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Effects of 11 years of conservation tillage on soil organic matter fractions in wheat monoculture in Loess Plateau of China

机译:黄土高原小麦单一耕作保护性耕作11年对土壤有机质的影响。

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The Loess Plateau in northwest China is one of the most eroded landscapes in the world, and it is urgent that alternative practices be evaluated to control soil erosion. Our objective was to determine how three different tillage practices for monoculture of winter wheat (Triticum aestivum L.) affected soil organic carbon (SOC) and N content after 11 years. Conventional tillage with residue removal (CT), shallow tillage with residue cover (ST), and no-tillage with residue cover (NT) were investigated. Carbon and N in various aggregate-size classes and various labile organic C fractions in the 0-15- and 15-30-cm soil layers were evaluated. The ST and NT treatments had 14.2 and 13.7% higher SOC stocks and 14.1 and 3.7% higher total N (Nt) stocks than CT in the upper 15cm, respectively. Labile C fractions: particulate organic C (POC), permanganate oxidizable C (KMnO-C), hot-water extractable C (HWC), microbial biomass C (MBC) and dissolved organic C (DOC) were all significantly higher in NT and ST than in CT in the upper 15cm. KMnO-C, POC and HWC were the most sensitive fractions to tillage changes. The portion of 0.25-2mm aggregates, mean weight diameter (MWD) and geometric mean diameter (GMD) of aggregates from ST and NT treatments were larger than from CT at both 0-15- and 15-30-cm soil depths. The ST and NT treatments had significantly higher SOC and Nt in the 0.25-2mm fraction at both depths and significantly higher Nt content in the upper 15cm. Positive significant correlations were observed between SOC, labile organic C fractions, MWD, GMD, and macroaggregate (0.25-2mm) C within the upper 15cm. We conclude that both variants of conservation tillage (NT and ST) increase SOC stock in the rainfed farming areas of northern China and are therefore more sustainable practices than those currently being used.
机译:中国西北的黄土高原是世界上最受侵蚀的景观之一,因此迫切需要对替代方法进行评估以控制水土流失。我们的目标是确定11年后,三种不同的耕作方式对冬小麦(Triticum aestivum L.)的单一耕作如何影响土壤有机碳(SOC)和氮含量。研究了带残留物去除的常规耕作(CT),带残留物覆盖的浅耕(ST)和带残留物覆盖的免耕(NT)。评估了0-15厘米和15-30厘米土壤层中各种骨料大小类别的碳和氮以及各种不稳定的有机C分数。在上部15厘米,ST处理和NT处理的SOC储量分别比CT高14.2%和13.7%,总N(Nt)储量分别比CT高14.1%和3.7%。不稳定的C馏分:NT和ST中的颗粒有机C(POC),高锰酸盐可氧化C(KMnO-C),热水可萃取C(HWC),微生物量C(MBC)和溶解有机C(DOC)均显着较高比在CT上方15cm KMnO-C,POC和HWC是对耕作变化最敏感的部分。在土壤深度为0-15和15-cm时,ST和NT处理的骨料的0.25-2mm骨料的比例,均重直径(MWD)和几何平均直径(GMD)均大于CT。 ST和NT处理在两个深度上的0.25-2mm分数中的SOC和Nt均显着较高,而在上部15cm中的Nt含量则显着较高。 SOC,不稳定的有机碳组分,MWD,GMD和上部15厘米以内的大骨料(0.25-2mm)C之间存在显着正相关。我们得出的结论是,保护性耕作的两种变体(NT和ST)都增加了中国北方雨养耕作地区的SOC量,因此比目前使用的耕作更具可持续性。

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