Nitrogen Mineralization in Texturally Contrasting Soils Subjected to Different Organic Amendments under Semi-Arid Climates

Nitrogen (N) is the prime essential nutrient for agricultural productivity, and its deficiency is overcome through the application of fertilizers. However, the rate of N mineralization from organic N sources is an important process to be monitored for efficient N use and sustainable agricultural man...

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Main Authors: Hafiz Muhammad Rashad Javeed, Mazhar Ali, Nitasha Kanwal, Iftikhar Ahmad, Aftab Jamal, Rafi Qamar, Ali Zakir, Hina Andaleeb, Raheela Jabeen, Emanuele Radicetti, Roberto Mancinelli
Format: Article
Language:English
Published: MDPI AG 2023-04-01
Series:Land
Subjects:
Online Access:https://www.mdpi.com/2073-445X/12/5/989
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author Hafiz Muhammad Rashad Javeed
Mazhar Ali
Nitasha Kanwal
Iftikhar Ahmad
Aftab Jamal
Rafi Qamar
Ali Zakir
Hina Andaleeb
Raheela Jabeen
Emanuele Radicetti
Roberto Mancinelli
author_facet Hafiz Muhammad Rashad Javeed
Mazhar Ali
Nitasha Kanwal
Iftikhar Ahmad
Aftab Jamal
Rafi Qamar
Ali Zakir
Hina Andaleeb
Raheela Jabeen
Emanuele Radicetti
Roberto Mancinelli
author_sort Hafiz Muhammad Rashad Javeed
collection DOAJ
description Nitrogen (N) is the prime essential nutrient for agricultural productivity, and its deficiency is overcome through the application of fertilizers. However, the rate of N mineralization from organic N sources is an important process to be monitored for efficient N use and sustainable agricultural management. Laboratory incubation studies were conducted for a period of 150 days to measure N mineralization (N<sub>min</sub>) from different organic amendments (OA) in texturally contrasting soils collected at three locations: SL1 (Bahawalpur, sandy loam), SL2 (Bahawalnagar, sandy loam), and SL3 (Rahim Yar Khan, sandy clay loam). A second study was also carried out for 25 days to monitor pH dynamics and ammonia volatilization from the same three OA-treated soils. The results showed that there was no significant difference in net N<sub>min</sub> between the soils for poultry manure (PMO) and feather meal (FMO), even if there was a substantial N<sub>min</sub> observed for PMC + FMO followed by poultry manure compost (PMC) at SL2 and SL3 soils. This might have happened due to higher microbial biomass carbon (257), nitrogen (61), fungal colonization (88 cfu g<sup>−1</sup> soil) and enzyme activity (79) in SL3 soil receiving PMC + FMO after 150 days of incubation. However, the first-order kinetic model (R<sup>2</sup> = 0.86–0.95) better explained the N<sub>min</sub> in all three soils amended with OA (PMC + FMO). The soil pH had more pronounced effects on N<sub>min</sub> in all three soils. A non-significant amount of ammonia volatilization was recorded regardless of the initial pH, buffering capacity, and texture variability of the soils. Further study on the particle size of OA and soil pH is warranted to determine the actual effect of OA on N<sub>min</sub>.
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spelling doaj.art-c959aa0880c04e1a8ba0114756bfe8472023-11-18T02:06:14ZengMDPI AGLand2073-445X2023-04-0112598910.3390/land12050989Nitrogen Mineralization in Texturally Contrasting Soils Subjected to Different Organic Amendments under Semi-Arid ClimatesHafiz Muhammad Rashad Javeed0Mazhar Ali1Nitasha Kanwal2Iftikhar Ahmad3Aftab Jamal4Rafi Qamar5Ali Zakir6Hina Andaleeb7Raheela Jabeen8Emanuele Radicetti9Roberto Mancinelli10Department of Environmental Sciences, COMSATS University Islamabad, Vehari Campus, Vehari 61100, PakistanDepartment of Environmental Sciences, COMSATS University Islamabad, Vehari Campus, Vehari 61100, PakistanDepartment of Environmental Sciences, COMSATS University Islamabad, Vehari Campus, Vehari 61100, PakistanDepartment of Environmental Sciences, COMSATS University Islamabad, Vehari Campus, Vehari 61100, PakistanDepartment of Soil and Environmental Sciences, Faculty of Crop Production Sciences, The University of Agriculture, Peshawar 25130, PakistanDepartment of Agronomy, Faculty of Agriculture, College of Agriculture, University of Sargodha, Sargodha 40100, PakistanDepartment of Environmental Sciences, COMSATS University Islamabad, Vehari Campus, Vehari 61100, PakistanDepartment of Biochemistry, Bahauddin Zakariya University, Multan 60000, PakistanDepartment of Biochemistry and Biotechnology, The Women University Multan, Multan 66000, PakistanDepartment of Chemical, Pharmaceutical and Agricultural Sciences (DOCPAS), University of Ferrara, 44121 Ferrara, ItalyDepartment of Agricultural and Forestry Sciences (DAFNE), University of Tuscia, 01100 Viterbo, ItalyNitrogen (N) is the prime essential nutrient for agricultural productivity, and its deficiency is overcome through the application of fertilizers. However, the rate of N mineralization from organic N sources is an important process to be monitored for efficient N use and sustainable agricultural management. Laboratory incubation studies were conducted for a period of 150 days to measure N mineralization (N<sub>min</sub>) from different organic amendments (OA) in texturally contrasting soils collected at three locations: SL1 (Bahawalpur, sandy loam), SL2 (Bahawalnagar, sandy loam), and SL3 (Rahim Yar Khan, sandy clay loam). A second study was also carried out for 25 days to monitor pH dynamics and ammonia volatilization from the same three OA-treated soils. The results showed that there was no significant difference in net N<sub>min</sub> between the soils for poultry manure (PMO) and feather meal (FMO), even if there was a substantial N<sub>min</sub> observed for PMC + FMO followed by poultry manure compost (PMC) at SL2 and SL3 soils. This might have happened due to higher microbial biomass carbon (257), nitrogen (61), fungal colonization (88 cfu g<sup>−1</sup> soil) and enzyme activity (79) in SL3 soil receiving PMC + FMO after 150 days of incubation. However, the first-order kinetic model (R<sup>2</sup> = 0.86–0.95) better explained the N<sub>min</sub> in all three soils amended with OA (PMC + FMO). The soil pH had more pronounced effects on N<sub>min</sub> in all three soils. A non-significant amount of ammonia volatilization was recorded regardless of the initial pH, buffering capacity, and texture variability of the soils. Further study on the particle size of OA and soil pH is warranted to determine the actual effect of OA on N<sub>min</sub>.https://www.mdpi.com/2073-445X/12/5/989poultry manurecompostingincubationpHammonia volatilization
spellingShingle Hafiz Muhammad Rashad Javeed
Mazhar Ali
Nitasha Kanwal
Iftikhar Ahmad
Aftab Jamal
Rafi Qamar
Ali Zakir
Hina Andaleeb
Raheela Jabeen
Emanuele Radicetti
Roberto Mancinelli
Nitrogen Mineralization in Texturally Contrasting Soils Subjected to Different Organic Amendments under Semi-Arid Climates
Land
poultry manure
composting
incubation
pH
ammonia volatilization
title Nitrogen Mineralization in Texturally Contrasting Soils Subjected to Different Organic Amendments under Semi-Arid Climates
title_full Nitrogen Mineralization in Texturally Contrasting Soils Subjected to Different Organic Amendments under Semi-Arid Climates
title_fullStr Nitrogen Mineralization in Texturally Contrasting Soils Subjected to Different Organic Amendments under Semi-Arid Climates
title_full_unstemmed Nitrogen Mineralization in Texturally Contrasting Soils Subjected to Different Organic Amendments under Semi-Arid Climates
title_short Nitrogen Mineralization in Texturally Contrasting Soils Subjected to Different Organic Amendments under Semi-Arid Climates
title_sort nitrogen mineralization in texturally contrasting soils subjected to different organic amendments under semi arid climates
topic poultry manure
composting
incubation
pH
ammonia volatilization
url https://www.mdpi.com/2073-445X/12/5/989
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