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Distribution of water-stable aggregates under soil tillage practices in a black soil hillslope cropland in Northeast China

机译:东北黑土坡耕地耕作下水稳定团聚体的分布

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Purpose Soil aggregates are the basic units of soil structure. Water-stable aggregates (WSAs) are greatly influenced by tillage practices. The main objective of our study was to assess the effects of different tillage practices on water aggregate stability on hillslope cropland in northern China and to identify the relationship between soil aggregates and soil structure stability.Materials and methods The study was conducted under on-farm conditions. Soils from plots with no tillage (NT), rotary tillage (RT), and conventional tillage (CT) treatments were sampled for 2 years (2016-2017) in the study area (Xiangyang village, Harbin city, Heilongjiang Province). Soil aggregates were collected, and the mean weight diameter (MWD) and geometric mean diameter (GMD) were calculated. The relationships between the soil aggregate variables and soil structural stability were determined using multivariate stepwise analysis.Results and discussion The results indicated that for macroaggregates, the MWD and GMD increased under NT and more readily formed WSAs > 5 mm. The effects of the different treatments on microaggregates were similar among the different slope positions. The variation in the proportion of macroaggregate across all the treatments was lower in 2017 than that in 2016. The reduction in soil macroaggregates under NT was much smaller than the reductions under RT and CT, suggesting that soil structure can be maintained under NT. The multivariate stepwise analysis showed that the proportion of WSAs > 5 mm were positively and significantly correlated with MWD and GMD and represented the predominant factor influencing soil structure according to the discriminant coefficients. The proportion of microaggregates also affected the MWD and GMD of the soil aggregates but had negative correlations with these variables. There were significantly positive correlations between the soil organic matter content and soil structure stability variables (macroaggregate content, MWD, and GMD).Conclusions Overall, macroaggregates in soil likely play a key role in soil structure stability. The soil aggregate stability is also affected by slope position. Comparing RT and NT, soil structure can be better maintained with NT.
机译:目的土壤聚集体是土壤结构的基本单位。耕作方法对水稳性骨料(WSA)有很大影响。本研究的主要目的是评估不同耕作方式对中国北方丘陵农田水团聚体稳定性的影响,并确定土壤团聚体与土壤结构稳定性之间的关系。材料和方法本研究是在农田条件下进行的。 。在研究区(黑龙江省哈尔滨市襄阳村)对两年(2016-2017年)的无耕地(NT),旋耕(RT)和常规耕作(CT)处理的土壤进行了采样。收集土壤团聚体,并计算平均重量直径(MWD)和几何平均直径(GMD)。结果和讨论结果表明,对于大集料,NT下MWD和GMD升高,且> 5 mm的WSA更容易形成。在不同的坡度位置之间,不同处理对微骨料的影响相似。 2017年所有处理中大集料比例的变化均低于2016年。NT下土壤大集料的减少量远小于RT和CT下的减少量,表明在NT下土壤结构可以保持。多元逐步分析表明,WSA> 5 mm的比例与MWD和GMD呈显着正相关,并且根据判别系数代表了影响土壤结构的主要因素。微团聚体的比例也影响土壤团聚体的MWD和GMD,但与这些变量负相关。土壤有机质含量与土壤结构稳定性变量(大骨料含量,MWD和GMD)之间存在显着的正相关。结论总体而言,土壤中的大骨料可能对土壤结构稳定性起关键作用。土壤骨料的稳定性也受坡度的影响。比较RT和NT,使用NT可以更好地保持土壤结构。

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