Effects of decreasing soil water content on seminal lateral roots of young maize plants

Soil micropores that contain water at or below field capacity cannot be invaded by seminal or first‐order lateral roots of maize plants because their root diameters are larger than 10 μm. Hence, at soil‐water levels below field capacity plant roots must establish a new pore system by displacement of soil particles in order to access soil water. We investigated how decreasing soil water content (SWC) influences growth and morphology of the root system of young maize plants. Plants were grown in rhizotrons 40 cm wide, 50 cm high, and approximately 0.7 cm thick. Five SWC treatments were established by addition of increasing amounts of water to soil and thorough mixing before filling the rhizotrons. No water was added to treatments 1–4 throughout the experiment. Treatment 5 was watered frequently throughout the experiment to serve as a control. Seminal‐root length and SWC in soil layers 0–10, 10–20, 20–30, 30–40, and 40–50 cm were measured at intervals of 2–3 d on scanner images by image analysis. At 15 d after planting, for treatments 1–4 shoot dry weight and total root length were directly related to the amount of water added to the soil, and for treatments 4 and 5, total root length and shoot dry weights were similar. Length of seminal roots visible at the transparent surface of the rhizotron for all treatments was highest in the uppermost soil layer and decreased with distance from the soil surface. For all layers, seminal‐root elongation rate was at maximum above a SWC of 0.17 cm³ cm^–3, corresponding to a matric potential of –30 kPa. With decreasing SWC, elongation rate decreased, and 20% of maximum seminal root elongation rate was observed below SWC of 0.05 cm³ cm^–3. After destructive harvest for treatment 1–4, number of (root‐) tips per unit length of seminal root was found uninfluenced over the range of initial SWC from 0.10 to 0.26 cm³ cm^–3. However, initial SWC close to the permanent wilting point strongly increased number of tips. Average root length of first‐order lateral (FOL) roots increased as initial SWC increased, and the highest length was found for the frequently watered treatment 5. The results of the study suggest that the ability to produce new FOL roots across a wide range of SWC may give maize an adaptive advantage, because FOL root growth can rapidly adapt to changing soil moisture conditions.     

Silicon alleviates the toxicity of cadmium and zinc for maize (Zea mays L.) grown on a contaminated soil

Although silicon (Si) is not an essential element, it presents a close relationship with the alleviation of heavy‐metal toxicity to plants. This work was carried out to evaluate the effects of Si application to soil on the amelioration of metal stress to maize grown on a contaminated soil amended with Si (0, 50, 100, 150, and 200 mg kg^–1) as calcium silicate (CaSiO₃). Additionally, the cadmium (Cd) and zinc (Zn) bioavailability as well as their distribution into soil fractions was also studied. The results showed that adding Si to a Cd‐ and Zn‐contaminated soil effectively diminished the metal stress and resulted in biomass increase in comparison to metal‐contaminated soil not treated with Si. This relied on Cd and Zn immobilization in soil rather than on the increase of soil pH driven by calcium silicate application. Silicon altered the Cd and Zn distribution in soil fractions, decreasing the most bioavailable pools and increasing the allocation of metals into more stable fractions such as organic matter and crystalline iron oxides.     

Influence of iron nutrition on sulphur uptake and metabolism in maize (Zea mays L.) roots

Abstract

Recent research has evidenced a relationship between Fe nutrition and S nutrition. Aim of the present work was to investigate the effect of Fe deficiency on the capacity of maize roots to take up and metabolize S. Maize (Zea mays L. cv. Cecilia) plants were grown for 10 d in nutrient solution (NS) with (+S) or without (?S) sulphate and Fe was added as Fe^III-EDTA at 80 μm. After removing the extraplasmatic Fe pool, half of the plants of each treatment (+S and ?S) were transferred to a new Fe-free NS. Roots were collected 4 and 24 h from the beginning of Fe deprivation. Fe deprivation slightly increased root thiols content in both nutritive conditions (+S and ?S). ATP sulphurylase activity was enhanced by sulphur deprivation, but greatly depressed when Fe and S were both omitted from the nutrient solution. O-Acetylserine sulphydrylase activity was also enhanced by S deprivation; this activity was increased by Fe starvation in +S plants, while it was unaffected by Fe nutrition in ?S plants. S deprivation greatly increased uptake rates of ³⁵SO₄ ^2? (1.9 ± 0.1 vs. 5.2 ± 0.2 μmol g^?1 root d.w. h^?1); furthermore, Fe deficiency increased ³⁵SO₄ ^2? uptake rates by 11 and 55% in +S and ?S plants, respectively. Data show that Fe-deficiency in maize results in a higher ability to take up sulphate, while limiting the first step of S assimilation in S deprived plants.     

接种自生固氮菌对玉米根际土壤酶活性和细菌群落功能多样性的影响

为了探索玉米根际土壤微生态特征对接种自生固氮菌的响应机理,在盆栽实验条件下,研究了3株自生固氮菌褐球固氮菌（Azotobacter chroococcum YCYS）、芸苔叶杆菌（Phyllobacterium brasssicacearum QL54）和类芽孢杆菌（Paenibacillus sabinae MX31）接种盆栽玉米（Zea mays L.）之后,玉米根际土壤酶活性和细菌群落功能多样性的变化。结果表明,接种自生固氮菌对玉米根际土壤酶活性和细菌群落功能多样性产生了一定的影响,而且不同自生固氮菌之间的接种效果有一定的差异。接种褐球固氮菌（A. chroococcum YCYS）和类芽孢杆菌（P. sabinae MX31）玉米根际土壤脲酶活性分别比对照高20.55%和9.58%。然而接种处理对玉米根际土壤碱性磷酸酶活性的影响差异不显著（P0.05）。BIOLOG结果显示,接种自生固氮菌可以提高细菌总代谢活性,其中接种褐球固氮菌（A. chroococcum YCYS）处理的AWCD是对照的1.8倍,并且细菌群落丰富度指数（R）显著高于对照（P0.01）。不同接种处理土壤根际细菌生理碳代谢优势群落结构不同。主成分分析（PCA）表明接种自生固氮菌可以调控根际土壤细菌群落功能多样性。     

Denitrification with and without maize plants (Zea mays L.) under irrigated field conditions

The study was conducted under irrigated field conditions to examine the effect of maize plants on denitrification. Both planted and unplanted field plots received 150kgNha^–1 as urea. In a third treatment, which was also planted and received urea at 150kgNha^–1, the soil nitrate N content was brought up to equal to that in the unplanted plots by applying additional doses of N as calcium nitrate. Soil cores were collected 24 and 72h after irrigation and the denitrification rate was measured by the acetylene inhibition method. Nitrate-N content, aerobically mineralizable C, microbial biomass carrying capacity and denitrification potential were also studied on field-moist soil. Maize plants grown under field conditions always had the potential to increase denitrification in conditions of both high and low water-filled porosity. When nitrate-N content of the planted soil decreased due to plant uptake, denitrification was reduced in the planted soils. However, when nitrate-N uptake by plants was compensated through additional doses of nitrate fertilizer, denitrification was always higher in planted than unplanted soil. The stimulatory effect of plants on denitrification was observed at both high and low soil nitrate-N concentrations, though it was more pronounced at high nitrate-N levels. The effect of plants on denitrification and related parameters was confined to the root zone. Received: 15 April 1996     

Kinetics of 15N-labelled nitrate uptake by maize (Zea mays L.) root segments

Abstract

Isotherms and kinetic constants of nitrate uptake by excised root segments from the apical root zone of 6-d-old maize seedlings pretreated with nitrate were investigated using ¹⁵N-labelled nitrate. The isotherms were resolved into two systems namely a multiphasic saturable system at substrate concentrations lower than 2 mol m^?-3 and a linear system at higher concentrations. The detailed analysis of the multiphasic saturable system suggested the existence of at least three phases, which followed the Michaelis-Menten kinetics. The I _max and K _m of each phase increase from the lower phase to the upper phase. The distance from the root tip and the presence of stele affected considerably the linear system but only slightly the saturable system.     

玉米立茬与粉碎秸秆覆盖对生长季土壤呼吸的影响

农田土壤呼吸(Rs)是全球CO_2循环的重要组成部分,生长季土壤呼吸对于作物的产量有巨大的影响,同时,作物残茬的覆盖模式会影响土壤呼吸。该文应用了粉碎秸秆覆盖地表(SH)和立茬覆盖地表(ST)是两种主流的作物残茬覆盖地表模式,自2000年起,玉米收获之后,在试验地块施用这2种作物残茬覆盖地表的模式。自2013年开始,在试验地块测量每年冬季的土壤结冻深度,积雪的厚度与CO_2通量,土壤温度与湿度。总土壤呼吸分为异养呼吸(HR)和根际呼吸(RR),该文使用放射性碳标记技术和数学方程计算异养呼吸和根际呼吸的CO_2通量。试验结果显示,与SH处理相比,ST处理地表平均积雪厚度可以增加44%,最大土壤冻深降低18%,并且冻土完全融化的时间将提前10到27 d。ST与SH的平均CO_2通量分别为16.55和14.02 mmol/m~2h。对于整个生长季,SH与ST的土壤呼吸差别在生长季开始和结束时期较小,在生长季的中期较大。ST的平均Rs比SH多3.3 mmol/m~2h,在ST中,HR是Rs的主要构成部分,而RR只约占总土壤呼吸10%。冗余分析结果显示,Rs和HR与土壤温度和积雪厚度呈正相关,与冻土深度呈负相关。该文的研究结果显示相比较于粉碎秸秆残茬覆盖,立茬覆盖地表有利于提高生长季的土壤呼吸,可为玉米的光合作用提供较多CO_2,这将有利于作物增产。     

Variation among maize (Zea mays L.) accessions of Bendel State,Nigeria

Summary Variability in maize zein protein band mobilities in sodium dodecyl sulphate-polyacrylamide gel electrophoresis (SDS-PAGE) was characterized to classify 27 maize accessions (OTUs) collected from Bendel State, Nigeria. The classification of the OTUs was achieved using two numerical procedures: average linkage cluster analysis and principal component analysis (PCA). Five clusters were delineated by the cluster analysis whereas the PCA complemented the cluster analysis by separating the OTUs with yellow kernels into one group and OTUs with early maturity into another. OTUs from the same geographical contiguity commonly grouped together. However some regional overlappings of the OTUs occurred. Results of the PCA revealed that zein bands that stained less intensely more strongly separated the OTUs into various clusters than did those that stained more intensely.     

Residual effects of poultry litter on silage maize (Zea mays L.) growth and soil properties derived from volcanic ash

Abstract

Poultry litter (PL) is a cheap alternative to conventional fertilizers. The use of PL in this way also reduces the environmental problems normally associated with its disposal. The residual effect of PL may reduce the amount of fertilizer (especially N fertilizer) required by subsequent crops. This study examines the residual effects of PL (with and without additional mineral fertilizer) on the properties of a volcanic ash soil and on silage maize (Zea mays) yields in central Chile. Poultry litter and mineral fertilizer were applied in 2002–2003 and their residual effects were determined in 2004–2006. The dry matter (DM) yield, nutrient balance and apparent nitrogen recovery efficiency (ANRE) of the silage maize were determined for each season, and the soil properties were analyzed at three depths (0–20, 20–40 and 40–60 cm) at the end of the third season. Crop yield showed a positive response to all fertilizer treatments. The residual effect, the nutrient balance, N uptake and ANRE also improved with fertilizer treatment, especially with the PL treatments. The average DM yield for the PL treatments was higher than that observed using mineral fertilizer by 2.8 and 1.2 Mg ha^?1 in the third and fourth years, respectively. The ANRE was generally higher in the PL treatments, although it decreased over time (12.4 and 1.7% for the last 2 years, respectively). The mean ANREs for the mineral fertilizer treatment were 4.1 and 1.6% for the same years. The results suggest that the PL treatments had an important positive residual effect in terms of N supply. This should be taken into account when planning the next crop. After two annual applications of PL, slight increases were observed in soil NO₃-N at a depth of 0–20 cm, and extractable P at depths of 20–40 cm and 40–60 cm. No other soil variables were significantly affected by any of the treatments. An additional source of K was found to be necessary to maintain an adequate soil K level.     

Plastic film mulching on soil water and maize (Zea mays L.) yield in a ridge cultivation system on Loess Plateau of China

Plastic film mulching has commonly been used for adaptation to water scarcity and for increasing agricultural productivity on the semiarid Loess Plateau of China. However, the effect of plastic film mulching on cropland soil water and thermal regimes on the semiarid Loess Plateau of China is not well understood. This study simultaneously monitored the dynamics of the soil water content and the soil temperature with high resolution in a ridge cultivation system with plastic film mulching (RS) and a flat cultivation system without plastic film mulching (FS) during the maize (Zea mays L.)-growing season. We found that, in general, the soil temperature and soil water content were significantly different among the ridge under RS (RS-ridge), the furrow under RS (RS-furrow) and FS throughout the maize-growing season (P < 0.05). Plastic film mulching increased the near-surface soil temperature by approximately 1°C throughout the study period. RS significantly increased the soil water content during the dry period (May to June), especially within the middle soil layer (30–60 cm), compared to FS. The lowest monthly average soil water content was found at a depth of 30–60 cm layer in FS during the dry period (May and June). The water depletion was found within deeper (100–160 cm) soil layers in May but the water storage in the same layer of FS in June increased although it was the dry period, which differed from RS. The RS practices showed a longer period of water supply from the deeper soil layer (100–160 cm) in May and June for meeting maize water demands during the early growing stage rather than in only May for FS. During June (dry period), the water storage at a depth of 0–60 cm was greater in RS than in FS, and the reverse was true at a depth of 60–160 cm. The results indicate that the dry soil layer at a depth of 30–60 cm formed during June in FS likely reduced water movement from deeper layers to the topsoil layer, and hence constrained the availability of surface soil water for meeting maize water requirements during the early growing stage (dry period). Our study suggests that RS tends to significantly increase surface soil water availability by restraining the formation of a dry soil layer during the early maize-growth stage primarily under dry conditions, and thus enhances maize productivity in the semiarid Loess Plateau of China.     

Metal binding properties of high molecular weight soluble exudates from maize (Zea mays L.) roots

Summary A high molecular weight (MW > 1000) soluble root exudate fraction (HS) was isolated from hydroponic axenic maize cultures in order to investigate its metal-binding properties. Measurements of the maximum binding ability (MBA) and the overall stability constants (log K) for cadmium-, copper-, lead- and zinc-HS associations were obtained from dialysis and ion-selective electrode titrations. All results showed the occurrence of organometallic bindings. Data fitted to linear Langmuir isotherms. The MBA, measured by dialysis titration, varied from 160 to 206 mEq/100 g HS according to the nature of the metal. log K values, following the series Pb > Cu > Cd 5 Zn, varied from 3.15 to 3.65. Due to these metal-binding properties, soluble root products could play a role in the transfer of metal into the rhizosphere.     

Critical limit of boron for maize (Zea mays L.) in red and lateritic soil of Jharkhand,India

ABSTRACT

To establish a critical limit in soils and plant, an experiment was conducted in red and lateritic soil (Alfisols) of farmer’s field in tribal-dominated Panchayat Kurum, Palkot block, Gumla district, Jharkhand, India. Based on the results of the field experiment, the critical limits were determined as 0.48, 0.50, 0.47, and 0.42 mg kg^?1 in the soil, respectively, for hot water, hot calcium chloride, salicylic acid, and ammonium acetate-extractable B, while a critical limit of 12.00 mg kg^?1 was observed in maize tissue using the graphical method. In an analysis of variance method, the critical limits of B in soils were found as 0.45, 0.54, 0.49, and 0.43 mg kg^?1 using hot water, hot calcium chloride, salicylic acid, and ammonium acetate extractants, respectively. Maize plants were highly responsive to B application where soil B level was below the critical limit (0.50 mg kg^?1). In a field experiment, grain yield of maize increased with increasing levels of B application, while soil application at 1.0 kg ha^?1 + two foliar application (at the knee and pre-flowering stages) of borax at 0.2% were showed significantly higher grain yield of the maize crop. The hot water, hot calcium chloride, salicylic acid, and ammonium acetate-extractable B were significantly and positively correlated with organic carbon and negatively correlated with the electrical conductivity of soils.     

玉米农田生态系统土壤呼吸作用季节动态与碳收支初步估算

从2005年4月底到9月底对玉米农田生态系统的土壤呼吸作用进行了连续观测.结果表明: 2005年玉米生长季土壤呼吸速率均值为3.16 μmol (CO2)·m-2·s-1, 最大值为4.77 μmol (CO2)·m-2·s-1, 出现在7月28日, 最小值为1.31 μmol (CO2)·m-2·s-1, 出现在5月4日.通过建立土壤呼吸速率与玉米根系生物量的回归方程, 对土壤异养呼吸作用占土壤呼吸作用的比例进行间接估算.玉米生长季中, 土壤异养呼吸作用占土壤呼吸作用的比例在36.4%～56.9%之间波动, 均值为45.5%.假定玉米果实和秸秆中的碳在收获期间未从农田中转移走, 2005年整个生长季中玉米农田生态系统的碳收支为-1 127.0 g (C)·m-2, 碳交换速率在0.52～ -18.05 g (C)·m-2·d-1之间波动.玉米生长初期, 玉米农田生态系统表现为碳的弱源; 玉米播种后36 d一直到收获, 玉米农田生态系统表现为碳汇.     

Effects of N‐fertilization on shoots and roots of rape (Brassica napus L.) and consequences for the soil matric potential

The underlying question of these investigations asked, how and to which extent rape plants react with transpiration and soil water uptake to different degrees of nitrogen fertilization. Therefore repeated campaigns with concurrent measurements of plant surfaces (leaves, stems, pods), diurnal courses of leaf transpiration and root length density of rape plants growing on heavily (240 kg ha^—1), moderately, (120 kg ha^—1), and nil N‐fertilized plots of an experimental field in northern Germany were performed during two growing seasons. Additionally, matric potentials at different soil depths were measured. In the first year (1994) investigations were concentrated primarily on shoot area development and transpiration, whereas in the subsequent year (1995) root measurements were mainly undertaken. Also, the influence of soil management (ploughing, conservation tillage) was taken into consideration. The plots where the shoot measurements were carried out were ploughed in 1994 and rotovated in 1995. Matric potentials were measured in both years in ploughed soil and, for comparison, also in soils with conservation tillage. Shoot area index, as measure of the transpiratory capacity of the canopy, increased on ploughed soil and reached a maximum before flowering. Thereafter it decreased until harvest when the relative amount of green stems and pods was increasing. Then, the measured transpiration rate per pod surface area was equal to, or higher than, the transpiration rate per leaf surface area. Plant surface area was smaller in plots with conservation tillage and decreased generally with decreasing N‐fertilization. Increasing plant surface area was joined by an increasing density of plant canopy. Light interception was thus highest in the plots receiving 240 kg N ha^—1. Although the shading effect may cause a reduction of transpiration per plant, the total plant mass per area generally resulted in a greater water loss from these plots. Roots reached at least 110 cm depth. Root length density was significantly higher in the upper 10—30 cm of soil than at greater depths. Root mass was smaller in soil with conservation tillage than in ploughed soil. Oscillations of soil matric potentials in the diurnal and long‐term periods were highest in the upper 10 cm of soil. Here, they corresponded well with the cumulative diurnal transpiratory water loss. It is concluded that the soil water dynamics depends largely on the distribution of plant roots. As a result, rape plants did not change their specific transpiration capacity as a response to increased nitrogen fertilization. However, the transpiring plant surface and root length density increased the turnover rate of water by a higher plant density per plot. This effect was more pronounced in ploughed than in rotovated plots.     

Improving iron bioavailability and nutritional value of maize (Zea mays L.) in sulfur-treated calcareous soil

Soil factors such as pH, calcium, carbonate, and bicarbonate precipitation products in calcareous soils reduce iron (Fe) availability to crops and limit grain Fe concentrations. In the present greenhouse study, we evaluated the potential of Fe fertilizer amendments combined with organic amendments, like biochar (BC) and poultry manure, in sulfur (S)-treated low pH calcareous soils (pH_S1) to assess Fe biofortification of maize. Elemental sulfur (S) was used both for lowering soil pH and Fe solubilization. Soil pH was successfully lowered down from 7.8 to 6.5 by S application at the rate of 2.5 g kg^?1 soil. Pot experiment results revealed that Fe fertilizer combined with BC and S (pH_S1) significantly increased root and shoot dry weight, grain weight, photosynthetic rate, transpiration rate, and stomatal conductance by 69%, 86%, 28%, 74%, 57%, and 33%, respectively, relative to the control. Similarly, combined application of Fe + BC in S-amended (pH_S1) soil increased starch (34%), protein (64%), and fat (1 fold) while antinutrient phytate and polyphenols were decreased up to 29% and 40%, respectively, over control. Regarding the maize nutrients profiles, application of Fe with BC gave the maximum increase of Fe and ferritin was increased 1.7 fold at pH_S1. The results of this study showed that Fe fertilization with BC at pH_S1 soil is beneficial for crop growth and Fe bioavailability.     

Influence of soil moisture,soil compaction and K fertilization on maize (Zea mays L.) grown on Iwo Soil

A greenhouse study was conducted to evaluate the performance of maize (Zea mays L.) on Iwo Soil in relation to different levels of soil moisture, soil compaction and K fertilization. Reductions in dry matter yields of maize were closely associated with soil moisture stress and compaction. There was significant interaction between soil moisture and bulk density, with highest yields occurring at 17% and 21% soil moisture levels for 1.6 and 1.2 g/cm³ bulk densities, respectively. Moisture stress and compaction resulted in greater reductions in the yield of roots than that of shoot. Yield and K uptake were more adversely affected by compaction compared to soil moisture stress. Addition of K increased yield and plant K content but the 60 ppm and 120 ppm rates were not significantly different in terms of improving crop performance. Implications of the results relative to long-term management of Iwo Soil are discussed.     

Biochar properties and soil type drive the uptake of macro‐ and micronutrients in maize (Zea mays L.)

The use of biochar in agriculture is a promising management tool to mitigate soil degradation and anthropogenic climate change. However, biochar effects on soil nutrient bioavailability are complex and several concurrent processes affecting nutrient bioavailability can occur in biochar‐amended soils. In a short‐term pot experiment, the concentration of N, P, K, S, Ca, Mg, Cu, Zn, Mn, B, Fe, and Na in the shoots of maize grown in three different soil types [sandy soil (S1), sandy loam (S2), and sandy clay loam (S3)] was investigated. The soils were either unamended or amended with two different biochars [wheat straw biochar (SBC) or pine wood biochar (WBC)] at two P fertilizer regimes (–/+ P). We used three‐way ANOVA and Principal Component Analyses (PCA) of transformed ionomic data to identify the effects of biochar, soil, and P fertilizer on the shoot nutrient concentrations. Three distinct effects of biochar on the shoot ionome were detected: (1) both biochars added excess K to all three soils causing an antagonistic effect on the uptake of Ca and Mg in maize shoots. (2) Mn uptake was affected by biochar with varying effects depending on the combined effect of biochar and soil properties. (3) WBC increased maize uptake of B, despite the fact that WBC increased soil pH and added additional calcite to the soil, which would be expected to reduce B bioavailability. The results of this study highlight the fact that the bioavailability of several macro and micronutrients is affected by biochar application to soil and that these effects depend on the combined effect of biochar and soils with different properties.     

氮肥种类和淹水胁迫对砂姜黑土区玉米苗期生长和养分吸收的影响

采用盆栽土培方法,比较0~14 d持续淹水胁迫条件下,不同形态的氮肥以及施氮、磷和钾肥对砂姜黑土区富钾低肥土壤上种植玉米苗期植株的地上部生物量、氮、磷和钾含量与累积量的影响。结果表明,在玉米3叶1心期(淹水胁迫处理前),施硝酸钾处理地上部的生物量明显高于除施硝酸铵处理以外的其它处理(P0.05)。在3个缺素处理中,不施钾处理地上部的生物量明显低于不施磷处理(P0.05),但与不施氮处理差异不显著。在淹水胁迫过程中,施肥和淹水胁迫的交互作用影响不显著,在淹水胁迫处理7 d时,施不同形态的氮肥以及施氮、磷和钾肥显著影响玉米地上部的生物量和氮累积量(P0.05),并极显著影响磷累积量和钾累积量(P0.01);淹水胁迫也显著降低了此时玉米植株地上部的氮累积量,并极显著降低其钾累积量(P0.01),且当胁迫处理延长至14 d时,淹水胁迫还引起生物量和磷累积量的显著下降(P0.05)。延长淹水胁迫持续时间,对生物量、氮累积量和钾累积量的肥效差异与胁迫的抑制效应分别呈现加大和增强的趋势。比较F值大小可知,在淹水胁迫处理7 d时,氮肥种类是玉米地上部生物量、氮和磷累积量变化的主要诱因;而当胁迫处理延长至14d时,淹水胁迫则上升为主要决定因子。与此不同,胁迫处理开始后,淹水胁迫始终是钾累积量变化的主要决定因子。在淹水胁迫条件下,尿素可能是有利于提高富钾低肥土壤苗期玉米耐淹水胁迫性的氮肥种类。