Studies on the Contents and Amounts of Microelements Taken Up by Meadow Sward in Conditions of Long-Term and Diversified Mineral Fertilization as to the Sward Fodder Value

2008 ◽  
Vol 23 (1) ◽  
pp. 1-15
Author(s):  
Krzysztof Gondek ◽  
Michał Kopeć
FLORESTA ◽  
2019 ◽  
Vol 49 (3) ◽  
pp. 485
Author(s):  
Lívia Mara Lima Goulart ◽  
Marianne Fidalgo de Faria ◽  
Grasiela Spada ◽  
Thiago Tássio de Souza Silva ◽  
Iraê Amaral Guerrini

The use of sewage sludge in agriculture and recovery of degraded areas has been shown as a promising alternative for its final destination. Studies on micronutrient levels after sludge application are necessary to avoid soil contamination at toxic levels. The objective of this work was to verify the micronutrient contents in the soil profile and pH, up to one-meter-deep, nine years after the application of sewage sludge and planting of native species of the Atlantic Forest. The experiment was implemented in a degraded Quartzeneic Neosol and conducted in randomized blocks with four replicates and eight treatments, consisting of six doses of sewage sludge (0, 2.5, 5, 10, 15 and 20 Mg ha-1, with supplementation of potassium due to low concentration in the residue), besides the control treatment, mineral fertilization and only potassium supplementation. After nine years, the contents of all micronutrients evaluated presented a significant response to the application of the treatments, and the application of sewage sludge provided an increase in their contents. Soil pH remained stable at sites receiving mineral fertilization and potassium supplementation. Only manganese and zinc showed mobility in the soil profile. The application of sewage sludge in degraded soil increases the micronutrient content and decreases its movement in the soil profile, and the application of the maximum dose of the residue does not provide toxic levels of these elements in the soil in the long term.


2021 ◽  
Author(s):  
Xue Li ◽  
Qiuxiang Wen ◽  
Shiyu Zhang ◽  
Na Li ◽  
Jinfeng Yang ◽  
...  

Abstract Aims The objectives of this study were to examine the long-term substitution of mineral phosphorus (P) fertilizers with manure (M) plus nitrogen (N) fertilizers and how they affect the forms of P that occur in soil, soil P distribution, and plant growth.Methods We used a solution of 31P nuclear magnetic resonance (31P-NMR) spectroscopy to study the correlations between long-term fertilization regimes and the forms of P that occur at different soil depths. Then we investigated yield, plant growth, and soil properties.Results A 40-year field experiment showed that the use of M + N fertilizers can significantly improve plant growth and yield. The proportion of organic P in the 20-40 cm soil layer was significantly increased by long-term M fertilization. The concentrations of various forms of P (orthophosphate, pyrophosphate, diesters, monoesters, and total inositol hexakisphosphate, IHP) in topsoil increased significantly with the combination of M with N + P mineral fertilization. The addition of M greatly increased the stereoisomers of IHP (myo-IHP, scyllo-IHP, neo-IHP, and D-chiro-IHP) and the proportion and concentration of corrected diesters. There were no significant differences in the pyrophosphate contents of the 40-60 cm soil layer according to fertilization type and year of fertilization. There were also no significant differences in IHP stereoisomers and diesters according to fertilization year. The P forms that contributed to corn yield were orthophosphate, diester, and IHP. Further, pyrophosphate made no significant contribution to corn growth. Conclusions Over the long-term, pig manure can significantly increase the amount of orthophosphate that is directly absorbed by crops and the amount of IHP stereoisomers that can be used by plants. Orthophosphate and IHP are the two key factors that have a positive effect on plant growth.


Author(s):  
С.А. Запивалов

В Центральном районе Нечернозёмной зоны в 2018–2020 годах изучалось шесть систем ведения долголетнего сенокоса. В среднем за годы исследования применение техногенной системы позволило получить 3,86 т/га сухого вещества (СВ), применение интегрированной — 5,08 т/га СВ, техногенно-органической — 4,75–5,16 т/га СВ, техногенно-минеральной экстенсивной — 3,97–7,13 т/га СВ, техногенно-минеральной интенсивной — 6,60–8,85 т/га СВ, комбинированной — 7,03–7,25 т/га СВ. Существенное влияние на урожайность оказывали погодные условия. В засушливый год не был сформирован полноценный 2-й укос, что не позволило травостоям реализовать потенциал продуктивности. Более эффективно ограниченный запас влаги в почве использовался в техногенно-минеральной интенсивной системе. В условиях достаточной влагообеспеченности был получен полноценный второй укос, составляющий 30–50% сбора СВ за сезон. При улучшении условий увлажнения урожайность наиболее заметно повышалась при применении техногенно-минеральной интенсивной системы. Отмечена высокая экономическая эффективность применения всех изучаемых систем за счёт длительного использования травостоя. В зависимости от технологии рентабельность производства корма составляла 74–220%, себестоимость 1 корм. ед. — 3,12–5,75 руб. Для получения 65,2–88,0 ГДж, 5,1–6,8 тыс. корм. ед. и 781–1153 кг сырого протеина с 1 га на суходольных лугах Центрального района Нечернозёмной зоны рекомендуется применять техногенно-минеральную интенсивную систему ведения сенокоса. В случае недостаточной обеспеченности хозяйств материально-техническими ресурсами рекомендуются техногенная, интегрированная, техногенно-органическая и техногенно-минеральная экстенсивная системы ведения, позволяющие поддерживать высокое участие бобовых видов в травостое, что обеспечивает использование биологического источника азота и позволяет получить с 1 га сенокосных угодий 39,0–56,7 ГДж, 3,1–4,5 тыс. корм. ед. и 462–688 кг сырого протеина. Six management systems for long-term hayfields were tested in the Central Non-Chernozem region in 2018–2020. Without fertilization 3.86 t ha-1 of dry matter (DM) was obtained. Integrated farming resulted in 5.08 t DM ha-1, application of organic fertilizers — 4.75–5.16 t DM ha-1, extensive farming with mineral fertilization — 3.97–7.13 t DM ha-1, intensive farming with mineral fertilization — 6.60–8.85 t DM ha-1, combined management system — 7.03–7.25 t DM ha-1. Weather significantly affected crop productivity. Under drought grasses showed poor growth after the first cut leading to low yield. Intensive farming with mineral fertilization allowed more effective use of soil water resources. Sufficient water availability positively affected grass growth after the first cut resulting in 30–50% of DM yield for a season. The best performance was observed under intensive farming with mineral fertilization. All the management systems provided high economic efficiency due to a long-term cultivation of swards. Payback amounted to 74–220%, prime cost of 1 feed unit — 3.12–5.75 rubles. Intensive farming with mineral fertilization was recommended in order to obtain 65.2–88.0 GJ, 5.1–6.8 thousand feed units and 781–1153 kg of crude protein from 1 ha. In case of insufficient material and technical resources other above-mentioned systems can be used, except for the combined one. These management systems maintained high proportion of legumes in swards, an effective mean to obtain nitrogen via nitrogen-fixing bacteria. As a result, swards yielded 39.0–56.7 GJ, 3.1–4.5 thousand feed units and 462–688 kg of crude protein from 1 ha.


2010 ◽  
Vol 58 (Supplement 1) ◽  
pp. 35-40
Author(s):  
S. Hoffmann ◽  
K. Berecz ◽  
S. Simon

Increasing doses of farmyard manure (FYM) or equivalent mineral NPK fertilizers and their combinations were analysed in a crop rotation with potato, maize and winter wheat with special regard to their long-term influence on soil fertility. The yield-increasing capacity of FYM doses was only 82%, as compared to the equivalent amount of mineral NPK. Fairly high N release (50.9 kg ha −1 ) could be observed on the unfertilized plots. Great differences in N utilization were recorded, depending on the form and dose of fertilizers. The average N utilization from FYM was only 29.3%, while that of the equivalent fertilizer application was 49.8%. The lowest soil reactions were observed without fertilization and at the highest NPK doses. Negative N balances generally resulted in low soil organic matter content. FYM and equivalent NPK fertilizers had a similar influence on the ammonium lactate (AL)-extractable K 2 O content of the soil, while an increase in the AL-P 2 O 5 content could be observed in the case of mineral fertilization.


Agronomy ◽  
2019 ◽  
Vol 9 (12) ◽  
pp. 784 ◽  
Author(s):  
Waqas Ahmed ◽  
Kailou Liu ◽  
Muhammad Qaswar ◽  
Jing Huang ◽  
Qinghai Huang ◽  
...  

Elevated mineral fertilization may change the composition and increase the availability of soil phosphorus (P) in subtropical paddy soils and thus affect long-term plant growth. However, an understanding of the response of soil P fractions to long-term nitrogen, phosphorus and potassium (NPK) additions remains elusive. This study aimed to explore the responses of soil P-fractions and their mobility to different long-term chemical fertilization rates under a double rice cropping system. The rates of nitrogen (N), phosphorus (P), and potassium (K) in the low NPK treatment (LNPK) were 90, 45, and 75 kg ha−1 year−1, respectively, and in the high NPK treatment (HNPK), they were 180, 90, and 150 kg ha−1 year−1, respectively. The results showed that the concentrations of soil organic matter (SOM), total P, Olsen P, total N, and mineral N were remarkably increased under HNPK by 17.46%, 162.66%, 721.16%, 104.42%, and 414.46%, respectively, compared with those under control (CT). Compared to the CT P fractions, HNPK increased the labile P fractions (i.e., NaHCO3-Pi and NaHCO3-Po) by 322.25% and 83.53% and the moderately labile P fractions (i.e., NaOH-Pi, NaOH-Po and HCl. dil. Pi) by 163.54%, 183.78%, and 3167.25% respectively, while the non-labile P was decreased by the HNPK addition. P uptake and grain yield were increased by LNPK and HNPK by 10.02% and 35.20%, respectively, compared with CT. P use efficiency indices were also higher under HNPK than under LNPK. There was a strong positive relationship between grain yield and P use efficiency (R2 = 0.97). A redundancy analysis (RDA) showed a strong correlation between soil chemical properties and the labile and moderately labile P pools. Structural equation modeling (SEM) revealed that SOM, mineral N, and available P strongly control the labile P pool. In conclusion, NPK additions under the paddy soils significantly influences the soil P fractions. The soil P dynamics and the mechanisms governing the interactions between plants and soil nutrients are clearly explained in this study.


2021 ◽  
Vol 123 ◽  
pp. 126219
Author(s):  
Josef Hakl ◽  
Eva Kunzová ◽  
Štěpánka Tocauerová ◽  
Ladislav Menšík ◽  
Marie Mrázková ◽  
...  

2011 ◽  
Vol 52 (No. 2) ◽  
pp. 55-63 ◽  
Author(s):  
S.S. Gonet ◽  
B. Debska

The objective of the study was to evaluate the effects of long-term fertilization of a sandy soil with differentiated doses of cattle slurry as well as its after-effect action on the possibilities of migration of dissolved organic carbon (DOC) and dissolved nitrogen (DNt) down to deeper layers of the soil profile. DOC and DNt were extracted with borate buffer and 0.004M CaCl<sub>2</sub> solution. Evaluation of effects of cattle slurry on the content of DOC and DNt was done in comparison with mineral fertilization. It was shown that the use of cattle slurry in the doses of 100 and 200&nbsp;m<sup>3</sup>/ha caused a significant increase of labile organic matter in the 0&ndash;25 and 25&ndash;50 cm layers of soil. As compared with mineral fertilization the application of slurry increased also the amounts of extracted DNt, but only in the surface layer. The DNt content in the deeper soil horizons did not depend on the kind of fertilization. Concentrations of DOC and DNt in the extracts depended not only on their content in soil but it was also modified substantially by the extractant used.


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