Sato Shinjiro, Solomon Dawit, Hyland Charles, Ketterings Quirine M, Lehmann Johannes
Department of Crop and Soil Sciences, Bradfield Hall, Cornell University, Ithaca, New York 14853, USA.
Environ Sci Technol. 2005 Oct 1;39(19):7485-91. doi: 10.1021/es0503130.
Previous studies suggested an increase in the proportion of calcium phosphates (CaP) of the total phosphorus (P) pool in soils with a long-term poultry manure application history versus those with no or limited application histories. To understand and predict long-term P accumulation and release dynamics in these highly amended soils, it is important to understand what specific P species are being formed. We assessed forms of CaP formed in poultry manure and originally acidic soil in response to different lengths of mostly poultry manure applications using P K-edge X-ray absorption near-edge structure (XANES) spectroscopy. Phosphorus K-edge XANES spectra of poultry manure showed no evidences of crystalline P minerals but dominance of soluble CaP species and free and weakly bound phosphates (aqueous phosphate and phosphate adsorbed on soil minerals). Phosphate in an unamended neighboring forest soil (pH 4.3) was mainly associated with iron (Fe) compounds such as strengite and Fe-oxides. Soils with a short-term manure history contained both Fe-associated phosphates and soluble CaP species such as dibasic calcium phosphate (DCP) and amorphous calcium phosphate (ACP). Long-term manure application resulted in a dominance of CaP forms confirming our earlier results obtained with sequential extractions, and a transformation from soluble to more stable CaP species such as beta-tricalcium calcium phosphate (TCP). Even after long-term manure application (> 25 yr and total P in soil up to 13,307 mg kg(-1)), however, none of the manure-amended soils showed the presence of crystalline CaP. With a reduction or elimination of poultry manure application to naturally acidic soils, the pH of the soil is likely to decrease, thereby increasing the solubility of Ca-bonded inorganic P minerals. Maintaining a high pH is therefore an important strategy to minimize P leaching in these soils.
以往研究表明,与无或有限施用历史的土壤相比,长期施用禽畜粪便的土壤中,磷酸钙(CaP)在总磷(P)库中的比例有所增加。为了解和预测这些高度改良土壤中磷的长期积累和释放动态,了解形成了哪些特定的磷形态非常重要。我们使用磷K边X射线吸收近边结构(XANES)光谱,评估了禽畜粪便和原始酸性土壤中形成的CaP形态,以应对不同时长(主要是禽畜粪便施用时长)的情况。禽畜粪便的磷K边XANES光谱未显示出结晶态磷矿物的迹象,但可溶性CaP形态以及游离和弱结合态磷酸盐(水溶态磷酸盐和吸附在土壤矿物上的磷酸盐)占主导。未改良的邻近森林土壤(pH 4.3)中的磷酸盐主要与铁(Fe)化合物有关,如纤铁矿和铁氧化物。短期施用粪便的土壤中既有与铁相关的磷酸盐,也有可溶性CaP形态,如磷酸二钙(DCP)和无定形磷酸钙(ACP)。长期施用粪便导致CaP形态占主导,这证实了我们早期通过连续提取获得的结果,并且发生了从可溶性CaP形态向更稳定的CaP形态(如β - 磷酸三钙(TCP))的转变。然而,即使经过长期施用粪便(>25年且土壤中总磷高达13307 mg kg⁻¹),没有一个施用粪便改良的土壤显示出结晶态CaP的存在。随着向天然酸性土壤减少或停止施用禽畜粪便,土壤pH可能会降低,从而增加与钙结合的无机磷矿物的溶解度。因此,保持高pH是使这些土壤中磷淋失最小化的重要策略。