Edaphic heterogeneity related to below-canopy water and solute fluxes in a Canarian laurel forest

被引:13
作者
Aboal, Jesus R. [1 ]
Saavedra, Santiago [2 ]
Manuel Hernandez-Moreno, Jose [3 ]
机构
[1] Univ Santiago de Compostela, Fac Biol, Dept Cell Biol & Ecol, Santiago De Compostela 15782, A Coruna, Spain
[2] Univ Santiago de Compostela, Dept Chem Engn, Santiago De Compostela 15782, A Coruna, Spain
[3] Univ La Laguna, Dept Edaphol, E-38207 San Cristobal la Laguna, Spain
关键词
Morella faya; Throughfall; Acidification; Stemflow; Leaching; Phosphorus; TROPICAL RAIN-FOREST; STEMFLOW CONTRIBUTION; SPATIAL-PATTERNS; CENTRAL AMAZONIA; OAK FOREST; THROUGHFALL; SOIL; DEPOSITION; TREES; AVAILABILITY;
D O I
10.1007/s11104-014-2285-4
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
To study the differences in the edaphic properties between stemflow infiltration areas around different tree species and between these and other areas of the forest. Soil samples were collected in stemflow infiltration areas and other areas only exposed to throughfall. pH, soluble salt concentration, soil organic carbon and nitrogen, exchangeable bases and Al3+, soluble and available phosphorus and phosphate retention were measured in the soil samples. The inputs of water and H+, Na+, K+, Ca2+, Mg2+, TOC, Fe, NO3 (-), SO4 (2-), PO4 (3-), and Cl- that reached these areas were calculated. Comparison of the soil properties measured in the throughfall and stemflow infiltration areas corresponding to each species revealed significant differences (p < 0.05), except for exchangeable Mg2+ and Al3+. Differences were observed between i) the stemflow infiltration areas around Morella faya and around each of the other species, and ii) the throughfall infiltration area and the stemflow infiltration area around each of the different species. pH, electric conductivity and available phosphorus of sampled soils were correlated with the corresponding stemflow inputs. The edaphic properties varied in different below-canopy infiltration areas (mainly between the stemflow infiltration area around M. faya and other parts of the forest soil).
引用
收藏
页码:177 / 188
页数:12
相关论文
共 54 条
[31]   RELATIONSHIPS AMONG ATMOSPHERIC DEPOSITION, THROUGHFALL, AND SOIL PROPERTIES IN OAK FOREST ECOSYSTEMS [J].
MACDONALD, NW ;
WITTER, JA ;
BURTON, AJ ;
PREGITZER, KS ;
RICHTER, DD .
CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE FORESTIERE, 1993, 23 (11) :2348-2357
[32]   The stemflow of trees in a Bornean lowland tropical forest [J].
Manfroi, OJ ;
Koichiro, K ;
Nobuaki, T ;
Masakazu, S ;
Nakagawa, M ;
Nakashizuka, T ;
Chong, L .
HYDROLOGICAL PROCESSES, 2004, 18 (13) :2455-2474
[33]   Laurel forests in Tenerife, Canary Islands .1. The site, stand structure and stand leaf area distribution [J].
Morales, D ;
Jimenez, MS ;
GonzalezRodriguez, AM ;
Cermak, J .
TREES-STRUCTURE AND FUNCTION, 1996, 11 (01) :34-40
[34]   Effect of water: Soil ratio on phosphate release: P, aluminium and fulvic acid associations in water extracts from Andisols and Andic soils [J].
Negrin, MA ;
EspinoMesa, M ;
HernandezMoreno, JM .
EUROPEAN JOURNAL OF SOIL SCIENCE, 1996, 47 (03) :385-393
[35]  
Pypker TG, 2011, ECOL STUD-ANAL SYNTH, V216, P371, DOI 10.1007/978-94-007-1363-5_18
[36]   Factors influencing decline in soil pH in Hawaiian Eucalyptus and Albizia plantations [J].
Rhoades, C ;
Binkley, D .
FOREST ECOLOGY AND MANAGEMENT, 1996, 80 (1-3) :47-56
[37]   Investigating the random relocation of gauges below the canopy by means of numerical experiments [J].
Ritter, Axel ;
Regalado, Carlos M. .
AGRICULTURAL AND FOREST METEOROLOGY, 2010, 150 (7-8) :1102-1114
[38]  
RUTTER A J, 1972, Agricultural Meteorology, V9, P367, DOI 10.1016/0002-1571(71)90034-3
[39]   Nutrient fluxes in rainfall, throughfall and stemflow in tree-based land use systems and spontaneous tree vegetation of central Amazonia [J].
Schroth, G ;
Elias, MEA ;
Uguen, K ;
Seixas, R ;
Zech, W .
AGRICULTURE ECOSYSTEMS & ENVIRONMENT, 2001, 87 (01) :37-49
[40]  
Schroth G, 1999, HYDROL PROCESS, V13, P1423, DOI 10.1002/(SICI)1099-1085(199907)13:10<1423::AID-HYP819>3.0.CO