Global warming is the main concern in today’s century as it comes with numerous side effects to the natural environment. Open Top Chambers (OTC) consist of metal constructions with transparent vertical side-walls and a frustum on top. An opening in the middle of the frustum allows an air exchange to reduce temperature and humidity effects in the chamber. The size of the open top chamber which is located in Universiti Putra Malaysia is slanted 60o , 50cm tall, 2.08m basal diameter hexagon chamber. The Open Top Chamber experiments were carried out to determine how much global warming has affected and is still affecting the temperature, pH, the moisture and the growth of the microbes in the tropical soil. The aim of this study is to eluc...
In order to understand the response of soil microbial biomass to warming, field warming experiments ...
Microbial decomposition of soil organic matter (SOM) is the source of most of the terrestrial carbon...
The temperature sensitivity (Q10) of soil heterotrophic respiration (Rh) is an important ecological ...
The effects of global warming are increasingly evident, where global surface temperatures and atmosp...
The effects of global warming are increasingly evident, where global surface temperatures and atmosp...
Bacteria are important biological components of soil that play pivotal roles in improving soil quali...
Microbes are dominant biota in soil where they interact with each other and plants, control nutrient...
Numerous field studies have found changes in soil respiration and microbial abundance under experime...
Increasing global temperatures have been reported to accelerate soil carbon (C) cycling but also to ...
We conducted a short-term laboratory soil warming incubation experiment, sampling both warmed and un...
A soil cooling system that prepares soil for temperate soil temperatures for the growth of temperate...
Although the maritime Antarctic has undergone rapid warming, the effects on indigenous soil-inhabiti...
Bacteria and fungi are the main agents in decomposition of soil organic matter. Their activity is de...
Soil microbial respiration and methanogenesis are key sources of atmospheric carbon. Conflicting evi...
Eutrophication and climate warming, induced by anthropogenic activities, are simultaneously occurrin...
In order to understand the response of soil microbial biomass to warming, field warming experiments ...
Microbial decomposition of soil organic matter (SOM) is the source of most of the terrestrial carbon...
The temperature sensitivity (Q10) of soil heterotrophic respiration (Rh) is an important ecological ...
The effects of global warming are increasingly evident, where global surface temperatures and atmosp...
The effects of global warming are increasingly evident, where global surface temperatures and atmosp...
Bacteria are important biological components of soil that play pivotal roles in improving soil quali...
Microbes are dominant biota in soil where they interact with each other and plants, control nutrient...
Numerous field studies have found changes in soil respiration and microbial abundance under experime...
Increasing global temperatures have been reported to accelerate soil carbon (C) cycling but also to ...
We conducted a short-term laboratory soil warming incubation experiment, sampling both warmed and un...
A soil cooling system that prepares soil for temperate soil temperatures for the growth of temperate...
Although the maritime Antarctic has undergone rapid warming, the effects on indigenous soil-inhabiti...
Bacteria and fungi are the main agents in decomposition of soil organic matter. Their activity is de...
Soil microbial respiration and methanogenesis are key sources of atmospheric carbon. Conflicting evi...
Eutrophication and climate warming, induced by anthropogenic activities, are simultaneously occurrin...
In order to understand the response of soil microbial biomass to warming, field warming experiments ...
Microbial decomposition of soil organic matter (SOM) is the source of most of the terrestrial carbon...
The temperature sensitivity (Q10) of soil heterotrophic respiration (Rh) is an important ecological ...