scholarly journals The Transformation Dynamics and Homogeneity of Different N Fractions in Compost Following Glucose Addition

Agriculture ◽  
2021 ◽  
Vol 11 (10) ◽  
pp. 971
Author(s):  
Caibin Li ◽  
Shuai Ding ◽  
Chenghang Du ◽  
Yi He ◽  
Zemeng Ma ◽  
...  
Keyword(s):  
Isotopic Labeling ◽  
Scientific Basis ◽  
Hot Water ◽  
Organic N ◽  
Microbial Biomass N ◽  
Mineral N ◽  
Available N ◽  
Microbial Responses ◽  
N Fractions ◽  
Time Point

The application of compost to soil is a common fertilization practice for improving soil quality and crop growth. The isotopic labeling technique is mostly used to investigate the contribution of compost N to crop uptake. However, compost N includes various N fractions and labeling dissimilarity, which may cause bias when calculating the compost N contribution to plants. Therefore, the labeling dynamics of different N fractions in compost and the homogenous labeling time point should be clarified. Given the 15N-labeling in chemical fertilizer and the carbon source, i.e., glucose, the compost N pools were divided into active N (mineral N, soluble organic N [SON], microbial biomass N [MBN]), stable N (hot-water extractable organic N [HWDON]), and recalcitrant N. The atom percentage excess (APE) of different N in compost notably varied at the beginning of incubation, ranging from 0–3.7%. After the addition of glucose, biological N immobilization was promoted (13.7% and 28.8% for MBN and HWDON, respectively) and promoted the transformation among available N pools. Adding distinct doses of glucose at three stages to 15N-labeled compost resulted in diverse microbial responses, thereby redistributing exogenous N in each fraction (15NH4+-N went into SO15N from day 15 to day 30 and increased by 5.1%; SO15N entered MB15N and HWDO15N during day 30 to day 45 and increased by 5.7% and 5.2%, respectively). On day 45, homogeneous 15N-labeled compost was achieved, which was 2.4% for 15N APE for all N fractions. Overall, the quantitative data for the transformation of N fractions in compost at distinct stages provides a scientific basis for compost labeling trials, in order to identify the time point at which compost N-labeling is homogeneous, which is necessary and meaningful to reduce the bias of the contribution rate of compost-N to plants.

scholarly journals Assessing the Response of Tomato Yield, Fruit Composition, Nitrogen Absorption, and Soil Nitrogen Fractions to Different Fertilization Management Strategies in the Greenhouse

HortScience ◽  
2019 ◽  
Vol 54 (3) ◽  
pp. 537-546
Author(s):  
Pengpeng Duan ◽  
Ying Sun ◽  
Yuling Zhang ◽  
Qingfeng Fan ◽  
Na Yu ◽  
...  
Keyword(s):  
Microbial Biomass ◽  
Soil Microbial Biomass ◽  
Organic N ◽  
Microbial Biomass N ◽  
Mineral N ◽  
Soil Microbial ◽  
Tomato Yield ◽  
Fruit Composition ◽  
Soil Microbial Biomass N ◽  
Biomass N

A greenhouse field experiment involving tomato (Solanum lycopersicum) was performed using different nitrogen (N) management regimes: sole application of differing rates of chemical N fertilizer (SC) (SC treatments: N0, N1, N2, and N3) and combined application of manure and chemical N fertilizer (MC) (MC treatments: MN0, MN1, MN2, and MN3). These were used to understand the relationship between comprehensive fruit composition, yield, and N fractions (soil mineral N; soil soluble organic N; soil microbial biomass N, and soil fixed ammonium) under greenhouse conditions. The results showed that the MC treatments significantly increased vitamin C and soluble sugar content compared with SC treatments. In addition, the MN2 treatment produced a high yield and had a positive effect on fruit composition. The N3 (563 kg N/ha) and MN3 (796 kg N/ha) treatments resulted in a high loss of N below the root zone (0–30 cm), consequently reducing N use efficiency. Soil mineral N, soil soluble organic N, and soil fixed ammonium tended to be higher during the first fruiting period, whereas soil microbial biomass N tended to be higher during the second fruiting period. MC treatments significantly increased the N fraction in the 0- to 30-cm soil layer; N fractions tended to be higher with the MN2 treatment. According to an optimum regression equation, soil fixed ammonium during the first fruiting period and soil microbial biomass N during the second fruiting period had a more significant influence on tomato yield and fruit composition. Overall, application MC at an appropriate rate (MN2: 608 kg N/ha) is a promising approach to achieving high yields and optimum taste, and it offers a more sustainable fertilizer management strategy compared with chemical N fertilization.

Soil nitrogen dynamics following herbicide kill and tillage of manured and unmanured grasslands

2013 ◽  
Vol 93 (2) ◽  
pp. 229-237 ◽  
Author(s):  
Martin H. Chantigny ◽  
J. Douglas MacDonald ◽  
Denis A. Angers ◽  
Philippe Rochette ◽  
Isabelle Royer ◽  
...  
Keyword(s):  
Soil Nitrogen ◽  
Swine Manure ◽  
Nitrogen Dynamics ◽  
Hot Water ◽  
Organic N ◽  
Grassland Soils ◽  
Mineral N ◽  
Liquid Swine Manure ◽  
Soil Nitrogen Dynamics ◽  
Soil Solutions

Chantigny, M. H., MacDonald, J. D., Angers, D. A., Rochette, P., Royer, I. and Gasser, M.-O. 2013. Soil nitrogen dynamics following herbicide kill and tillage of manured and unmanured grasslands. Can. J. Soil Sci. 93: 229–237. Grassland soils accumulate N, which could be lost following land-use change. Adjacent grassland sites, with and without liquid swine manure applied annually for 28 yr, were subdivided and left undisturbed (Control), or killed by herbicides with and without full inversion tillage (FIT) in the autumn or spring. We monitored hot-water extractable organic N (HWEON), and mineral N forms in KCl extractions and soil solutions (tension lysimeters) for 1 yr. Mean soil mineral N increased by 1 to 2.8 g m−2 in the weeks following herbicide kill and FIT of the unmanured soils, and by 2.6 to 3.0 g m−2 in the manured soil. These increases corresponded to declines in soil HWEON (−0.4 to −1.9 g m−2 unmanured site; −2.4 to −4.9 g m−2 manured site), suggesting that HWEON comprised N that is rapidly mineralized following grassland termination. More than 80% of N mineralized in the weeks following termination accumulated as NH4 in the unmanured soils, compared with >70% as NO3 in the manured soils. As a result, more mineral N (mainly NO3) was found in the soil solution of manured soils. Manured grassland soils may represent a high risk of N loss following termination with herbicide in combination with FIT in the autumn, because of the rapid nitrification of mineralized N. For spring FIT, however, the rapid mineralization of soil N may represent a substantial nutrient source to the following crop.

Plant uptake of nitrogen from the organic nitrogen fraction of animal manures: a laboratory experiment

2000 ◽  
Vol 134 (2) ◽  
pp. 159-168 ◽  
Author(s):  
D. R. CHADWICK ◽  
F. JOHN ◽  
B. F. PAIN ◽  
B. J. CHAMBERS ◽  
J. WILLIAMS
Keyword(s):  
N Mineralization ◽  
Organic N ◽  
Pig Slurry ◽  
Mineral N ◽  
N Content ◽  
Total N ◽  
N Supply ◽  
Ammonium N ◽  
Cow Slurry ◽  
N Fractions

Twenty slurries, 20 farmyard manures (FYM) and 10 poultry manures were chemically analysed to characterize their nitrogen (N) fractions and to assess their potential organic N supply. The organic N fraction varied between manure types and represented from 14% to 99% of the total N content. The readily mineralizable N fraction, measured by refluxing with KCl, was largest in the pig FYMs and broiler litters, but on average only represented 7–8% of the total N content. A pot experiment was undertaken to measure N mineralization from the organic N fraction of 17 of these manures. The ammonium-N content of the manures was removed and the remaining organic N mixed with a low mineral N status sandy soil, which was sown with perennial ryegrass (Lolium perenne L.). N offtake was used as a measure of mineralization throughout the 199 day experiment. The greatest N mineralization was measured from a layer manure and a pig slurry, where N offtake represented 56% and 37% of the organic N added, respectively. Lowest (%) N mineralization was measured from a dairy cow slurry (< 2%) and a beef FYM (6%). The mineralization rate was negatively related to the C[ratio ]organic N ratio of the ammonium-N stripped manures (P < 0·01, r = −0·63).

scholarly journals Changes in nitrogen pools in the maize-soil system after urea or straw application to a typical intensive agricultural soil: A 15N tracer study

2020 ◽  
Author(s):  
Jie Zhang ◽  
Ping He ◽  
Dan Wei ◽  
Liang Jin ◽  
Lijuan Zhang ◽  
...  
Keyword(s):  
Rhizosphere Soil ◽  
Bulk Soil ◽  
15N Tracer ◽  
Organic N ◽  
Microbial Biomass N ◽  
Soil System ◽  
Total N ◽  
Available N ◽  
Leaf Stage ◽  
Exogenous Substrate

AbstractA 15N maize pot experiment was conducted to compare the N value of fertilizer alone and fertilizer combined with straw at an equivalent N rate. The four treatments were control (CK), 15N-urea, 15N-urea plus straw, and 15N-straw plus urea. Soil N pools, maize N and their 15N abundance were determined during maize growth. At maturity 26.0% of straw N was assimilated by maize in the urea plus straw treatment. From the eighth leaf stage to maturity, urea plus straw had a significantly (P < 0.05) higher concentration and percentage of exogenous substrate N present as soil total N (TN), particulate organic N (PON), and mineral associated total N (MTN) in bulk and rhizosphere soils than the urea-only treatment. From silking to maturity in the urea plus straw treatment, rhizosphere soil significantly (P < 0.05) increased the percentage of exogenous substrate N present as inorganic N (Inorg-N) and MTN, and significantly (P < 0.05) decreased that present as PON and microbial biomass N (MBN) compared with the bulk soil. From the eighth leaf stage to maturity, rhizosphere soil significantly (P < 0.05) increased the percentage of straw N present as Inorg-N and MTN except for MTN at the silking stage, and significantly decreased (P < 0.05) that present as PON compared with the bulk soil. Overall, straw was an available N source to the crop, and the increase in straw N availability needs to be considered from the interaction of fertilization practices and the crop rhizosphere.

Factors influencing the availability of mineral nitrogen in clay soils of the brigalow (Acacia harpophylla) region of Central Queensland

1992 ◽  
Vol 43 (5) ◽  
pp. 1197
Author(s):  
PR Grace ◽  
IC MacRae ◽  
RJK Myers
Keyword(s):  
Microbial Biomass ◽  
Clay Soils ◽  
Microbial Biomass C ◽  
Microbial Biomass N ◽  
Mineral N ◽  
Available N ◽  
Soil Microbial ◽  
Biomass N ◽  
Chloris Gayana ◽  
Highly Correlated

Microbiological and chemical assays were performed on clay soils from woodland (Acacia harpophylla-Casuarina cristata), grassland (Panicurn maximum var trichoglume-Chloris gayana) and cropland (Vigna mungo) in the brigalow region of Central Queensland. Over a 15 month period, the microbial biomass C in the top 3.5 cm of native brigalow woodland soil was on average 3630 8g C g-l, 50% more than an associated perennial pasture and over 400% more than an annually cropped soil. Microbial biomass N (575 8g N g-l) in woodland soil was on average 41% and 270% higher than in pasture and cropped soils respectively and highly correlated with seasonal soil moisture content. Viable counts of bacteria were consistently lower (average 69.2%) in the 0-3.5 cm and 3.5-7.5 cm strata of woodland soil compared with pasture and annual crop sites. Soil NO-3- N levels increased two fold in the upper 3.5 cm of the woodland site during low rainfall periods. This increase may be attributed to a more efficient distribution of mineral N mediated by the increased presence of a fungal population in this community. Leaching may also play a significant role in the distribution of plant available N in the brigalow region as suggested by the inverse relationship N = 54.11-0.67 R (P<0.01), where N is soil NO-3-N (8g N g-l) and R is rainfall in the preceding 3 month period (mm month-1).

scholarly journals Subcritical water extraction to isolate kinetically different soil nitrogen fractions

2013 ◽  
Vol 10 (11) ◽  
pp. 7435-7447 ◽  
Author(s):  
S. Sleutel ◽  
M. A. Kader ◽  
K. Demeestere ◽  
C. Walgraeve ◽  
J. Dewulf ◽  
...  
Keyword(s):  
Bonding Strength ◽  
N Mineralization ◽  
Subcritical Water ◽  
Water Extraction ◽  
Organic N ◽  
Soil N ◽  
Subcritical Water Extraction ◽  
Available N ◽  
Upland Soils ◽  
N Fractions

Abstract. Soil organic N is largely composed of inherently biologically labile proteinaceous N and its persistence in soil is mainly explained by stabilization through binding to minerals and other soil organic matter (SOM) components at varying strengths. In order to separate kinetically different soil N fractions we hypothesize that an approach which isolates soil N fractions on the basis of bonding strength is required, rather than employing chemical agents or physical methods. We developed a sequential subcritical water extraction (SCWE) procedure at 100, 150 and 200 °C to isolate SOM fractions. We assessed these SCWE N fractions as predictors for aerobic and anaerobic N mineralization measured from 25 paddy soil cores in incubations. SCWE organic carbon (SCWE OC) and N (SCWE N) increased exponentially with the increase of temperature and N was extracted preferentially over OC. The efficiency of SCWE and the selectivity towards N were both lower in soils with increasingly reactive clay mineralogy. Stepwise linear regression found no relations between the SCWE fractions and the anaerobic N mineralization rate but instead with pH and a model parameter describing the temperature dependency of SCWE extraction. Both were linked to texture, mineralogy and content of pedogenic oxides, which suggests an indirect relation between anaerobic NH4+ release and these edaphic soil factors. N mineralization appeared to be largely decoupled from SOM quantity and quality. From the present study on young paddy soils low in pedogenic oxides and with high fixed NH4+ content we cannot infer the performance of SCWE to isolate bio-available N in more developed upland soils. There may be potential to separate kinetically different SOM pools from upland soils because 1° for aerobic N mineralization at 100–150 °C SCWE N was the best predictor; and 2° SCWE selectively extracted N over C and this preference depended on the mineralogical composition. Hence N fractions differing in bonding strength with minerals or SOM might be isolated at different temperatures, and specifically this association has frequently been found a prominent stabilization mechanism of N in temperate region cropland soils.

scholarly journals Effects of different groundcover matters on nutrient availability in an integrated apple orchard in Eastern-Hungary

2010 ◽  
pp. 21-25
Author(s):  
Péter Tamás Nagy
Keyword(s):  
Nutrient Availability ◽  
Apple Orchard ◽  
The Other ◽  
Mineral N ◽  
Available N ◽  
Soil Layers ◽  
P Content ◽  
Set Up ◽  
The One ◽  
N Fractions

The aim of our study is to examine the effects of different groundcover methods on nutrient availability and uptake of apple orchard. Theexperiment was carried out at the orchard of TEDEJ Rt. at Hajdúnánás-Tedej, in Eastern Hungary. The orchard was set up on lowland chernozem soil in the Nyírség region. It was established in the autumn of 1999, using Idared cultivar grafted on MM106 rootstocks at a spacing of 3.8 x 1.1 m.The applied treatments were divided into two groups according to origins and effects. On the one hand, different livestock manures (cow,horse and pig), on the other hand different mulch-matters (straw, pine bark mulch, black foil) were used. The different manures and mulcheswere applied on the surface to test the effectiveness of these materials.The effectiveness of manure treatments was higher than the other treatments on AL soluble P content of soil. Mostly the manure treatmentsincreased the AL soluble K of soil. Our all treatments increased 0.01 M CaCl2 soluble NO3 - -N content of the examined soil layers. The effectof manure treatments was the highest. From the results it was evident that the amount of easily soluble organic nitrogen fraction distributedmore homogeneously than the other mineral N fractions examined.Our results can be summarized as follows:1. Our results pointed out that the used ground covering matters divided into several categories regarding its effect.2. The available N, P and K contents of soil were mostly increased by applying manures.3. The effectiveness of straw, mulch and mostly black foil was lower.4. Differences were found between nutrient supplying treatments and the treatments which did not supply nutrients.

scholarly journals Green Manuring Effect on Changes of Soil Nitrogen Fractions, Maize Growth, and Nutrient Uptake

Agronomy ◽  
2018 ◽  
Vol 8 (11) ◽  
pp. 261 ◽  
Author(s):  
Lu Yang ◽  
Jinshun Bai ◽  
Jia Liu ◽  
Naohua Zeng ◽  
Weidong Cao
Keyword(s):  
Green Manure ◽  
N Uptake ◽  
Partial Substitution ◽  
Organic N ◽  
Soil N ◽  
Path Modeling ◽  
Mineral N ◽  
N Accumulation ◽  
Maize Growth ◽  
N Fractions

Green manure is a promising, at least partial, substitution for chemical fertilizer in agriculture, especially for nitrogen (N), which in soil can be radically changed by exogenous input. However, it is not well understood how, after green manure incorporation, soil N changes coordinate with crop N uptake and consequently contribute to fertilizer reduction in a maize–green manure rotation. A four-year field study was performed consisting of (1) control, no fertilization; (2) F100, recommended inorganic fertilization alone; (3) G, green manure incorporation alone; (4) F70 + G (70% of F100 plus G); (5) F85 + G; and (6) F100 + G. The results show that treatments with 15–30% reduction of inorganic fertilizer (i.e., F70 + G and F85 + G) had similar grain yield, dry matter (DM) accumulation, and N uptake as F100 treatment. F100 + G maize had 17% greater DM and 15% more N uptake at maturity relative to F100. Of the five soil N fractions examined, dissolved organic N (DON) and mineral N (Nmin) explained over 70% of the variation of maize DM and N accumulation. Partial least squares path modeling further revealed that soil N fractions had positive indirect effects on DM production through N uptake, which might be coordinated with improved DON and Nmin status at both early and mid-late stages of maize growth. Overall, the results highlight enhanced maize production with reduced fertilizer inputs based on green manure incorporation in temperate regions.

BIOLOGICAL PROPERTIES OF SOME PRINCE EDWARD ISLAND SOILS: RELATIONSHIP BETWEEN MICROBIAL BIOMASS NITROGEN AND MINERALIZABLE NITROGEN

1987 ◽  
Vol 67 (2) ◽  
pp. 333-340 ◽  
Author(s):  
M. R. CARTER ◽  
J. A. MACLEOD
Keyword(s):  
Microbial Biomass ◽  
N Mineralization ◽  
Prince Edward Island ◽  
Organic N ◽  
Microbial Biomass N ◽  
Soil N ◽  
Mineral N ◽  
Organic C ◽  
Mineralization Potential ◽  
N Mineralization Potential

The mineral N flush, a measure of microbial biomass N, and the N mineralization potential (No) were determined in eight representative agricultural soils (Humo-Ferric Podzols and Gray Luvisols) of Prince Edward Island. The acidic (pH 5.0–5.8) soils, varying in texture from loam to loamy sand had an organic C range of 0.75–2.74%. Both mineral N flush (4–38 μg N g−1 soil) and the percentage soil organic N in the mineral N flush (0.4–2.0%) were relatively low compared to other studies. This observation was related to the generally low pH range of these soils. Potentially mineralizable soil N (No) ranged from 44 to 247 μg N g−1 and accounted for 4.5–13.3% of the total soil organic N. The No was closely related to the mineral N flush (r2 = 0.94) but poorly related to percent organic matter (r2 = 0.26) or organic N (r2 = 0.38). The results indicate that for these soils of similar properties, with low levels of residual mineral N, the mineral N flush could be utilized as an indirect measure of the soil N mineralization potential. Key words: Biomass C, mineral N flush, N mineralization potential, Podzolic soil, Luvisolic soil

scholarly journals Effects of two wood-based biochars on the fate of added fertilizer nitrogen—a 15N tracing study

2021 ◽  
Author(s):  
Subin Kalu ◽  
Gboyega Nathaniel Oyekoya ◽  
Per Ambus ◽  
Priit Tammeorg ◽  
Asko Simojoki ◽  
...  
Keyword(s):  
Plant Uptake ◽  
Plant Biomass ◽  
Application Rate ◽  
Control Treatment ◽  
Organic N ◽  
N Leaching ◽  
Soil N ◽  
Mineral N ◽  
Total N ◽  
Application Rates

AbstractA 15N tracing pot experiment was conducted using two types of wood-based biochars: a regular biochar and a Kon-Tiki-produced nutrient-enriched biochar, at two application rates (1% and 5% (w/w)), in addition to a fertilizer only and a control treatment. Ryegrass was sown in pots, all of which except controls received 15N-labelled fertilizer as either 15NH4NO3 or NH415NO3. We quantified the effect of biochar application on soil N2O emissions, as well as the fate of fertilizer-derived ammonium (NH4+) and nitrate (NO3−) in terms of their leaching from the soil, uptake into plant biomass, and recovery in the soil. We found that application of biochars reduced soil mineral N leaching and N2O emissions. Similarly, the higher biochar application rate of 5% significantly increased aboveground ryegrass biomass yield. However, no differences in N2O emissions and ryegrass biomass yields were observed between regular and nutrient-enriched biochar treatments, although mineral N leaching tended to be lower in the nutrient-enriched biochar treatment than in the regular biochar treatment. The 15N analysis revealed that biochar application increased the plant uptake of added nitrate, but reduced the plant uptake of added ammonium compared to the fertilizer only treatment. Thus, the uptake of total N derived from added NH4NO3 fertilizer was not affected by the biochar addition, and cannot explain the increase in plant biomass in biochar treatments. Instead, the increased plant biomass at the higher biochar application rate was attributed to the enhanced uptake of N derived from soil. This suggests that the interactions between biochar and native soil organic N may be important determinants of the availability of soil N to plant growth.

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