In the Pearl River Delta with more than 1000 years of intensive land reclamation history, the developmentof acid sulphate soils has been generally limited in terms of their acid potential (pyrite content) and spatiale...In the Pearl River Delta with more than 1000 years of intensive land reclamation history, the developmentof acid sulphate soils has been generally limited in terms of their acid potential (pyrite content) and spatialextent. This is attributed to the rapid delta progradation, partially resulted from increasing sediment yieldcaused by deforestation within the catchment and the empolderment in the estuarine embayment. Theempolderment practice accompanied by the clearance of mangroves stopped the upward growth of the pyriticlayer on the one hand and limited the vertical accretion of non-pyritic freshwater sediments over the pyriticestuarine sedimellts on the other. In such a case, the Pyritic layer in the area is frequently thin and ofshallow occurrence. Under forced leaching-recharge conditions for the paddy rice cultivation, the leaching ofacid sulphate materials prevails over its production and this leads to a net loss in pyrite oxidation products.Land excaVation for fishpond farming accelerates Pyrite oxidation due to the direct exposure of the pyriticsediments to air on the pond bunds. Severe acidification can intensify the environmental degradation ofestuarine ecosystems.展开更多
文摘In the Pearl River Delta with more than 1000 years of intensive land reclamation history, the developmentof acid sulphate soils has been generally limited in terms of their acid potential (pyrite content) and spatialextent. This is attributed to the rapid delta progradation, partially resulted from increasing sediment yieldcaused by deforestation within the catchment and the empolderment in the estuarine embayment. Theempolderment practice accompanied by the clearance of mangroves stopped the upward growth of the pyriticlayer on the one hand and limited the vertical accretion of non-pyritic freshwater sediments over the pyriticestuarine sedimellts on the other. In such a case, the Pyritic layer in the area is frequently thin and ofshallow occurrence. Under forced leaching-recharge conditions for the paddy rice cultivation, the leaching ofacid sulphate materials prevails over its production and this leads to a net loss in pyrite oxidation products.Land excaVation for fishpond farming accelerates Pyrite oxidation due to the direct exposure of the pyriticsediments to air on the pond bunds. Severe acidification can intensify the environmental degradation ofestuarine ecosystems.
