O'Connor Lauren J, Kahn Lewis P, Walkden-Brown Stephen W
Centre for Animal Health and Welfare, School of Rural Science and Agriculture, University of New England, Armidale, NSW 2351, Australia.
Vet Parasitol. 2008 Aug 17;155(3-4):223-34. doi: 10.1016/j.vetpar.2008.05.010. Epub 2008 May 14.
A factorial experiment (3 x 4 x 2 x 3) was conducted in programmable incubators to investigate interaction between the effects of rainfall amount, rainfall distribution and evaporation rate on development of Haemonchus contortus to L3. Sheep faeces containing H. contortus eggs were incubated on sterilised soil under variable temperatures typical of summer in the Northern Tablelands of NSW, Australia. Simulated rainfall was applied in 1 of 3 amounts (12, 24 or 32 mm) and 4 distributions (a single event on the day after deposition, or the same total amount split in 2, 3 or 4 equal events over 2, 3 or 4 days, respectively). Samples were incubated at either a Low or High rate of evaporation (Low: 2.1-3.4 mm/day and High: 3.8-6.1 mm/day), and faeces and soil were destructively sampled at 4, 7 and 14 days post-deposition. Recovery of L3 from the soil (extra-pellet L3) increased over time (up to 0.52% at day 14) and with each increment of rainfall (12 mm: <0.01%; 24 mm: 0.10%; 32 mm: 0.45%) but was reduced under the High evaporation rate (0.01%) compared with the Low evaporation rate (0.31%). All rainfall amounts yielded significantly different recoveries of L3 under Low evaporation rates but there was no difference between the 12 and 24 mm treatments under the High evaporation rate. The distribution of simulated rainfall did not significantly affect recovery of infective larvae. Faecal moisture content was positively associated with L3 recovery, as was the ratio of cumulative precipitation and cumulative evaporation (P/E), particularly when measured in the first 4 days post-deposition. The results show that evaporation rate plays a significant role in regulating the influence of rainfall amount on the success of L3 transmission.
在可编程培养箱中进行了一项析因实验(3×4×2×3),以研究降雨量、降雨分布和蒸发速率对捻转血矛线虫发育至L3阶段的影响之间的相互作用。将含有捻转血矛线虫卵的绵羊粪便置于澳大利亚新南威尔士州北部台地夏季典型的可变温度下的无菌土壤中进行培养。模拟降雨设置为3种降雨量(12、24或32毫米)中的1种以及4种分布方式(沉积后第二天单次降雨,或相同总量分别在2、3或4天内分为2、3或4次等量降雨事件)。样本在低蒸发速率(低:2.1 - 3.4毫米/天)或高蒸发速率(高:3.8 - 6.1毫米/天)下进行培养,并且在粪便和土壤沉积后第4、7和14天进行破坏性采样。从土壤中回收的L3(粪便外L3)随时间增加(第14天高达0.52%)且随降雨量的每次增加而增加(12毫米:<0.01%;24毫米:0.10%;32毫米:0.45%),但与低蒸发速率(0.31%)相比,在高蒸发速率下有所降低(0.01%)。在低蒸发速率下,所有降雨量产生的L3回收率均有显著差异,但在高蒸发速率下,12毫米和24毫米处理之间没有差异。模拟降雨的分布对感染性幼虫的回收率没有显著影响。粪便含水量与L3回收率呈正相关,累积降水量与累积蒸发量之比(P/E)也是如此,尤其是在沉积后的前4天测量时。结果表明,蒸发速率在调节降雨量对L3传播成功的影响方面起着重要作用。