{"title":"ASPECT CONCERNING TO THE AGRICULTURAL EXPLOITATION, ON LANDS WITH DRAINAGE WORKS FROM PALTINOASA-DRAGUSENI SECTOR, SUCEAVA COUNTY","authors":"O. Radu","doi":"10.15551/FPPZT.V1I7.366","DOIUrl":"https://doi.org/10.15551/FPPZT.V1I7.366","url":null,"abstract":"","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-07-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126636275","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"LES RELATIONS ENTRE L’ERODABILITE DES SOLS ET LEURS PROPRIETES PHYSICO-MECANIQUES","authors":"Iulian Cătălin Stângă","doi":"10.15551/fppzt.v4i1.328","DOIUrl":"https://doi.org/10.15551/fppzt.v4i1.328","url":null,"abstract":"L’erodabilite represente la susceptibilite des sols d’etre erodes sous l’action des\u0000pluies, du ruissellement ou du vent. Cette susceptibilite est conditionnee par les proprietes\u0000physico-chimiques des sols. Dans l’article ci-dessous, on montre les relations qui existent entre\u0000l’erodabilite et les proprietes physico-mecaniques des sols, dont les plus importantes sont la\u0000granulometrie (surtout le rapport entre differentes fractions texturales), la structure, la densite,\u0000la permeabilite et la conductivite hydrauliques.","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"63 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-03-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"132994853","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"APPROCHE GÉOGRAPHIQUE SUR LES ANDOSOLS","authors":"Eugen Rusu","doi":"10.15551/FPPZT.V4I1.306","DOIUrl":"https://doi.org/10.15551/FPPZT.V4I1.306","url":null,"abstract":"De la conţinutul japonez inţial al noţiunii de andosol, referitor la solurile negre\u0000formate pe cenusi vulcanice si pe tufuri, conceptul a evoluat pe baza cercetărilor ulterioare,\u0000incluzând soluri formate pe o categorie mai largă de roci vulcanice, care prin alterare, dau\u0000produsele alofanice specifice.","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"119 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-03-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"117294784","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"ABOUT RENDZINA SOILS WHICH IS FORMED ON GYPSUM FROM SLON DEPRESSION","authors":"M. Parichi, A. Stănilă, V. Duca, N. Rizea","doi":"10.15551/FPPZT.V4I1.319","DOIUrl":"https://doi.org/10.15551/FPPZT.V4I1.319","url":null,"abstract":"By now, in our country wasn ׳ t separated areas with exclusit rendzine gypsom.\u0000In most cases, these types of soils apear in association with other soils. We found rendzina\u0000and cambic rendzina in upper basin of Drajna valley witch, is locate on mountain-hill\u0000morphological contact and limited from cast by Pintenul de Homorâciu (Paleogen\u0000structure). These soils are possibly, to represent on maps. On large areas appear only\u0000cambic rendzina in various conditions of slopes. Analytic data about these soil indicate a\u0000large content of cley (52-56 per cent), neutral reaction middle-large cation exchange\u0000capacity (34-49 me/100 g soil) and middle-large humus content.","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"48 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-03-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114804778","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"CARACTERIZAREA UNOR ASOCIAŢII VEGETALE HALOFILE DIN BAZINUL BAHLUI PE BAZA INDICILOR ECOLOGICI","authors":"Angela Lupașcu, Liliana-Gabriela Aniței, Lilian Niacșu","doi":"10.15551/FPPZT.V4I1.315","DOIUrl":"https://doi.org/10.15551/FPPZT.V4I1.315","url":null,"abstract":"","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"242 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-03-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122155397","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
C. Secu, M. Costica, A. Lupașcu, N. Costică, I. Moglan
{"title":"BIO-PEDO-GEOGRAPHYCAL REGARDS ON GARBAGE DUMPS FROM TOMEŞTI - IAŞI","authors":"C. Secu, M. Costica, A. Lupașcu, N. Costică, I. Moglan","doi":"10.15551/FPPZT.V4I1.331","DOIUrl":"https://doi.org/10.15551/FPPZT.V4I1.331","url":null,"abstract":"The garbage dump from Tomesti (Iasi) represents a water and soil pollution source, as\u0000well as a peril for the population’s health. The study has pursued the analysis of some indicators\u0000of water quality (which have evidenced exceeds of the currently admitted values), the\u0000identification of the plant species from the garbage dump perimeter (table 1) and the\u0000presentation of the general geographical landscape.","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"37 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-03-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122171133","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"SOIL ACIDIFICATION BY FERROLYSIS IN A PEDOLOGICAL SEQUENCE OF MUNTELE MIC, CARAŞ-SEVERIN COUNTY","authors":"G. Rogobete, A. Grozav, D. Beutură, I. Nemes","doi":"10.15551/FPPZT.V6I1.237","DOIUrl":"https://doi.org/10.15551/FPPZT.V6I1.237","url":null,"abstract":"Soil acidification process in aerated soils is a consequence of: (1) production of\u0000various acids in the soil, (2) the effect of ion uptake of biota, (3) nitrogen inputs and (4) the\u0000addition of dissolved strong acids. The soils formed by acidolysis process are Umbric Podzols,\u0000Umbric – entic Podzols, Haplic Umbrisols – Dystric Cambisol and Dystric Fluvisols.\u0000In the case of presence of an argic horizon with alternating aerobic and anaerobic\u0000conditions the main process is ferrolysis. During wet periods, iron oxides undergo reduction and\u0000in aerobic conditions with Fe2+ oxidation, it will be generating acid soils, like Stagni – albic\u0000Luvisols.","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"16 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-03-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"116824377","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"SOIL COVER IN TUTOVA DRAINAGE BASIN","authors":"I. Stângă, Ana-Maria Iacob","doi":"10.15551/fppzt.v9i1.153","DOIUrl":"https://doi.org/10.15551/fppzt.v9i1.153","url":null,"abstract":"This article covers a monographic presentation of the soils from the Tutova drainage basin. The analysis of the pedogeographic assemblage was performed based on the soil surveys of the territories corresponding to Tutova’s drainage basin, and completed with field research. The taxonomic classification was done in accordance with the Romanian System of Soil Taxonomy (2003) and the soil map was created at a 1:25.000 scale. The zonal soils dominate the region; the Chernisols are on the first rank with a share of 39.95%, followed by Luvisols with a percent of 27.62%. Among the soils with an azonal and intrazonal character, the entic soils are dominant (21.90%), followed by Anthrosols (8.89%) and by Hydrisols (1.64%).","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"9 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-03-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131019689","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"CHARACTERIZATION OF SOIL TRICHODERMA ISOLATES FOR POTENTIAL BIOCONTROL OF PLANT PATHOGENS","authors":"S. Matei, G. Matei, P. Cornea, G. Popa","doi":"10.15551/FPPZT.V10I1.170","DOIUrl":"https://doi.org/10.15551/FPPZT.V10I1.170","url":null,"abstract":"Various fungal strains belonging to genus Trichoderma act as biological control agents for soil born plant pathogens. Two new strains of Trichoderma harzianum (T.h.) and Trichoderma viride (T.v.) were isolated from forest soils in Ilfov county and their morphological aspects, enzymatic and antagonistic activity were examined. Current chemical fungicides had constantly, in time, less influence on pathogens due to their diversity, adaptability and increasing resistance.\u0000The paper present the morphological characterization of two strains of Trichoderma isolated from forest soils. Growth rate was higher in strain T.v.SP456 (0,675mm/h) than in strain T.h.P8 (0,505mm/h) when fungi were grown on Czapek culture medium.\u0000Morphological description is completed with photographs of colonies in Petri plates and microscopical aspects of fungal structures belonging to Trichoderma strains SP456 and P8.\u0000Comparative aspects concerning the level of main enzymes released by T.h. isolate P8 and T.v.SP456 in liquid culture media showed differences as a function of genetic structure of each fungal isolate. The optimum culture media for inducing peroxidase, polyphenol-oxidase, β-1,3-glucanase activity in T.v.SP456 isolate was Czapek and PDA for phenil-alanin-ammonium-oxidase and chitinase. T.v.SP456 was more efficient than T.h.P8 concerning enzymes activity.\u0000The interaction between Trichoderma fungal strains SP456 and P8 and strawberry plant pathogen strains, three belonging to Botrytis cinerea (S1, P1, P2) and one to Phytophtora spp. were examined, also. Both Trichoderma strains act as mycoparasites for plant pathogens. The inhibition percent of radial growth was higher for T.v.SP456 when compared with T.h.P8 for almost all pathogenic isolates.","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"15 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-03-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133257310","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"THE ECO-PEDOLOGICAL AND PEDO- FUNCTIONAL FRAMEWORK OF CHERNOZEM SUITABILITY TO UNCONVENTIONAL TILLAGE SYSTEMS FROM THE DNIESTER-PRUT INTERFLUVE","authors":"G. Jigau","doi":"10.15551/FPPZT.V8I1.156","DOIUrl":"https://doi.org/10.15551/FPPZT.V8I1.156","url":null,"abstract":"Some elements, even unconventional tillage systems have come to the attention of both research and production activities starting from the early nineteen eighties. Although research in the pilot lands have revealed promising results, until recently they remained unsolicited. The main factor that has supported such a situation was the total dependence to conventional farming systems, based on plowing, and this is supported by the low prices practiced by energy agents and also by the low prices of mineral fertilizers. In addition, in relation to economic interests, conventional systems materialized into increased land productivity and income. At the same time, in relation to ecologic balance, they have produced profound changes, evidenced by increased vulnerability to the actions of various soil degradation processes, diseases and pests and the emergence of new limiting factors.\u0000Specified negative consequences accumulate from one year to another, from one stage to another. More frequently, the specified changes affect attributes like (bulk density, structure, porosity etc.) and soil physical regimes (moisture, aeration, heat etc.). Also the chemical and biological characteristics of soil undergo significant changes.\u0000This paper is an analysis of the behavior of soils under unconventional tillage systems.","PeriodicalId":202276,"journal":{"name":"Soil Forming Factors and Processes from the Temperate Zone","volume":"20 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2012-03-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"124096630","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}