接种蚯蚓对潮土氮素矿化特征的影响

在室内恒温（20℃）培养，间歇破坏性采样（于培养后第2、6、13、20、27、41、55天采样）的条件下，研究蚯蚓活动对土壤中氮素矿化特征的影响。共设置4个处理：（1）对照处理-不接种蚯蚓不添加秸秆（S）；（2）仅接种蚯蚓不添加秸秆处理（E）；（3）不接种蚯蚓仅添加秸秆处理（O）；（4）接种蚯蚓并添加秸秆处理（0E）。结果表明：在整个培养时期中，仅接种蚯蚓处理（E）的土壤铵态氮和硝态氮含量均较对照处理（S）有显著提高（P〈0．05），分别较同期对照处理（S）高出0．54-5．71倍和0．04-2．01倍；接种蚯蚓添加秸秆处理（OE）的土壤中的铵态氮含量较同期仅添加秸秆处理（0）增高了0．42-7．26倍，并达到显著性差异（P〈0．05），但两处理的硝态氮含量无显著性差异（P〉0．05）。从整体水平来看，无论是否添加秸秆，接种蚯蚓处理（E，OE）的土壤矿质氮水平均较相应的对照处理（S，O）有显著提高（P〈0．05），到培养55d时，分别增加了1．93倍和2．36倍。仅接种蚯蚓处理（E）的土壤氮素矿化速率和累积矿化速率较对照处理（S）有显著提高（P〈0．05）；添加秸秆后，无论是否接种蚯蚓，土壤累积矿化速率均为负值，表现为对土壤矿质氮的净固定，而从土壤氮素矿化速率的变化来看，前期的各个时间段中主要表现为矿质氮的净固定，后期逐渐表现为一定程度的矿化。此外，仅接种蚯蚓处理（E）的全氮含量除了培养2d外，其他培养时期均与对照处理（S）有显著差异（P〈0．05），到培养55d时，其全氮含量较同期对照处理（S）增高了6．55％。相关性分析结果表明，在仅接种蚯蚓处理（E）中，培养前后蚯蚓鲜重的减少量与土壤全氮含量之间存在极显著正相关（P〈0.01），根据一元线性方程将蚯蚓损失的鲜重换算为蚯蚓体损失的氮量后发现，在整个培养期中蚯蚓体本身排泄的氮大约占土壤全氮含量增加量的百分比为42％-100％。     

露地洋葱施肥、土壤养分及产量状况的分析研究

在农户调查和土壤测试相结合的基础上,分析了山东惠民县露地洋葱土壤养分状况、肥料投入及其对产量和养分平衡的影响。结果表明,施用有机肥农户占总调查户的44%,平均由有机肥带入的氮磷钾养分量分别为N 170kg hm-2、P2O5112 kg hm-2、K2O 223 kg hm-2。化肥氮、磷投入量较高,平均分别为N 458 kg hm-2和P2O5399 kg hm-2,是洋葱氮磷吸收量的4.0和6.0倍,化学钾肥不足(K2O 131 kg hm-2),占洋葱钾吸收量的55%。收获时0~30 cm土壤无机氮含量达到88 kg hm-2,O lsen-P(P)和速效钾(K)平均含量分别为25.5和104 mg kg-1。自春季返青前到收获期间,30~60 cm和60~90 cm土壤无机氮含量均有不同程度的提高,土壤氮表观损失量与氮素投入量呈显著直线相关,维持土壤氮素平衡的最大氮素供应量为290 kg hm-2。相关分析表明,无论是氮、钾化肥投入量还是各阶段土壤无机氮、速效钾含量都与洋葱产量无显著相关,而磷肥用量及0~30 cm土壤剖面O lsen-P含量与产量有显著正相关(p<0.05)。     

Kinetic Parameters of Gross N Mineralization of Peat Soils as Related to the Composition of Soil Organic Matter

Peat land has been considered as an alternative type of land for agricultural development especially in the tropics. In the present study, the N-supplying capacity, one of the most important soil properties in terms of crop production, of peat soils was examined. Ten peat soil samples were collected from Indonesia, Malaysia, and Japan. Gross N mineralization in the soil samples was estimated using a zero-order model, and kinetic parameters of mineralization were determined using a simple type model. Soil organic matter composition was investigated using ¹³C CPMAS NMR. Mineralization potential ( N ₀), apparent activation energy ( E _a), and mineralization rate constant ( k ) ranged between 571–2,445 mg kg⁻¹, 281–8,181 J mol⁻¹, and 0.009–0.020 d⁻¹, respectively. Although none of the parameters showed a significant correlation with the soil C/N ratio, a negative correlation was observed between the k value and the ratio of the proportion of alkyl C in total C to that of O -alkyl C estimated by ¹³C CPMAS NMR. The latter suggested that the k values were higher in the peat soils relatively rich in readily decomposable organic matter including carbohydrates.     

不同品种水稻产量形成过程的养分积累与分配特征研究

通过测定三系杂交稻"汕优63"、两系杂交稻"两优2186"和常规稻"IR64"不同器官N、P和K含量动态,探讨了3种水稻各生育期的养分积累与分配特征。结果表明:3种水稻稻株N含量均随生长过程逐渐下降,同一生育期水稻N含量以"汕优63"最高;除"汕优63"K含量在齐穗时明显上升外,3种水稻的K含量随生长过程逐渐下降;而P含量总体上在分蘖盛期最高。完熟期3种水稻的N积累量依次为24.79g/m2、15.14g/m2和14.42g/m2,P积累量为4.766g/m2、3.306g/m2和3.678g/m2,K积累量为2.439g/m22、.029g/m2和1.725g/m2。"汕优63"分配到籽粒中的N素比例为61.23%,分别比"两优2186"、"IR64"高17.97%和11.23%;分配到籽粒中的P素比例为62.97%,分别比"两优2186"、"IR64"高6.41%和9.63%;分配到籽粒中的K素比例为27.51%,分别比"两优2186"、"IR64"低3.00%和2.39%。在全生育期中,"汕优63"、"两优2186"和"IR64"的N需求量依次为31.33g/m2、22.88 g/m2、24.82g/m2,N、P、K吸收比依次为1∶0.192∶0.098、1∶0.219∶0.134和1∶0.255∶0.120。3种水稻中"汕优63"的养分生产效率最低。N、P、K生产效率"汕优63"依次为37.25kg/kg、193.80kg/kg和378.80kg/kg,"两优2186"依次为52.54 kg/kg、240.38kg/kg和392.16kg/kg,"IR64"依次为58.38kg/kg、228.83kg/kg和487.80kg/kg。三系杂交稻"汕优63"的N、P、K需求量大,积累量高,分配到籽粒中的比例亦高,与其高产特性相吻合。在保证N、P、K供给的前提下,进一步提高养分生产效率是实现"汕优63"高产、高效的关键。     

Irrigation practices may affect denitrification more than nitrogen mineralization in warm climatic conditions

Predicting the impact of irrigation practices on soil N mineralization and N balance is an important issue to optimize N fertilization and reduce the N losses towards the environment. The effect of summer irrigation on N dynamics was investigated in two arable fields in Southern France. Net N mineralization was assessed by combining frequent measurements of water and mineral N contents in soil and the use of a calculation model (LIXIM). It was first calculated assuming that denitrification was negligible. This hypothesis led to inconsistent results, apparent net N mineralized being smaller under irrigated than non-irrigated conditions and net mineralization kinetics being erratic. The occurrence of denitrification was confirmed by the use of ¹⁵NO₃ tracing in an experiment carried out in summer, including three irrigated treatments. The average ¹⁵N recovery varied from 45% to 85% and was smallest in the most frequently irrigated treatment. Over the 8-week experiment, the N losses varied from 30 to 38 kg ha⁻¹ in the irrigated treatments. They were satisfactorily simulated by a simple denitrification model (NEMIS). Combining the LIXIM model and the simulated or calculated denitrification allowed to predict satisfactorily the evolution of soil mineral N accounting for the effects of temperature and moisture. The net N mineralized for 8 weeks varied from 34 kg N ha⁻¹ in the un-irrigated to 46 kg N ha⁻¹ in the irrigated treatments. The drying–rewetting cycles did not induce a flush of N mineralization. Our results suggest that denitrification has to be accounted for in irrigated systems, particularly in warm conditions and when the topsoil contains high nitrate contents.     

Nitrogen fertilizer–induced mineralization of soil organic C and N in six contrasting soils of Bangladesh

A 90‐day laboratory incubation study was carried out using six contrasting subtropical soils (calcareous, peat, saline, noncalcareous, terrace, and acid sulfate) from Bangladesh. A control treatment without nitrogen (N) application was compared with treatments where urea, ammonium sulfate (AS), and ammonium nitrate (AN) were applied at a rate of 100 mg N (kg soil)^–1. To study the effect of N fertilizers on soil carbon (C) turnover, the CO₂‐C flux was determined at nine sampling dates during the incubation, and the total loss of soil carbon (TC) was calculated. Nitrogen turnover was characterized by measuring net nitrogen mineralization (NNM) and net nitrification (NN). Simple and stepwise multiple regressions were calculated between CO₂‐C flux, TC, NNM, and NN on the one hand and selected soil properties (organic C, total N, C : N ratio, CEC, pH, clay and sand content) on the other hand. In general, CO₂‐C fluxes were clearly higher during the first 2 weeks of the incubation compared to the later phases. Soils with high pH and/or indigenous C displayed the highest CO₂‐C flux. However, soils having low C levels (i.e., calcareous and terrace soils) displayed a large relative TC loss (up to 22.3%) and the added N–induced TC loss from these soils reached a maximum of 10.6%. Loss of TC differed depending on the N treatments (urea > AS > AN >> control). Significantly higher NNM was found in the acidic soils (terrace and acid sulfate). On average, NNM after urea application was higher than for AS and AN (80.3 vs. 71.9 and 70.9 N (kg soil)^–1, respectively). However, specific interactions between N‐fertilizer form and soil type have to be taken into consideration. High pH soils displayed larger NN (75.9–98.1 mg N (kg soil)^–1) than low pH soils. Averaged over the six soils, NN after application of urea and AS (83.3 and 82.2 mg N (kg soil)^–1, respectively) was significantly higher than after application of AN (60.6 mg N (kg soil)^–1). Significant relationships were found between total CO₂ flux and certain soil properties (organic C, total N, CEC, clay and sand content). The most important soil property for NNM as well as NN was soil pH, showing a correlation coefficient of –0.33** and 0.45***, respectively. The results indicate that application of urea to acidic soils and AS to high‐pH soils could be an effective measure to improve the availability of added N for crop uptake.     

几种包膜缓控释肥粒养分释放特征的研究

采用水浸泡法对国内外4种包膜控释肥料的养分释放特性进行了系统的研究。结果表明,4种缓控释肥料的初期溶出率均小于12%,微分溶出率在0.4%～1.5%之间,这符合国际上公认的缓/控释肥的评价标准,初期溶出率小于15%、微分溶出率在0.25%～2.5%之间。采用水浸泡法测定包膜控释肥料养分释放特征,简便快速,检测时间短,重复次数少,养分浓度变化直接反映出包膜控释肥料的释放速率特性,还可以定量的测定其供肥性能,控释肥料有控制养分释放、延长供应时间的作用;其中腐殖酸和炭基有利于提高肥料颗粒的水稳定性,减缓养分的释放速率。     

对间隙淋洗长期通气培养条件下黄土高原土壤供氮能力的评价

采用间隙淋洗长期通气培养法,通过对黄土高原物理化学性质差异较大的10种农田土样起始矿质氮、起始提取态总氮、起始可溶性有机氮,以及培养期间淋洗矿质氮、淋洗总氮、可溶性有机氮含量及其与作物吸氮量关系的研究,分析并评价黄土高原主要农田土壤氮素矿化能力以及包括和不包括培养淋洗可溶性有机氮对土壤供氮能力的影响。结果表明,供试土样起始可溶性有机氮平均为N 23.9 mg/kg,是起始提取态总氮的28.8%,土壤全氮的2.4%。在通气培养淋洗总氮中,可溶性有机氮所占比例不高,经过217 d通气培养,淋洗出的可溶性有机氮平均为N 28.8mg/kg,占淋洗总氮量的19.8%。相关分析表明,淋洗可溶性有机氮量与第1季作物吸氮量相关不显著,但与连续2季作物总吸氮量显著相关。淋洗矿质氮、淋洗总氮与两季作物总吸氮量的相关系数明显高于与第一季作物吸氮量的相关系数;与第一季作物吸氮量达显著相关水平,与连续两季作物吸氮量达极显著相关水平。总体上看,可溶性有机氮和土壤全氮、土壤微生物氮不能作为反映短期可矿化氮的指标;间隙淋洗通气培养淋洗液中淋洗矿质氮、淋洗总氮是评价可矿化氮的较好指标,不仅适宜于第一季作物,而且也适用于对连续两季作物土壤供氮能力的评价。     

Establishment of trees on mixtures of pulverized fuel ash and Gypsum. Part II: Nutrition and trace elements

Nutrients and trace elements were determined in the foliage of nine tree species grown in mixtures of pulverized fuel ash (PFA) and gypsum. No serious macronutrient deficiencies were observed. Treatments with PFA consistently increased foliar levels of boron, potassium and molybdenum, and the poor performance of some tree species in pure PFA was attributed to boron toxicity. Gypsum hindered the uptake of boron when mixed with PFA, however, and co-disposal of the two wastes could be used to minimize problems associated with boron toxicity.     

Enhancement of revegetation on construction fill by fertilizer and topsoil application: Effect on mycorrhizal infection

The influence of topsoil and fertilizer application on denuded road construction sites was evaluated to assess its contribution to improvement of vegetation re-establishment. the study sites were within a mixed hardwood and conifer forest on crushed, unweathered subsurface material with low fertility and low biological activity. Topsoils were removed from the site, stockpiled and reapplied to the site after construction. the effect of topsoil amendment on plant growth, soil fertility, mycorrhizal infection and an index of microbial biomass were measured in field and greenhouse experiments. Plant growth on the topsoil amended field plots were greatly increased relative to treatments with fertilizer but no topsoil. Three years after establishment, dry weight production on the plots without topsoil treatment was about 40 per cent of the plots treated with topsoil. Greenhouse experiments were designed to compare fresh, dried and stockpiled topsoil. These experiments indicated that storage of the harvested topsoil for five months in a stockpile had minor effects on plant growth, soil fertility, mycorrhizal infection and microbial biomass. Topsoil volumes had to exceed 20 per cent of the total soil volume to achieve statistically significant benefits and higher ratios showed greater benefit. the percentage of mycorrhizal infection was greatest in topsoil treatments without fertilizer. the addition of fertilizer increased growth but reduced the percentage of roots forming mycorrhizae. When the total weight of infected roots was calculated, however, infection was found to be greatest with a moderate level of fertilizer (equivalent to approximately 27 kg N ha⁻¹ and 39 kg P ha⁻¹), and was less in both higher fertilizer treatments and in unfertilized treatments. Topsoil amendment increased microbial biomass nitrogen but fertilizer treatment did not.