{"title":"耕作和覆盖对粗质土壤中土壤有机质物理池和化学池碳稳定性的影响","authors":"Shahida Nisar, Dinesh Kumar Benbi","doi":"10.1016/j.geodrs.2024.e00827","DOIUrl":null,"url":null,"abstract":"<div><p>Characterization of soil organic carbon (SOC) in terms of size, storage inside aggregates and chemical recalcitrance is vital to understand mechanisms of its stabilization and to devise climate smart agricultural management practices. Tillage and residue retention are known to influence carbon (C) storage within soil aggregates and its accumulation as particulate organic matter as well as organomineral complexes. However, the effect of tillage and crop residue retention on C stabilization in coarse textured soils through various mechanisms is not well understood. We studied the effect of conservation agriculture involving no tillage with surface residue mulch (NTM) in maize-wheat sequence on particulate (POC) and mineral associated organic C (MinOC), C storage within aggregates and acid non-hydrolysable C (NHC) in a sandy loam soil. Compared to conventional tillage without residue retention (CTM<sub>0</sub>), the NTM improved SOC stocks by 23% in top 15-cm soil and significantly increased coarse POC (∼92 to 284%) and fine POC (67 to 123%) with relatively little effect on MinOC. This indicated that MinOC had relatively small contribution towards SOC stabilization in coarse textured sandy loam soils with limited potential to form organomineral complexes. The results further showed that the effects of NTM were brought about by improved aggregate stability and C preservation inside macroaggregates of size >1 mm. Furthermore, greater amount of SOC (2.64 g C kg<sup>−1</sup>) and macroaggregate associated C (0.35–0.59 g C kg<sup>−1</sup>) occurred in recalcitrant forms (NHC) under NTM compared to conventional (CT) and deep tillage (DT). The NTM also impacted the belowground C input through improved root length density (RLD) and development of fibrous roots expressed as specific root length (SRL), which influenced SOC build-up and stabilization. It is concluded that compared to the existing practice of CTM<sub>0</sub>, the conservation agriculture involving NT with residue retention leads to SOC sequestration in coarse textured soils. Its large scale adoption, besides helping in climate change mitigation will lead to soil health improvement.</p></div>","PeriodicalId":56001,"journal":{"name":"Geoderma Regional","volume":"38 ","pages":"Article e00827"},"PeriodicalIF":3.1000,"publicationDate":"2024-06-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Tillage and mulching effects on carbon stabilization in physical and chemical pools of soil organic matter in a coarse textured soil\",\"authors\":\"Shahida Nisar, Dinesh Kumar Benbi\",\"doi\":\"10.1016/j.geodrs.2024.e00827\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Characterization of soil organic carbon (SOC) in terms of size, storage inside aggregates and chemical recalcitrance is vital to understand mechanisms of its stabilization and to devise climate smart agricultural management practices. Tillage and residue retention are known to influence carbon (C) storage within soil aggregates and its accumulation as particulate organic matter as well as organomineral complexes. However, the effect of tillage and crop residue retention on C stabilization in coarse textured soils through various mechanisms is not well understood. We studied the effect of conservation agriculture involving no tillage with surface residue mulch (NTM) in maize-wheat sequence on particulate (POC) and mineral associated organic C (MinOC), C storage within aggregates and acid non-hydrolysable C (NHC) in a sandy loam soil. Compared to conventional tillage without residue retention (CTM<sub>0</sub>), the NTM improved SOC stocks by 23% in top 15-cm soil and significantly increased coarse POC (∼92 to 284%) and fine POC (67 to 123%) with relatively little effect on MinOC. This indicated that MinOC had relatively small contribution towards SOC stabilization in coarse textured sandy loam soils with limited potential to form organomineral complexes. The results further showed that the effects of NTM were brought about by improved aggregate stability and C preservation inside macroaggregates of size >1 mm. Furthermore, greater amount of SOC (2.64 g C kg<sup>−1</sup>) and macroaggregate associated C (0.35–0.59 g C kg<sup>−1</sup>) occurred in recalcitrant forms (NHC) under NTM compared to conventional (CT) and deep tillage (DT). The NTM also impacted the belowground C input through improved root length density (RLD) and development of fibrous roots expressed as specific root length (SRL), which influenced SOC build-up and stabilization. It is concluded that compared to the existing practice of CTM<sub>0</sub>, the conservation agriculture involving NT with residue retention leads to SOC sequestration in coarse textured soils. 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引用次数: 0
摘要
要了解土壤有机碳(SOC)的稳定机制并制定气候智能型农业管理方法,就必须从其大小、聚集体内部储存情况以及化学抗逆性等方面确定其特征。众所周知,耕作和残留物保留会影响碳(C)在土壤团聚体中的储存及其作为颗粒有机物和有机矿物复合物的积累。然而,耕作和作物秸秆保留通过各种机制对粗纹理土壤中碳稳定的影响尚不十分清楚。我们研究了在玉米-小麦序列中采用免耕和表面残留物覆盖(NTM)的保护性耕作对砂壤土中颗粒有机碳(POC)和矿物相关有机碳(MinOC)、聚集体中的碳储存以及酸性不可水解碳(NHC)的影响。与不保留残留物的常规耕作(CTM0)相比,NTM 使表层 15 厘米土壤中的 SOC 储量提高了 23%,并显著增加了粗颗粒有机碳(92% 至 284%)和细颗粒有机碳(67% 至 123%),而对 MinOC 的影响相对较小。这表明,MinOC 对粗质砂壤土中 SOC 的稳定作用相对较小,形成有机矿物复合物的潜力有限。结果进一步表明,NTM 的效果是通过改善集料稳定性和在大小为 1 毫米的大集料中保存 C 来实现的。此外,与传统耕作(CT)和深耕(DT)相比,在非转基因耕作下,更多的 SOC(2.64 g C kg-1)和与大团聚体相关的 C(0.35-0.59 g C kg-1)以难降解形式(NHC)出现。通过提高根长密度(RLD)和发展以特定根长(SRL)表示的须根,非农耕技术还影响了地下碳输入,从而影响了 SOC 的积累和稳定。结论是,与现有的 "CTM0 "做法相比,采用 "NT "和 "残留物保留 "的保护性农业可在粗质土壤中固存 SOC。大规模采用这种方法,除了有助于减缓气候变化,还能改善土壤健康。
Tillage and mulching effects on carbon stabilization in physical and chemical pools of soil organic matter in a coarse textured soil
Characterization of soil organic carbon (SOC) in terms of size, storage inside aggregates and chemical recalcitrance is vital to understand mechanisms of its stabilization and to devise climate smart agricultural management practices. Tillage and residue retention are known to influence carbon (C) storage within soil aggregates and its accumulation as particulate organic matter as well as organomineral complexes. However, the effect of tillage and crop residue retention on C stabilization in coarse textured soils through various mechanisms is not well understood. We studied the effect of conservation agriculture involving no tillage with surface residue mulch (NTM) in maize-wheat sequence on particulate (POC) and mineral associated organic C (MinOC), C storage within aggregates and acid non-hydrolysable C (NHC) in a sandy loam soil. Compared to conventional tillage without residue retention (CTM0), the NTM improved SOC stocks by 23% in top 15-cm soil and significantly increased coarse POC (∼92 to 284%) and fine POC (67 to 123%) with relatively little effect on MinOC. This indicated that MinOC had relatively small contribution towards SOC stabilization in coarse textured sandy loam soils with limited potential to form organomineral complexes. The results further showed that the effects of NTM were brought about by improved aggregate stability and C preservation inside macroaggregates of size >1 mm. Furthermore, greater amount of SOC (2.64 g C kg−1) and macroaggregate associated C (0.35–0.59 g C kg−1) occurred in recalcitrant forms (NHC) under NTM compared to conventional (CT) and deep tillage (DT). The NTM also impacted the belowground C input through improved root length density (RLD) and development of fibrous roots expressed as specific root length (SRL), which influenced SOC build-up and stabilization. It is concluded that compared to the existing practice of CTM0, the conservation agriculture involving NT with residue retention leads to SOC sequestration in coarse textured soils. Its large scale adoption, besides helping in climate change mitigation will lead to soil health improvement.
期刊介绍:
Global issues require studies and solutions on national and regional levels. Geoderma Regional focuses on studies that increase understanding and advance our scientific knowledge of soils in all regions of the world. The journal embraces every aspect of soil science and welcomes reviews of regional progress.