Juan Fernando GALLARDO LANCHO

Prof. Dr. Juan Fernando GALLARDO LANCHO

IRNASa (retired), Consejo Superior de Investigaciones Científicas, Madrid, Spain
orcid

Research Focus & Metrics

Academic Career Length

51Years (1976-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 December 2003 in Biogeochemistry
Verified
Journal Article
Closed access
PDF file
BMB. Michalzik
B. Michalzik
ETE. Tipping
E. Tipping
JMJ. Mulder
J. Mulder
Juan Fernando GALLARDO LANCHOJuan Fernando GALLARDO LANCHO
Juan Fernando GALLARDO LANCHO
EME. Matzner
E. Matzner
MEM.A. Vicente Esteban
M.A. Vicente Esteban

12 May 2003 in Physiologia Plantarum
Verified
Journal Article
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León Aloys BravoLeón Aloys Bravo
León Aloys Bravo
Juan Fernando GALLARDO LANCHOJuan Fernando GALLARDO LANCHO
Juan Fernando GALLARDO LANCHO
ANAlejandro Navarrete
Alejandro Navarrete
NONélida Olave
Nélida Olave
JMJosé Martínez
José Martínez
LCLuis J. Corcuera
Luis J. Corcuera

11 November 2000 in Communications in Soil Science and Plant Analysis
Verified
Journal Article
Closed access
KSKnut Schneider
Knut Schneider
María-Belén TurriónMaría-Belén Turrión
María-Belén Turrión
Juan Fernando GALLARDO LANCHOJuan Fernando GALLARDO LANCHO
Juan Fernando GALLARDO LANCHO
The acid phosphatase activity (APA) is a key factor in phosphorus (P), mineralization, P nutrition of plants, and P cycling. However, the widely used method of Tabatabai and Bremner for APA determinations is seriously restricted in soils with high organic matter contents, owing to interference in photometric detection by dissolved organic matter. The objectives of this study were: A) to modify the procedure of Tabatabai and Bremner with a view to its application to forest soils rich in organic carbon, b) to determine APA contents in forest soils of the Sierra de Gata mountains, and c) to establish relationships between the APA with different soil parameters. The modified procedure was well adapted to forest soils with high organic matter contents and had good reproducibility, while maintaining the relative simplicity and accuracy of the original Tabatabai and Bremner procedure. APA in the forest soils studied was high but did not correlate with labile P. The APA in the soils studied depended principally on availability of readily degradable energy sources and soil nitrogen (N).
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1 February 1998 in Agriculture, Ecosystems & Environment
Verified
Journal Article
Closed access
GMG. Masciandaro
G. Masciandaro
BCB. Ceccanti
B. Ceccanti
Juan Fernando GALLARDO LANCHOJuan Fernando GALLARDO LANCHO
Juan Fernando GALLARDO LANCHO

1 July 1993 in Geomicrobiology Journal
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Journal Article
Closed access
BCB. Ceccanti
B. Ceccanti
BPB. Pezzarossa
B. Pezzarossa
Juan Fernando GALLARDO LANCHOJuan Fernando GALLARDO LANCHO
Juan Fernando GALLARDO LANCHO
GMG. Masciandaro
G. Masciandaro
Two natural soil ecosystems, representative of agricultural management in a temperate Mediterranean climate, were selected: a sandy soil located at Peccioli Farm, Pisa (Italy), and a silt‐loam soil located at Salamanca, Muñovela (Spain). Within the systems, three areas were sampled (0–10 cm) during the dry season, each corresponding to a different soil use: native undisturbed (NS), cultivated (CS, crop‐pasture rotation) and intensively cultivated soil (ICS, monoculture). Total C, N, exchangeable metals (Mn, Fe, Cu, Zn), ATP, urease, benzoyl‐argininamide (BAA)‐hydrolyzing and casein‐hydrolyzing proteases, phosphatase, ß‐glucosidase, and dehydrogenase were determined and compared. Exchangeable metals, ATP, enzyme activity, C, and N were found to be significantly higher (p = 1%) in native than in cultivated and intensive‐agriculture soils. A good correlation (p = 5%) was found between ATP, hydrolases, C, and N, indicating that all these parameters are related to soil microbial biomass and activity in such “low‐energy”; ecosystems. Dehydrogenase did not correlate with C, N, and protease activities, meaning that the soil ecosystems have low concentrations of exogenous substrates to metabolize, and microorganisms were in a low state of activity. These parameters may be taken as markers of agriculture‐induced changes in soil ecosystems.

1 September 2001 in Biology and Fertility of Soils
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Journal Article
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KSKnut Schneider
Knut Schneider
María-Belén TurriónMaría-Belén Turrión
María-Belén Turrión
PGPauline F. Grierson
Pauline F. Grierson
Juan Fernando GALLARDO LANCHOJuan Fernando GALLARDO LANCHO
Juan Fernando GALLARDO LANCHO
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