This study explores agronomic management (AM) effects on soil parameters under diverse conditions. Investigating tillage practices (TP), nutrient management (NM), crop rotation (CR), organic matter (OM), irrigation management (IM), and mulching (MS), it aims to reveal impacts on soil productivity, nutrient availability, microbial activity, and overall health. Varied TP affect soil quality through compaction, porosity, and erosion risk. Proper NM is vital for nutrient cycling, preventing imbalances and acidification. CR disrupts pest cycles, reduces weed pressure, and boosts nutrient recycling. OM management enhances soil quality by influencing organic carbon, nutrient availability, pH, fertility, and water retention. Optimizing IM regulates soil water content without inducing waterlogging. MS contributes to OM content, nutrient retention, soil structure, and temperature-moisture regulation, benefiting soil biota, aggregation, soil health and agricultural productivity. The review emphasizes integrated nutrient, CR, and OM management's positive impact on fertility and microbial activity. Different TP and IM variations impact soil health and crop production. Judicious implementation of these practices is essential for sustainable agriculture. This synthesis identifies uncertainties and proposes research directions for optimizing productivity while ensuring environmental sustainability. Ongoing inquiry can guide a balanced approach between yields and resilient soil stewardship for future generations.

To evaluate the response of saffron to animal manure, and biological and chemical fertilizer in an arid climate, an experiment was performed as split plots based on a randomized complete blocks design with three replications during three consecutive crop growth seasons (2015-2018) at the Research Farm of University of Gonabad, Iran. The experimental treatments included application (60 t ha^-1) and non-application (control) of manure as the main plot and the use of biosulfur (5 kg ha^-1), biophosphate (3 L ha^-1), nitroxin (3 L ha^-1), chemical fertilizer (150, 100, and 100 kg ha^-1 of urea, triple superphosphate, and potassium sulfate, respectively), and no fertilizer application (control) as the sub-plot. The results showed a highly significant response of the quantitative traits of saffron to the application of manure, which increased the leaf, flower, and corm indices of saffron by a mean of 15.1-35.7% than control. The interaction effect of manure with biological and chemical fertilizers for leaf, flower, and weeds indices of saffron was significant. There was no significant difference between the interaction treatments of manure and chemical fertilizer with nitroxin and biophosphorus fertilizers in most of the mentioned traits in the three experiment years. The simultaneous application of these fertilizers increased the average by about 60, 105, 135, 110, 165, and 55% of the leaf dry weight, the number of flowers, fresh flower yield, dry flower yield, dry stigma yield, and weed dry weight of saffron, respectively as compared to control. There was no significant difference between the chemical fertilizer with nitroxin or biophosphate in terms of the effect on the traits related to saffron corm so the use of these fertilizers, as compared to control, increased replacement corm weight, replacement corm size, and bud number per corm by, respectively, about 35, 60, and 40% on average. The chemical and biological fertilizers improved the content of crocin, picrocrocin, and safranal of saffron stigma. The best results were obtained from the use of chemical fertilizers, although no significant difference was observed between this treatment and the nitroxin and biophosphate treatments. Overall, the results of this three-year experiment show a very high response of the saffron plant to the simultaneous use of manure and biological fertilizers and, therefore, it is possible to replace chemical fertilizers with organic and biological fertilizers in saffron cultivation to implement organic agriculture and achieve acceptable quantitative and qualitative yields in areas similar to the experiment location.

Soil thermal conductivity (λ) is a critical property influencing heat transfer in agro-environmental systems (A-ES), affecting soil temperature, water dynamics, and nutrient availability. Understanding the impact of soil management practices (SMP) and climate adaptation strategies (CAS) on λ is essential for optimizing agricultural productivity and ensuring soil sustainability. This review examines the influence of conventional and conservation tillage, crop rotation, mulching, and organic matter incorporation on soil λ. Conventional tillage practices often disrupt soil structure, reducing water retention and altering soil thermal characteristics (TCs), while conservation tillage enhances soil aggregation and moisture conservation, leading to improved λ. Crop rotation and mulching regulate soil microclimates, minimizing temperature fluctuations and contributing to thermal stability. Additionally, the review highlights the significance of soil texture, moisture content, and organic matter in determining λ. With increasing climate variability, integrating SMP and CAS can mitigate adverse effects on TCs, promoting resilience in agricultural systems. However, knowledge gaps remain regarding the long-term impacts of these strategies on λ across diverse soil types and climatic conditions. Future research should focus on developing integrated approaches that optimize SMP and CAS for improved λ, ensuring sustainable agricultural practices. Expanding studies on soil thermal dynamics will improve our ability to develop adaptive management strategies that support long-term soil health and productivity. This review underscores the necessity of sustainable soil management in the face of climate change, providing insights for future research and practical applications in agricultural systems.

Agricultural activity is the major anthropogenic source of nitrous oxide (N ₂ O) emissions from terrestrial ecosystems. Conservation agriculture including crop residue management can play a key role in enhancing soil resilience to climate change and mitigating N ₂ O emissions. We investigated the effects of crop residue rates, including 100 % (R ₁₀₀ ), 50 % (R ₅₀ ), and residue removal (R ₀ ), on N ₂ O emissions in corn-wheat rotation under conventional (CT) and no-tillage (NT) systems. The key factors evaluated affecting N ₂ O emissions included soil temperature, soil moisture, soil ammonium, and soil nitrate concentrations. Results showed that the N ₂ O emissions increased with the increasing rate of residue under both CT and NT systems. Both R ₁₀₀ and R ₅₀ significantly ( p < .05) increased the N ₂ O emissions compared to R ₀ during the annual rotation cycle. Soil moisture and mineral nitrogen (ammonium and nitrate) were the main driving factors that stimulated N ₂ O emission in both CT and NT systems. In the NT and CT systems, cumulative N ₂ O emissions showed a significant increase with R ₅₀ (+75.5 % in NT, +36.5 % in CT) and R ₁₀₀ (+134 % in NT, +40 % in CT) as compared to R ₀ . Furthermore, no significant differences were found between R ₁₀₀ and R ₅₀ in the CT system, while in the NT system significant increases were observed for R ₁₀₀ compared to R ₅₀ . Overall, our study justified as a first approach only during the first year that crop residue removal led to decreased N ₂ O emissions under semi-arid conditions. However, due to the deteriorating impact of crop residue removal on crop productivity and soil C sequestration, this management method cannot be considered a sustainable agronomic practice. We suggest long-term studies to determine the appropriate rate of postharvest crop residue to achieve less N ₂ O emissions and climate-friendly agricultural practices.