on field-scale (1:25,000) soil maps. The maps have been used by Scottish Environment Protection Agency, Scottish Water and Scottish Government to assess soil risks to waters from field to regional scale. The work brought scientists together with policy makers, agencies and the water industry to pool their knowledge to apply these practical tools for decision-making. It highlights the need to apply existing knowledge to answer salient questions. All three examples described show that providing the right type of information, which is based on fundamental soils data, can directly influence the implementation of policies, investment and monitoring decisions and provide evidence in support of government. However, this requires both researchers and agency scientists to develop skills as knowledge brokers and to normalize the use of soil data in everyday agency settings.