Results 161 to 170 of about 584,184 (359)
Responses of ectomycorrhizal fungi to mineral substrates [PDF]
Boreal forest soils are complex, heterogeneous growth substrates where organic and mineral components provide nutrient resources for soil organisms and plants. Mineral nutrients are cycled between living and dead organic components of the forest soil and
Rosling, Anna
core
High‐elevation endemic plants predicted to lose habitat from changing climate in Washington State
Abstract Premise High‐elevation plants face unique challenges from potential climate change impacts that will likely require upslope migration into increasingly smaller suitable habitat. This situation is particularly acute for endemic species that by definition occupy small geographic ranges.
Nicholas L. Gjording +4 more
wiley +1 more source
On the basis of two long-term fertilization experiments performed on the SGGW experimental field at Łyczyn, the effect of particular fertilizer components (N, P, K, Ca) and manure as well as the application of the increasing doses of mineral fertilizers (
Beata Rutkowska +2 more
doaj
Effects of Tillage Methods on Soil Organic Carbon and Total Nitrogen Content in the Loess Plateau [PDF]
Tingting Meng, MENG Tingting
openalex +1 more source
Potential of soil minerals to sequester soil organic carbon
Heidy Soledad Rodríguez Albarracín +7 more
openaire +1 more source
A leaf phenomics approach for estimating belowground traits in North American licorice
Abstract Premise Selective breeding over thousands of years has prioritized aboveground yield, with little regard for changes belowground. Roots underpin plant growth and resilience, but our knowledge of these critical structures lags behind that of aboveground structures.
Zachary N. Harris +5 more
wiley +1 more source
Measurable soil organic carbon fractions for modeling soil carbon sequestration
The objective of this research was to isolate biologically meaningful and measurable soil organic matter (SOM) fractions related to the organic carbon (C) pools described in the Century SOM model. This was achieved by measuring the changes of isolated C fractions during a six-month incubation study of three different soils, varying in clay content ...
openaire +1 more source

