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首页> 外文期刊>Soil Biology & Biochemistry >Experimental evidence for the role of earthworms in compacted soil regeneration based on field observations and results from a semi-field experiment
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Experimental evidence for the role of earthworms in compacted soil regeneration based on field observations and results from a semi-field experiment

机译:基于田间观察和半田间试验结果的worm在压实土壤再生中的作用的实验证据

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摘要

In laboratory experiments, earthworms are often observed to burrow through compacted soil layers, leading to the general assumption that these animals play a significant role in regenerating compacted soils in agricultural plots. To demonstrate this role under field conditions, the abundance of earthworm macropores inside compacted zones was estimated on plots under reduced (RT) or conventional tillage (CT). Then, different types of compacted zones typically found in CT (plough pan and compacted clods) and RT plots (compacted volume under wheel tracks) were experimentally simulated in wooden boxes, buried in the field and inoculated with different earthworm species. After 6 weeks of incubation, the number of macropores inside the compacted zones was examined. Field observations showed that approximately 10% and 30% of the compacted zones were colonised by at least one macropore in CT and RT plots, respectively. A significantly greater number of anecics was found in RT plots, but we could not conclude that this ecological type of earthworm plays a more major role in the regeneration process in these plots since there were fewer compacted zones and these covered a smaller area in CT. The semi-field experiment provided evidence that earthworm-mediated regeneration of compacted zones is possible and its nature varies between ecological types of earthworm. Lumbricus terrestris, which makes individual burrows that are vertical and deep, was the main species to cross through the plough pan. The other three earthworm species (Aporrectodea giardi, A. caliginosa and A. rosea) did burrow inside the other types of compacted zones (wheel tracks and compacted clods). In every case, however, macropore density was far greater in non-compacted zones, illustrating that avoidance of compacted soil by earthworms is important and should be taken into account when extrapolating results from laboratory studies.
机译:在实验室实验中,经常观察到s在压实的土壤层中钻洞,导致人们普遍认为这些动物在农业土地上的压实土壤再生中起着重要作用。为了证明在田间条件下的这种作用,在减少耕作(RT)或常规耕作(CT)的地块上,估算了压实区内inside的大量存在。然后,在木箱中实验性地模拟了通常在CT(犁地盘和压实土块)和RT图(轮迹下的压实体积)中发现的不同类型的压实带,将其埋在田间并接种了不同的earth物种。温育6周后,检查压实区内的大孔数量。现场观察表明,在CT和RT图中,分别有至少10个大孔定植了大约10%和30%的压实带。在RT地块中发现了大量的风药,但是我们不能得出结论,这种生态类型的worm在这些地块中的再生过程中起着更重要的作用,因为压实区较少,而CT覆盖的面积较小。半田间实验提供了证据,证明mediated介导的致密带再生是可能的,and的性质在ecological的生态类型之间也有所不同。 mb草(Lumbricus terrestris)是穿过犁盘的主要树种,它们使垂直和深深的单个洞穴成为可能。其他三个earth物种(Aporrectodea giardi,A。caliginosa和A. rosea)确实在其他类型的压实区域(轮迹和压实土块)内钻洞。但是,在每种情况下,非压实区的大孔密度都高得多,这说明avoid避免压实土壤很重要,在从实验室研究中推断结果时应予以考虑。

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