Titlebook: Conifer Cold Hardiness; Francine J. Bigras,Steve J. Colombo Book 2001 Springer Science+Business Media Dordrecht 2001 Plant physiology.Tree

驅(qū)逐

書目名稱Conifer Cold Hardiness影響因子(影響力)




書目名稱Conifer Cold Hardiness影響因子(影響力)學(xué)科排名




書目名稱Conifer Cold Hardiness網(wǎng)絡(luò)公開度




書目名稱Conifer Cold Hardiness網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Conifer Cold Hardiness被引頻次




書目名稱Conifer Cold Hardiness被引頻次學(xué)科排名




書目名稱Conifer Cold Hardiness年度引用




書目名稱Conifer Cold Hardiness年度引用學(xué)科排名




書目名稱Conifer Cold Hardiness讀者反饋




書目名稱Conifer Cold Hardiness讀者反饋學(xué)科排名

引水渠

Molecular Biology of Conifer Frost Tolerance and Potential Applications to Tree Breedingmancy) by mid-winter, when frost tolerance is maximal; and (3) frost tolerance is minimal (?3 to ?10°C) from budbreak and cambial reactivation in the spring until growth cessation in the autumn (.. Riding and Little 1984; Mellerowicz et al. 1992a; Dormling 1993; Qamaruddin et al. 1993; other chapter

斗志

象形文字

1568-2544 ientists, pathologists, advanced nursery andsilvicultural practitioners, and graduate students involved in plantbiology, plant physiology, horticulture and forestry with an interestin cold hardiness.978-90-481-5587-3978-94-015-9650-3Series ISSN 1568-2544

托運(yùn)

Transport and Mixing in Geophysical Flows. In horticulture, the concept of plant hardiness zones is well established. These zones are based on the lowest mean air temperatures of the coldest month and, as their first usage was in the USA (Rehder 1940), are based on the Fahrenheit scale of temperature. The U.S. Department of Agriculture (US

四指套

,Charge-Glass State in θ-(BEDT-TTF)2X,mancy) by mid-winter, when frost tolerance is maximal; and (3) frost tolerance is minimal (?3 to ?10°C) from budbreak and cambial reactivation in the spring until growth cessation in the autumn (.. Riding and Little 1984; Mellerowicz et al. 1992a; Dormling 1993; Qamaruddin et al. 1993; other chapter

四指套

single

Asseverate

alcohol-abuse

Transport and Mixing in Geophysical Flowsdivided with respect to various relationships between temperature and precipitation, whilst Thornthwaite’s (1948) classification is based on potential evapo-transpiration. The distribution of major vegetation types is explained and even predicted by such classifications. Resistance to low temperatur