15N-labelled Fertilizer Research Articles

Field-based assessment of the effect of conventional and biodegradable plastic mulch film on nitrogen partitioning, soil microbial diversity, and maize biomass

In an agricultural context, the use of conventional low-density polyethylene (LDPE) and biodegradable plastic mulch film has been actively promoted, however, the effects on physical and biochemical soil properties, crop growth dynamics, yield, and nutrient cycling of conventional and biodegradable mulch film use in a temperate climate remain largely undetermined. Here, we conducted a field experiment, exploring the effects of no mulch (control), conventional (LDPE), and biodegradable (PLA/PBAT) plastic mulch film on soil and crop (Zea mays L.) nitrogen (N) partitioning after application of 15N-labelled ammonium-nitrate fertiliser. Further, we also investigated the treatment effects on soil physical and biochemical properties (e.g., microbial diversity, compound-specific microbial 15N incorporation, N dynamics), plant development, as well as monitoring the biotic and abiotic degradation of the plastic mulch films. We found that conventional mulch film increased crop yield by 25 % and 15N uptake by 34 % compared to the control, simultaneously reducing 15N retention by 40 % in the topsoil (0–10 cm), but not affecting microbial N use efficiency and N transformation and incorporation into the protein pool. Biodegradable film application resulted in similar biomass (306 ± 14 g plant−1) to both control (275 ± 14 g plant−1) and conventional mulch (344 ± 20 g plant−1) treatments, but significantly reduced 15N crop uptake by 63 % compared to the conventional mulch film. We ascribe this to the accelerated mechanical breakdown and faster degradation of the biodegradable mulch film during the growing season. These findings suggest that current biodegradable plastic mulch film polymer blends may not be a suitable alternative to conventional mulch film in terms of short-term productivity and N use efficiency in a temperate climate for maize production.

Time-dependent regulation of soil aggregates on fertilizer N retention and the influence of straw mulching

Fertilizer nitrogen (N) turnover is highly controlled by soil aggregation. However, the functions of the various aggregates that regulate long-term fertilizer N retention under conservation management remain unexplored. In this study, 15N-labeled fertilizer was initially applied in situ to investigate the effects of maize straw mulching on fertilizer N allocation in soil aggregates at a decadal scale. The topsoil was fractionated into macroaggregate, microaggregate, and silt-clay (SC) fractions. Macroaggregate was further divided into particulate organic matter (POM) and mineral-associated organic matter (MAOM). A higher enrichment factor of fertilizer N than of soil total N in macroaggregate indicated that the fertilizer N was more apt to incorporation into macroaggregate. The fertilizer N in the bulk soil declined gradually to 84.0% by the 13th year. Temporally, the reduction proportion of fertilizer N in the SC fraction was the largest before 5th years, whereas macroaggregate was the main reactive spot for fertilizer N transformation from 9 to 13 years. Therefore, the function of aggregates was time-dependent in controlling fertilizer N retention and turnover via the release of previously entrapped fertilizer N, but encapsulated the subsequently applied N (i.e., unlabeled fertilizer), whereas mineral adsorption contributed to the long-term stabilization of fertilizer N. Compared with fertilization alone, straw mulching improved aggregates stability, favored the initial fertilizer N retention in macroaggregate by enriching fertilizer N in POM, and reduced the proportion of N loss in MAOM after 9 years. These finding indicate that the improvement in fertilizer N stability related to straw decomposition was sequentially attributed to the enhancement of aggregate encapsulation and persistent interaction with soil minerals. Therefore, this study provides new insights into the functional heterogeneity of soil aggregates at different time stages and the intricate interplay between carbon availability-controlled fertilizer N retention and the improvement in soil aggregation.

Mycorrhizal associations of temperate forest seedlings mediate rhizodeposition, but not soil carbon storage, under elevated nitrogen availability.

Tree-mycorrhizal associations are associated with patterns in nitrogen (N) availability and soil organic matter storage; however, we still lack a mechanistic understanding of what tree and fungal traits drive these patterns and how they will respond to global changes in soil N availability. To address this knowledge gap, we investigated how arbuscular mycorrhizal (AM)- and ectomycorrhizal (EcM)-associated seedlings alter rhizodeposition in response to increased seedling inorganic N acquisition. We grew four species each of EcM and AM seedlings from forests of the eastern United States in a continuously 13C-labeled atmosphere within an environmentally controlled chamber and subjected to three levels of 15N-labeled fertilizer. We traced seedling 15N uptake from, and 13C-labeled inputs (net rhizodeposition) into, root-excluded or -included soil over a 5-month growing season. N uptake by seedlings was positively related to rhizodeposition for EcM- but not AM-associated seedlings in root-included soils. Despite this contrast in rhizodeposition, there was no difference in soil C storage between mycorrhizal types over the course of the experiment. Instead root-inclusive soils lost C, while root-exclusive soils gained C. Our findings suggest that mycorrhizal associations mediate tree belowground C investment in response to inorganic N availability, but these differences do not affect C storage. Continued soil warming and N deposition under global change will increase soil inorganic N availability and our seedling results indicate this could lead to greater belowground C investment by EcM-associated trees. This potential for less efficient N uptake by EcM-trees could contribute to AM-tree success and a shift toward more AM-dominated temperate forests.

Interactive Effects of Biochar and Nitrogen Fertilizer on Plant Performance Mediated by Soil Microbial Community in a Eucalypt Plantation

Interest in improving plant nitrogen use efficiency (NUE) in conjunction with reduced usage of nitrogen (N) fertilizers in forestry management is growing. Although biochar amendment is widely applied to increase soil nutrient availability and NUE, the mechanism underlying their positive effects remains little understood. We treated the economically important eucalypt species with biochar (BC), N-enriched fertilizer with 15N isotope labeling (NF), and biochar plus 15N-labeled fertilizer (NFB). Moreover, we determined plant N absorption and soil N availability, soil bacterial community composition and its putative keystone taxa, and plant NUE and competition index under different treatments. Our results indicated that NF and NFB significantly increased plant atom % 15N in both eucalypt stem, root, and foliar, as well as the competition index of eucalypt to forbs for acquiring N. NF and BC increased the network complexity of keystone taxa by shifting putative keystone taxa, including phylum Proteobacteria, Chloroflexi, Actinobacteria, Acidobacteria, and Firmicutes. Piecewise structural equation modeling indicated that variations in plant performance were best directly and positively predicted by soil Proteobacteria. This study highlights the importance of interactive effects between biochar and N fertilizer on plant performance mediated by soil microbial community. The change in soil putative keystone taxa has the potential to be a suitable predictor for plant performance in terms of biochar. Our findings may provide important implications for improving fertilization and afforestation management.

Shallow wet irrigation reduces nitrogen leaching loss rate in paddy fields by microbial regulation and lowers rate of downward migration of leaching water: a 15N-tracer study.

China consumes 35% of the world's fertilizer every year; however, most of the nitrogen fertilizers, which are essential for rice cultivation, are not used effectively. In this study, factors affecting the nitrogen leaching loss rate were studied in typical soil and rice varieties in South China. The effects of various irrigation measures on rice growth and nitrogen leaching loss were investigated by conducting experiments with eight groups. These groups included traditional irrigation (TI) and shallow wet irrigation (SWI). The TI is a common irrigation method for farmers in South China, maintaining a water layer of 5-8cm depth. For SWI, after establishing a shallow water layer usually maintaining at 1-2cm, paddy is irrigated when the field water level falls to a certain depth, then this process is then repeat as necessary. The nitrogen distribution characteristics were determined using 15N isotope tracing. In addition, the effects of nitrification, denitrification, and microbial composition on soil nitrogen transformation at different depths were studied by microbial functional gene quantification and high-throughput sequencing. The results revealed that in the SWI groups, the total nitrogen leaching loss rate reduced by 0.3-0.8% and the nitrogen use efficiency (NUE) increased by 2.18-4.43% compared with those in the TI groups. After the 15N-labeled nitrogen fertilizer was applied, the main pathways of nitrogen were found to be related to plant absorption and nitrogen residues. Furthermore, paddy soil ammonia-oxidizing archaea were more effective than ammonia-oxidizing bacteria for soil ammonia oxidation by SWI groups. The SWI measures increased the relative abundance of Firmicutes in paddy soil, enhancing the ability of rice to fix nitrogen to produce ammonium nitrogen, thus reducing the dependence of rice on chemical fertilizers. Moreover, SWI enhanced the relative abundance of nirS and nosZ genes within surface soil bacteria, thereby promoting denitrification in the surface soil of paddy fields. SWI also promoted ammonia oxidation and denitrification by increasing the abundance and activity of Proteobacteria, Nitrospirae, and Bacteroidetes. Collectively, SWI effectively reduced the nitrogen leaching loss rate and increase NUE.

The Effect of Soil Microbial Residues-Mediated Nitrogen Conservation and Supply during the Growing Season on Nitrogen Uptake by Wheat

Microbial residue nitrogen can indicate soil quality and is crucial for soil nitrogen retention and supply. However, it is still unclear how the dynamic changes in soil microbial residue nitrogen affect crop nitrogen uptake in agricultural practice. Based on a long-term wheat-maize rotation experiment with different nitrogen application rates (150 kg N ha−1, 200 kg N ha−1, and 300 kg N ha−1), 15N-labeled nitrogen fertilizer was applied during the wheat season to track the dynamics of soil microbial residue nitrogen and its mediated fertilizer nitrogen. The results showed that nitrogen addition was beneficial to the accumulation of microbial residue nitrogen (mainly fungal microbial residue nitrogen). Its contribution rate to soil total nitrogen is 54.87–56.55%, and the fertilizer nitrogen allocated to it accounts for 27.10–47.50% of the remaining fertilizer nitrogen in the soil. Ultimately, 6.77–10.24% of the nitrogen fertilizer applied remained in the soil as microbial residue nitrogen. In addition, microbial residue nitrogen is mainly mineralized during the jointing and filling stages of wheat. In a word, the accumulation and mineralization of soil microbial residue nitrogen during the application of 200 kg N ha−1 better guaranteed the uptake of nitrogen by wheat, which provided a reliable basis for guiding farmland fertility improvement and nitrogen fertilizer reduction in the North China Plain.

Effects of arbuscular mycorrhizal fungi on uptake, partitioning and use efficiency of nitrogen in wheat

Arbuscular mycorrhizal fungi (AMF) can promote the growth and yield of crops by increasing the use of nutrients. However, the influence of AMF on the uptake, utilization and partitioning of nitrogen (N) from different sources remain uncertain. Therefore, we investigated AMF inoculation on plant biomass, N-uptake (from fertilizers and soil), -partitioning and N use-efficiency (NUE) in two wheat cultivars using 15N isotope labeling in a field and pot experiment. Results showed that AMF inoculation increased both plant biomass and N accumulation, and altered N partitioning in wheat. AMF inoculation significantly increased root N concentration and decreased grain N concentration (GNC) and leaf N concentration. The decrease in GNC by the AMF was mainly attributed to the variations in pre-anthesis accumulated N in vegetative organs and a reduction in the amount of N translocation. AMF significantly increased root dry weight by 13.5–18.2%, N uptake of the root by 25.4–37.2%. The N partitioning ratio in roots increased, but decreased in grains. Further, AMF significantly increased plant uptake of top-dressed 15N-labeled fertilizer by 15.0–17.8%. AMF promoted grain N absorbed from fertilizer (basal and topdressing fertilizer) but reduced its uptake from soil. Importantly, fertilizer N recovery efficiency (FNRE), N utilization efficiency (NUtE) and NUE were higher in AMF than in the control (CK), demonstrating the benefits of AMF inoculation on growth in wheat. Therefore, using AMF as biofertilizers in field conditions may be an effective agronomic practice in order to ensure sustainable production.

Stable-isotope probing highlights the active microbes associated with carbon flow under different cultivation conditions: Rhizosphere soil versus bulk soil and upland soil versus paddy soil

Plant carbon (C) released into the rhizosphere will ultimately impact the bulk soil, varying with soil water status. However, the microbial communities involved, and how they vary between rhizosphere and bulk soil, and under varying water regimes, are little understood. Here, within a continuous 13CO2 labeling chamber, a rhizobox-like system was utilized to cultivate ryegrass (upland) and rice (paddy) to identify the root-derived C flow and associated active microbes. The 15N-labeled fertilizer was used to measure the N flow from the soils and plants. The 13C labeled soil organic C (13C-SOC) values of upland soil were greater than those of paddy soil. There was a reduction in 13C-SOC values from the rhizosphere to the bulk soils, but the total 15N labeled N (15N-TN) values exhibited an increase trend from this direction. The isotopic enrichment of PLFAs and DNA sequencing results indicated that the bacterial and fungal abundance and diversity exhibited augmentation in the rhizosphere soil under both cultures compared with the bulk soils. Bacteria played a much more important role than fungi in the C flow in the paddy soil. However, fungi dominantly contributed to this flow in the upland soils. Our findings revealed a vital role of Ascomycota fungi (especially Talaromyces) and Actinobacteria bacteria (Actinomycetales and Gaiellales) in contributing to the assimilation of root-derived C for the upland and paddy soils, respectively.

Early share of 15N-labelled fertilizer between trees and crop in young temperate alley-cropping system

Nitrogen (N) partitioning between trees and crops in alley-cropping systems (AC) may increase the N fertilizer use, but more investigation is needed to elucidate it for young trees. The aim of this study was to explore the share of N between crops and three tree species after a few years of tree establishment in AC. Using 15N labeling (10 atm% as 15NH4,15NO3 form), we traced the fate of N fertilizer in wheat associated with four-year-old trees at Ramecourt alley-cropping experimental site. The 15N abundance of tree leaves and crop whole-plant was compared between samples collected in AC, in sole-crop control (CC) and in unlabeled and unfertilized pure-forest control plots (FC). The wheat δ15N increased from 0.7 ± 0.6‰ to 994 ± 474‰ before and 12 days after labeling and remained stable until harvest. For natural abundance, no significant difference in wheat δ15N was observed between AC and CC. The same result was observed for labeled treatment. The percentage of wheat N derived from fertilizer was on average 27 ± 17% and no effect of type of system or associated tree species was observed. Tree foliar δ15N was multiplied by 1.5, 1.8 and 4 for willow, hornbeam and wild cherry respectively compared to unlabeled trees in AC. The percentage of tree foliar N derived from fertilizer was on average 0.04 ± 0.04% and no significant difference was observed between tree species. The wheat associated with trees allocated significantly more tracer N to ears than wheat in monocrop. From this study, we succeeded in quantifying the beginning of tree/crop sharing of N fertilizer using labeling method and evidenced tree species effect. Young trees in AC contributed to valorize the N fertilizer without significant effect on global wheat uptake and favored its valorization in wheat grain.

Uptake of Fertilizer Nitrogen and Soil Nitrogen by Sorghum Sudangrass (Sorghum bicolor × Sorghum sudanense) in a Greenhouse Experiment with 15N-Labelled Ammonium Nitrate

A greenhouse experiment with sorghum sudangrass (Sorghum bicolor × Sorghum sudanense) and maize (Zea mays) was conducted to assess information on differences in their nitrogen and fertilizer utilization when used as energy crops. The aim was to contribute to the scarce data on sorghum sudangrass as an energy crop with regards to nitrogen derived from fertilizer (NdfF) in the plant’s biomass and fertilizer nitrogen utilization (FNU). Sorghum sudangrass and maize were each grown in eight bags of 45 L volume and harvested at maturity after 154 days. Each crop treatment was further divided in a control treatment (four bags each) that did not receive N fertilization and a fertilization treatment (four bags each) that received 1.76 g N, applying a 15N-labelled liquid ammonium nitrate fertilizer. Fertilization took place at the start of the experiment. After harvest, the whole plant was divided in the fractions “aboveground biomass” (ABM) and “stubble + rootstock” (S + R). Weight, N content and 15N content were recorded for each fraction. In addition, N content and 15N content were assessed in the soil before sowing and after harvest. The experiment showed that FNU of sorghum sudangrass (65%) was significantly higher than that of maize (49%). Both crops accumulated more soil N than fertilizer N. The share of fertilizer N on total N uptake was also higher with sorghum sudangrass (NdfF = 38%) compared to maize (NdfF = 34%). The observations made with our control plant (maize), showed that the results are plausible and comparable to other 15N studies on maize regarding yields, NdfF, and FNU, leading to the assumption that results on sorghum sudangrass are plausible as well. We therefore conclude that the results of our study can be used for the preliminary parametrization of sorghum sudangrass in soil organic matter (SOM) balance at field level.

Long term co-application of lime and phosphogypsum increases 15 N recovery and reduces 15 N losses by modulating soil nutrient availability, crop growth and N cycle genes

In no-tillage rotation systems, the recovery of nitrogen (N) fertilizer in the soil–plant system is affected by soil fertility and biological changes caused by the surface application of lime (L) and phosphogypsum (PG). Here we assessed the effect of surface-applied L and/or PG on the fate of 15N-labeled fertilizer, soil chemical properties, microbial gene copy number (16 S rRNA of prokaryotes and genes of N cycle) and grain yield of maize (Zea mays L. intercropped with ruzigrass) in rotation with soybean [Glycine max (L.) Merrill] during two growing seasons. We found that applying L improved soil fertility, particularly when combined with PG (LPG treatment), resulting in higher grain yield. Moreover, compared with the control, the recovery of 15N-labeled ammonium sulfate [(15NH4)2SO4] increased in maize and ruzigrass dry matter but decreased in soybean grown on the residue of the first growing season in two treatments (L and LPG). The losses of 15N-labeled fertilizer were highest in the control and PG treatments. A large amount of 15N-labeled fertilizer was found in the deep layers of PG-amended soil, indicating leaching of fertilizer-derived 15N. Conversely, the analysis of soil microbial N cycle genes revealed that the abundances of denitrifiers were highest in the control (no correctives applied), suggesting that the N fertilizer remaining in the soil increased denitrification rates. Surface application of a combination of L and PG is clearly a feasible strategy for increasing soil fertility, 15N recovery from fertilizer, and grain yield while reducing environmental pollution associated with nitrification and denitrification.

LDPE and biodegradable PLA-PBAT plastics differentially affect plant-soil nitrogen partitioning and dynamics in a Hordeum vulgare mesocosm

Micro and macroplastics are emerging contaminants in agricultural settings, yet their impact on nitrogen (N) cycling and partitioning in plant-soil-microbial systems is poorly understood. In this mesocosm-scale study, spring barley (Hordeum vulgare L.) was exposed to macro or microplastic produced from low density polyethylene (LDPE) or biodegradable plastic at concentrations equivalent to 1, 10 and 20 years of plastic mulch film use. Partitioning of 15N-labelled fertiliser into plant biomass, soil and leachate yielded a partial mass balance. Soil N partitioning was probed via compound-specific 15N-stable isotope analyses of soil microbial protein. Concentration-dependent decreases in plant 15N uptake occurred with increased leached nitrogen for LDPE microplastic. Assimilation into soil microbial protein was higher for biodegradable plastics, which we associate with early-stage biodegradable plastic degradation. Partitioning of 15N into inorganic soil N pools was affected by LDPE size, with lower assimilation into the microbial protein pool. While microplastics and macroplastics altered soil N cycling, the limited impacts on plant health indicated the threshold for negative effects was not reached at agriculturally relevant concentrations. This study highlights the difference between conventional and biodegradable plastics, and emphasises that the interplay of micro and macroplastics on soil N cycling must be considered in future studies.

Using 15N Isotope to Evaluate the Effect of Brown Coal Application on the Nitrogen Fate in the Soil–Plant System

The problems of high nitrogen (N) fertilizer application rate and low N utilization efficiency are common worldwide in vegetable plantations. Application of brown coal (BC, also known as lignite) can increase crop yield and fertilizer N recovery efficiency (NRE). However, the effect of BC application on the utilization and distribution of exogenous N in the soil–plant system under different fertilization strategies is unclear. The pot experiment was set up in three factors of randomized design, including 15N-labeled urea fertilizer, BC, and organic manure, and pakchoi was used as the test crop. There were five rates of 15N-labeled urea, including 0, 100, 200, 300, and 400 kg N ha−1, two rates of BC with 5 and 0 t ha−1, and the organic manure with 0 t ha−1 which constitutes ten treatments. The other four treatments were the combination of one 15N-labeled urea rate of 100 kg N ha−1, two rates of BC with 5 and 0 t ha−1, and two rates of organic manure with 100 and 0 kg N ha−1. In conclusion, the interaction of all N fertilizer rates combined with BC improved soil 15N retention efficiency by 10.14% compared without BC amendment. Between 200 and 300 kg N ha−1, the average potential loss rate of 15N decreased by 10.41%. The application of BC could reduce N loss by enhancing plant N uptake and increasing soil retention. The combined use of 200 kg N ha−1 fertilizer and 5 t ha−1 of BC would maintain a high fertilizer NRE and ensure pakchoi yield.

Exploring nitrogen management methods for depressing the decline of wheat grain protein in plastic film mulch via 15N-labelling technique

Sustainably meeting the increasing food and nutrition demand for humanity is a great challenge for the coming decades; for this purpose, improving the yield and quality of cereal crops in drylands is a crucial strategy. Plastic film mulch (PM) systems are widely used in drylands to increase wheat yield; however, they generally reduce wheat grain protein. Here, we address the challenge by optimizing the N fertilizer application methods of PM system. Compared with the traditional flat system, PM3 (striped fertilization on the underside of the ridges) increased mean grain yield by 17% without reducing the grain protein concentration in 2019–2022. Moreover, PM3 increased grain yield by 10% and grain protein concentration by 13% compared with PM1 (broadcasting fertilizers). Results showed that PM3 increased the supply of 15N-labelled fertilizer in Wheat Row of the 0–20 cm soil layer after flowering by 146%, thus increasing the contribution of fertilizer N to grain N by 51–89% and grain N accumulation by 14–27% at 14–48 days after flowering, respectively. Notably, although soil N contributed 54–71% of plant N uptake, the difference in grain N accumulation among PM systems was mainly attributed to differences in plant N uptake after flowering due to changes in the fertilizer N supply. This study provided new insights into improving grain protein concentrations in PM systems through optimized N management, and this may be a starting point for further discussion on achieving collective improvements in yield and quality of grain in PM systems.

Nitrate leaching losses and the fate of 15N fertilizer in perennial intermediate wheatgrass and annual wheat - A field study.

Perennial grains, such as the intermediate wheatgrass (Thinopyrum intermedium) (IWG), may reduce negative environmental effects compared to annual grain crops. Their permanent, and generally larger, root systems are likely to retain nitrogen (N) better, decreasing harmful losses of N and improving fertilizer N use efficiency, but there have been no comprehensive N fertilizer recovery studies in IWG to date. We measured fertilizer N recovery with stable isotope tracers in crop biomass and soil, soil N mineralization and nitrification, and nitrate leaching in IWG and annual wheat in a replicated block field experiment. Nitrate leaching was drastically reduced in IWG (0.1 and 3.1 kg N ha-1 yr-1) in its third and fourth year since establishment, compared with 5.6 kg N ha-1 yr-1 in annual wheat and 41.0 kg N ha-1 yr-1 in fallow respectively. There were no differences in net N mineralization or nitrification between IWG and annual wheat, though there was generally more inorganic N in the soil profile of annual wheat. More 15N fertilizer was recovered in the straw and all depths of the roots and soils in IWG than annual wheat. However, annual wheat recovered much more 15N fertilizer in the seeds compared to IWG, which had lower grain yields. 15N-labeled fertilizer contributed little (<3 %) to nitrate-N in leachate, highlighting the role of soil microbes in regulating loss of current year fertilizer N. The large reduction in nitrate leaching demonstrates that perennial grains can reduce harmful nitrogen losses and offer a more sustainable alternative to annual grains.

Methods to quantify the nitrogen derived from the fertilizer in maize applying blends of controlled-release and NBPT-treated urea

The use of 15N tracers in blends of N-fertilizers contributes to determining the N derived from each N-fertilizer in the plant, improving the recommendation in the field. However, to evaluate the contribution of two 15N-labeled fertilizers to maize nutrition is an expensive process, and it is challenging to manufacture 15N-labeled controlled-release urea (CRU) considering a polymer-sulfur coated urea (PSCU). The objective of this study was to evaluate, in a field experiment, two methods to quantify the N derived from the PSCU (NdfPSCU) in maize plant using two blends (70% PSCU + 30% urea (U) and 30% PSCU + 70% U) applied in three ways (incorporated, broadcast and split application). The first method quantifies the NdfPSCU by subtracting the total N uptake in the N treatment by the sum of the N uptake in the control treatment (without N-fertilizer application) and the N derived from the U (NdfU) in the plant quantified with 15N. The second method quantifies the NdfPSCU using 15N (precise and direct method). Despite the first method is less expensive than the second it underestimated the NdfPSCU in four maize growth stages in Rhodic Eutrustox soil, being necessary the use of 15N in the PSCU to quantify the NdfPSCU with blends of PSCU + U.

Growth and nitrogen status of cotton (Gossypium hirsutum L.) under salt stress revealed using 15N-labeled fertilizer

Abstract Salt stress is a vital factor limiting nitrogen uptake and cotton growth in arid regions. The mechanisms underlying salt stress tolerance in cotton plants under high soil salinity have not been fully elucidated. Therefore, the aim of this study was to examine the proportion and mechanism of cotton nitrogen uptake under salt stress using the 15N isotope labeling technique. Cotton plants were grown in four undisturbed saline soils (1, 3, 6 and 9 dS m−1), and the experiment was designed using the ENVIRO-GRO (E-G) model. The results showed that the dry matter of roots, stems and leaves of the cotton parts in slightly saline soil (C2, 3 dS m−1) was not significant compared with the non-saline soil (C1, 1 dS m−1). The cotton fruit grown in low-salinity soil (C2, 3 dS m−1) had significantly higher dry matter than that grown in the other treatments, implying that cotton plants grown in 3 dS m−1 soil have the best nitrogen uptake and salt tolerance. Cotton plants grown in weakly (C3, 6 dS m−1) and moderately (C4, 9 dS m−1) saline soils exhibited premature senescence. The distribution of total nitrogen and nitrate content in cotton was the best explanatory variable of total 15N recovery, of which cotton 15N recovery was between 26.1% and 47.2%, and soil 15N recovery was between 7.7% and 14.9%. Our findings provide guidance for further exploitation and utilization of saline soil resources and sustainable development of the agricultural soil ecosystem in arid regions.

Effects of Irrigation and N Fertilization on 15N Fertilizer Utilization by Vitis vinifera L. Cabernet Sauvignon in China

This study investigated the interactions between different irrigation and nitrogen (N) fertilization rates and their effects on the 15N fertilizer absorption and utilization of Cabernet Sauvignon grapevines in a vineyard near Xinjiang, China. The fertilizer treatments consisted of three 15N-labeled urea nitrate fertilizer applications (191.4, 254.4, and 317.4 kg/ha). The irrigation treatments included two fractions (0.75 and 1.0) of estimated vineyard water use (ETc). The results showed that: (i) the residual amount of 15N fertilizer in the soil was mainly in the surface layer (0–20 cm), the residual fertilizer N in the surface layer accounted for 68–87% of the total residual N, the residual 15N fertilizer at different depths differed significantly, and the residual 15N was positively correlated with the amount of fertilizer applied (p &lt; 0.05); (ii) The absorption of fertilizer N by grapevines accounted for only 12–17% of the total N absorption, and the proportion absorbed from soil N was as high as 82–87%. There was no significant difference in the amount of N absorbed between different water and fertilizer treatments; (iii) The 15N uptake under the different water and fertilizer treatments differed and was significantly higher in the roots than in other organs, followed by the fruit, the leaves, and finally, the stems. Our results provide a reference for improving the soil environment and encouraging a sustainable development of the grape industry. According to the experimental results, it was recommended that farmers adopt irrigation levels of 1.0 ETc and fertilizer application of 254.4 kg N/ha.

Impact of Nutrient Management on Wheat/Vegetable Yields and the Fate of 15N-Labeled Fertilizer in the Yangtze River Basin

The Yangtze River Basin (YRB) crosses three economic zones and major agricultural regions of eastern, central, and western China. Increasing non-point source pollution, caused by excessive nitrogen (N) inputs to farms, is one of the main causes of water contamination in the YRB. To improve N fertilizer use efficiency, we conducted a field experiment using 15N-labeled urea at three sites located in upstream, midstream, and downstream regions of the YRB to evaluate the impacts of improved fertilizer management on crop yield, fertilizer N recovery, and losses in three crop rotations: rice–wheat (RW), rice–vegetable (RV) [tuber mustard at Jiangjin (Chongqing), cabbage at Shayang (Hubei), and savoy cabbage at Rugao (Jiangsu)] and maize–wheat (MW). Applying only 50% of the traditional application of N and P fertilizer maintained the wheat yield at Jiangjin and Shayang and savoy cabbage yield at Rugao. However, it caused a 27% reduction of the wheat yield at Rugao. The 15N recovery showed that 27% of the fertilizer N was retained in the soil and that 25% less fertilizer N was lost to the environment compared to the traditional fertilizer application. Improved fertilizer management would reduce the environmental cost of farming in the YRB, but with some consequences to winter crop yields.

Determining Nitrogen Accumulation and Nitrogen Use Efficiency of Mung Bean with Organic Nitrogen and 15N-labeled Chemical Fertilizer

ABSTRACT The study investigated the dynamics of nitrogen accumulation in mung been under different nitrogen levels and different nitrogen forms. A pot experiment was conducted, including six treatments: no fertilizer applied (N0), 233 g 15N.plant −1 (N1), 292 g 15N. plant −1 (N2), 350 g 15N.plant −1 (N3), 146 g 15N+146 g organic nitrogen (N organic), plant −1 (ON1), and 292 N organic. Plant −1 (ON2). The organic nitrogen was provided by the fermented soybean cake. The 15N was provided in chemical nitrogen form. The yield in N2 was the highest among N0-N3. With 15N increasing, Rhizobia fresh weight showed downward trend. Compared with N2, both ON1 and ON2 improved the 1000-grain weight, yield and grain crude protein content. According to 15N-labeled method, mung bean plants got more nitrogen from soil before R1 stage than other growth periods, later the absorbed nitrogen would be dynamically exchanged out of plant through root-Rhizobia interaction, but mung bean again accumulated more nitrogen from soil at R8. N2 had the largest 15N translocation rate from roots to grains in the experiment; The nitrogen use efficiency increased with chemical nitrogen increasing, the value being 14.0% in N1, 22.5% in N2 and 26.1% in N3. The nitrogen use efficiency of ON1 was 23.0%. The repart coefficient of 15N ranged from 50.4–56.7% in grains, 3.0–3.1% in shells, 18.7–27.2% in leaves, 14.3–15.4% in stems and 4.9–8.3% in roots. The nitrogen use efficiency calculated based on nitrogen difference was 6.6–31.3% higher than that based on 15N tracer technique. In sum, appropriate nitrogen fertilizer (N2) is beneficial to the increase of mung bean yield. The application of organic nitrogen fertilizer could alleviate the inhibition effect of nitrogen fertilizer on Rhizobia, reduce the loss of soil nitrogen, and further improve the yield of mung bean.