Movement of faecal indicator organisms in earthworm channels under a loamy arable and grassland soil

被引:25
|
作者
Joergensen, RG
Kuntzel, H
Scheu, S
Seitz, D
机构
[1] Inst Bodenwissensch, D-37075 Gottingen, Germany
[2] Inst Allgemeine Hyg & Umwelthyg, D-37073 Gottingen, Germany
[3] Inst Zool 2, Abt Okol, D-37073 Gottingen, Germany
[4] Bur Standorterkundung Geries Ingn, D-37073 Gottingen, Germany
关键词
faecal pollution; coliforms; streptococci; microbial biomass; soil; drilosphere; substrate induced respiration; fumigation extraction;
D O I
10.1016/S0929-1393(98)00030-4
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
It is a critical issue for the application of animal slurry in water protection areas whether macropores such as earthworm burrows can contribute to the contamination of groundwater with faecal organisms. The aim of the current field experiment was to investigate the effects of the factors: slurry addition, land use (grassland/arable land), sampling date, depth (15, 45 and 75 cm), and drilosphere (soil surrounding an earthworm burrow) on the movement of faecal indicator organisms (total coliforms, faecal coliforms and faecal streptococci) into the subsoil. The experiment was carried out under worst case conditions, i.e., a soil at field capacity, irrigated directly after application of fresh cattle slurry with high rates of water. Under these conditions, we showed that significant numbers of faecal coliforms were transferred after slurry addition down earthworm burrows to the subsoil. We also showed that the numbers transferred in the grassland soil exceeded those of the arable soil. However, only about 0.16% (= 1.3 x 10(3) m(-2)) of the applied faecal coliforms were found under grassland around the earthworm burrows at a depth of between 40 and 80 cm. Total coliforms or faecal streptoccoci were not affected by slurry addition at any depth. In the drilosphere, the numbers of all faecal indicator organisms were always significantly increased in comparison to the bulk soil and also the contents of microbial biomass which were similar to those of the surface horizons. This means that the competition with the autochthonous soil microflora and thus, the decay rate of the introduced faecal bacteria, were also similar to the surface soil. Total and faecal coliforms were significantly related to each other and to the total microbial biomass. indicating that a certain percentage of these two groups belongs to the autochthonous soil bacterial microflora. The number of faecal streptococci varied enormously between replicate plots and the variation appeared to be independent of the factors studied. (C) 1998 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:1 / 10
页数:10
相关论文
共 17 条
  • [1] Depth transfer of fecal indicator organisms in an arable clayey soil
    Joergensen, RG
    Seitz, D
    ZEITSCHRIFT FUR PFLANZENERNAHRUNG UND BODENKUNDE, 1998, 161 (03): : 309 - 314
  • [2] Microbial diversity and abundance in loamy sandy soil under renaturalization of former arable land
    Kacergius, Audrius
    Voke, Diana
    PEERJ, 2023, 11
  • [3] MOVEMENT OF METRIBUZIN IN A LOAMY SAND SOIL UNDER IRRIGATED POTATO PRODUCTION
    BURGARD, DJ
    DOWDY, RH
    KOSKINEN, WC
    CHENG, HH
    WEED SCIENCE, 1994, 42 (03) : 446 - 452
  • [4] Changes of pore morphology, infiltration and earthworm community in a loamy soil under different agricultural managements
    Lamandé, M
    Hallaire, V
    Curmi, P
    Pérès, G
    Cluzeau, D
    CATENA, 2003, 54 (03) : 637 - 649
  • [5] Carbon dynamics in a 60 year fallowed loamy-sand soil compared to that in a 60 year permanent arable or permanent grassland UK soil
    Yuping Wu
    Sarah Kemmitt
    Rodger P. White
    Jianming Xu
    Philip C. Brookes
    Plant and Soil, 2012, 352 : 51 - 63
  • [6] Carbon dynamics in a 60 year fallowed loamy-sand soil compared to that in a 60 year permanent arable or permanent grassland UK soil
    Wu, Yuping
    Kemmitt, Sarah
    White, Rodger P.
    Xu, Jianming
    Brookes, Philip C.
    PLANT AND SOIL, 2012, 352 (1-2) : 51 - 63
  • [7] Denitrifier Community Dynamics in Soil Aggregates under Permanent Grassland and Arable Cropping Systems
    Miller, M. N.
    Zebarth, B. J.
    Dandie, C. E.
    Burton, D. L.
    Goyer, C.
    Trevors, J. T.
    SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2009, 73 (06) : 1843 - 1851
  • [8] Soil structure and earthworm activity in a marine silt loam under pasture versus arable land
    A.G. Jongmans
    M.M. Pulleman
    J.C.Y. Marinissen
    Biology and Fertility of Soils, 2001, 33 : 279 - 285
  • [9] Soil structure and earthworm activity in a marine silt loam under pasture versus arable land
    Jongmans, AG
    Pulleman, MM
    Marinissen, JCY
    BIOLOGY AND FERTILITY OF SOILS, 2001, 33 (04) : 279 - 285
  • [10] The impact of soil organisms on soil functioning under neotropical pastures:: a case study of a tropical anecic earthworm species
    Jiménez, JJ
    Decaëns, T
    AGRICULTURE ECOSYSTEMS & ENVIRONMENT, 2004, 103 (02) : 329 - 342