Structure and functioning of earthworm communities in woodland flooding systems used for drinking water production

被引:20
|
作者
Schuetz, Kirsten [1 ]
Nagel, Peter [1 ]
Dill, Andreas [2 ]
Scheu, Stefan [3 ]
机构
[1] Univ Basel, Dept Environm Sci, Inst Biogeog, CH-4056 Basel, Switzerland
[2] Univ Basel, Dept Environm Sci, Inst Geog, CH-4056 Basel, Switzerland
[3] Tech Univ Darmstadt, Inst Zool, D-64287 Darmstadt, Germany
关键词
infiltration; macropores; soil invertebrates; ecosystem engineers; floodplain forest; clogging; groundwater recharge;
D O I
10.1016/j.apsoil.2008.02.002
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Earthworms are known to influence water infiltration in soils, but most of the existing knowledge relates to grasslands and arable systems; little is known on the role of earthworms for water infiltration in forests. We studied earthworm populations and water infiltration rates in woodland flooding sites used for groundwater recharge and the production of drinking water. Intensive flooding may detrimentally affect earthworm populations and simultaneously result in clogging of the topsoil, with the latter being a common problem in groundwater recharge systems. However, clogging does not occur at our study site, the "Lange Erlen" (Basel, Switzerland) and total earthworm numbers and biomass in flooded sites exceeded those of non-flooded sites (+51% and +71%, respectively). Total earthworm numbers (r = 0.85***), numbers of endogeic (r = 0.64*) and epigeic (r = 0.81**) earthworms and numbers of two species (Lumbricus rubellus, r = 0.62* and Allolobophora chlorotica, r = 0.77**) significantly correlated with water infiltration rates. The results suggest that short-term flooding (max. 10 days) interrupted by longer recovery periods favor earthworm populations which likely contribute to the long-term (ca. 100 years) sustainability of the studied forest groundwater recharge system and thereby to effective and cost efficient drinking water production. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:342 / 351
页数:10
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