Abstract:A b s t r a c t. The objectives of the research were to: fulfil the preliminary assessment of the sensitivity of the soil, water, atmosphere, and plant and denitrification and decomposition models to variations of climate variables based on the existing soil database; validate the soil, water, atmosphere, and plant and denitrification and decomposition modelled outcomes against measured records for soil temperature and water content. The statistical analyses were conducted by the sensitivity analysis, Nash-Sut… Show more
“…The Spearman's rank correlation coefficients for relationships between soil temperature and air temperature ranged from 0.78 to 0.82 (at P < 0.05) and from 0.73 to 0.76 (at P < 0.05) between treatments of CT and RT, respectively. These results also agreed with data obtained by Balashov et al (2014) and Licht and Al-Kaisi (2005).…”
Section: Resultssupporting
confidence: 92%
“…Water-retention curves of undisturbed soil samples were measured by a pressure-plate apparatus at water potentials of −5, −20, −50, −100 and − 300 kPa (Soil Survey Laboratory Methods Manual 1996). A saturated hydraulic conductivity of undisturbed soil samples was measured using the lab method as published in Antal and Igaz (2006).…”
Greenhouse gases such as N 2 O and CO 2 are formed in microbiological processes of nitrification and denitrification and also governed by microbial decomposition of soil organic matter (SOM) plant residues. A key factors influencing these processes are temperature and soil moisture. Therefore the objectives of this study were to: (1) evaluate the seasonal variations in SOM content, temperature, water-filled pore space (WFPS) and mineral nitrogen content under conventional tillage (CT) and reduced tillage (RT) system, and (2) assess the direct CO 2 and N 2 O emissions associated with the seasonal variations in the soil properties under both tillage systems. An experiment was carried out in a randomized blocks with two different tillage system: CT and RT in a Haplic Luvisol (loamy) covering the growing season of spring barley. Each block included treatments: no mineral fertilizers; mineral fertilizers; mineral fertilizers plus plant residues. Overall, the SOM content and temperatures were insignificantly higher in the plough layers of RT than CT during the entire period of study. Soil moisture content (SMC) and WFPS were insignificantly higher in CT than RT. The application of mineral fertilizers resulted in a significant increase of mean NO 3 − concentrations only in the plough layers of CT. SMC was a stronger driving factor of mean daily CO 2 emissions in all treatments, while variations in soil temperatures and SMC were jointly responsible for changes in mean daily N 2 O emissions in all the treatments of CT and RT. The postponed highest peaks of mean daily N 2 O emissions from RT were observed under aerobic soil conditions several days after the heavy rainstorm. The cumulative CO 2 and N 2 O fluxes were insignificantly higher from CT than RT over the entire period of study.
“…The Spearman's rank correlation coefficients for relationships between soil temperature and air temperature ranged from 0.78 to 0.82 (at P < 0.05) and from 0.73 to 0.76 (at P < 0.05) between treatments of CT and RT, respectively. These results also agreed with data obtained by Balashov et al (2014) and Licht and Al-Kaisi (2005).…”
Section: Resultssupporting
confidence: 92%
“…Water-retention curves of undisturbed soil samples were measured by a pressure-plate apparatus at water potentials of −5, −20, −50, −100 and − 300 kPa (Soil Survey Laboratory Methods Manual 1996). A saturated hydraulic conductivity of undisturbed soil samples was measured using the lab method as published in Antal and Igaz (2006).…”
Greenhouse gases such as N 2 O and CO 2 are formed in microbiological processes of nitrification and denitrification and also governed by microbial decomposition of soil organic matter (SOM) plant residues. A key factors influencing these processes are temperature and soil moisture. Therefore the objectives of this study were to: (1) evaluate the seasonal variations in SOM content, temperature, water-filled pore space (WFPS) and mineral nitrogen content under conventional tillage (CT) and reduced tillage (RT) system, and (2) assess the direct CO 2 and N 2 O emissions associated with the seasonal variations in the soil properties under both tillage systems. An experiment was carried out in a randomized blocks with two different tillage system: CT and RT in a Haplic Luvisol (loamy) covering the growing season of spring barley. Each block included treatments: no mineral fertilizers; mineral fertilizers; mineral fertilizers plus plant residues. Overall, the SOM content and temperatures were insignificantly higher in the plough layers of RT than CT during the entire period of study. Soil moisture content (SMC) and WFPS were insignificantly higher in CT than RT. The application of mineral fertilizers resulted in a significant increase of mean NO 3 − concentrations only in the plough layers of CT. SMC was a stronger driving factor of mean daily CO 2 emissions in all treatments, while variations in soil temperatures and SMC were jointly responsible for changes in mean daily N 2 O emissions in all the treatments of CT and RT. The postponed highest peaks of mean daily N 2 O emissions from RT were observed under aerobic soil conditions several days after the heavy rainstorm. The cumulative CO 2 and N 2 O fluxes were insignificantly higher from CT than RT over the entire period of study.
“…Several studies have investigated the effectiveness of the DNDC model to access and predict GHG emissions and crop yields under different management practices and emissions scenarios in wheat fields and have demonstrated that the simulated results of DNDC are helpful in choosing best management practices to decrease nitrate leaching and N 2 O and NO emissions (Ludwig et al, 2011;Smith et al, 2013;Cui et al, 2014;Sansoulet et al, 2014). In addition, DNDC is also widely used and compared with other models to investigate the influence of future climate change and the application of advanced agricultural management measures to achieve good application results in barley fields (Abdalla et al, 2011;Smith et al, 2012;Cardenas et al, 2013;Balashov et al, 2014;Deng et al, 2015).…”
“…In terms of preferential flow, it cannot be limited by macropores as irregular wetting patterns within the soil matrices can also affect water flow (DEKKER & RITSEMA, 1996). Water and solute transport in heterogeneous and variably saturated soil matrices have been studied in the past several decades by numerous researchers (BALASHOV et al, 2014;HARDELAUF et al, 2007;HARTER & ZHANG, 1999;HOREL et al, 2015;TWARAKAVI et al, 2010). Preferential flow can greatly influence both water and solute movement through the soil, as it was found by several studies (e.g.…”
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