Zhigang Yi

ORCID: 0000-0002-9864-1011
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About
Contact & Profiles
Research Areas
  • Soil Carbon and Nitrogen Dynamics
  • Atmospheric chemistry and aerosols
  • Plant responses to elevated CO2
  • Fire effects on ecosystems
  • Odor and Emission Control Technologies
  • Toxic Organic Pollutants Impact
  • Air Quality and Health Impacts
  • Atmospheric and Environmental Gas Dynamics
  • Soil and Unsaturated Flow
  • Peatlands and Wetlands Ecology
  • Environmental and Agricultural Sciences
  • Soil and Water Nutrient Dynamics
  • Effects and risks of endocrine disrupting chemicals
  • Air Quality Monitoring and Forecasting
  • Microbial Community Ecology and Physiology
  • Atmospheric Ozone and Climate
  • Plant Genetic and Mutation Studies
  • Wastewater Treatment and Nitrogen Removal
  • Composting and Vermicomposting Techniques
  • Mercury impact and mitigation studies
  • Environmental Toxicology and Ecotoxicology
  • Clay minerals and soil interactions
  • Remote Sensing and Land Use
  • Microbial bioremediation and biosurfactants
  • Sugarcane Cultivation and Processing

Fujian Agriculture and Forestry University
2013-2024

Max Planck Institute for Chemistry
2018-2019

Chinese Academy of Sciences
2007-2013

Guangzhou Institute of Geochemistry
2007-2013

South China Botanical Garden
2007-2012

Shanghai Institutes for Biological Sciences
2011

Peking University
2010

National Institute of Measurement and Testing Technology
2007

Wuhan University
2006

The uptake rates of carbonyl sulfide (COS) by soils in subtropical forests with different successional stages were measured using static chambers Dinghushan Biosphere Reserve (DBR) south China from July 2004 to March 2005. three typical tropical studied included monsoon evergreen broad‐leaf forest (BF), pine and mixed (MF) (PF), representing succession the region. COS exchange also compared between plots litter‐fall remaining (plots L) those removed S) each forest. Results showed that these...

10.1029/2006jd008048 article EN Journal of Geophysical Research Atmospheres 2007-04-16

Vegetation restoration can affect the process of soil organic carbon (SOC) decomposition, but how this effect is related to moisture and temperature remains uncertain. Thus, we performed an incubation 120 days using soils degraded land, plantation forest, secondary natural at two levels under levels. We found that amount cumulative SOC decomposition in forest was ca. 11.7 times higher than from land. Higher treatment increased soils. However, did not increase only 60%WHC treatment. The...

10.3390/f13040578 article EN Forests 2022-04-06

Volatile organic compounds (VOCs) are the key precursors of tropospheric ozone and contributors to formation secondary aerosols (SOAs). VOCs from six functional zones in a coastal city China were collected via SUMMA canister determined gas chromatography-mass spectrometry (GC-MS). The average annual concentrations total (TVOCs) as follows: background site (36.00 µg m–3) < residential (48.71 port (61.09 ≈ development (62.25 traffic (73.82 industrial (98.33 m–3). TVOCs spring summer higher...

10.4209/aaqr.2018.04.0122 article EN Aerosol and Air Quality Research 2018-01-01

Abstract A new continuous integrated cavity output spectroscopy analyzer and an automated soil chamber system were used to investigate the exchange processes of carbonyl sulfide (OCS) between soils atmosphere under laboratory conditions. The patterns OCS found be highly dependent on moisture ambient CO 2 concentration. With increasing moisture, ranged from emission dry conditions uptake within optimum range, followed again by at high moisture. Elevated was have a significant impact rate...

10.1002/2016jg003678 article EN cc-by-nc-nd Journal of Geophysical Research Biogeosciences 2017-05-11

The exchange of dimethyl sulfide (DMS), carbon disulfide (CS 2 ), and (DMDS) between soil the atmosphere was investigated in three subtropical forests south China, namely, a monsoon evergreen broadleaf forest (BF) climax successional stage, pine mixed (MF) midsuccessional (PF) primary stage. soils acted as sources for DMS with average flux BF (1.27 ± 1.40 pmol m −2 s −1 ) significantly higher than those MF (0.46 0.30 or PF (0.47 0.36 ). Litter‐removed plots showed 55%, 21%, 53% lower...

10.1029/2010jd014130 article EN Journal of Geophysical Research Atmospheres 2010-09-17
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