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Based on recent findings, we develop a new model for the role of glomalin; we postulate a primary role in fungal physiology and secondarily arising effects in the soil environment that lead to observed correlations of GRSP with soil aggregate stability.
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Our results showed that compared with undisturbed soils, soils under the disturbed use dramatically depleted in SOC, particulate OC (POC), non-particulate OC (NPOC), GRSP, easily extractable GRSP (EE-GRSP) and difficulty extractable GRSP (DE-GRSP).
Concurrent with advances in molecular biology, several recent studies have highlighted problems with quantifying GRSP from soil.
Apart from this, the higher contribution of GRSP-C in NPOC (13 to 17%), tended to increase with decreasing soil disturbance, suggesting the role of GRSP in accumulation and stabilization of SOC in this zone.
Further, a linear correlation was found among the fractions of GRSP and SOC, and in turn resulted in the similar relationship with soils bulk density, porosity, pH, available phosphorus, total phosphorus, organic nitrogen's, cations (calcium and potassium), arbuscular mycorrhizal (AM) abundance, and with microbial activity.
To mark the Third Road Safety Week in Viet Nam, the NTSC with support from WHO and UNICEF, and the Global Road Safety Partnership (GRSP) will implement a series of public education campaigns targeted at saving young children's lives and those of vulnerable road users.
We use the gRSP files and set the gARFs to "none" in this thread.
The Chandra gRSP files used here were obtained from the LETG Observer Information page.
If gARF files are used, please ensure that the gRMF files are read in and not the gRSP files, which already include the gARFs.
These results indicate that the factors involve in SOC accumulation simultaneously encourage AM proliferation and in turn GRSP enrichment.
Glomalin-related soil proteins (GRSP) are glycoproteins abundantly produced by arbuscular mycorrhizal fungi in roots and soil.
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