根据90个样点表层(0~20cm)土壤磷素的化验数据,在ArcGIS8.1平台上运用地统计学方法研究了横断山北部土壤磷素的空间分布特征及其影响因素.结果表明,该区土壤全磷和速效磷含量均属中上水平,全磷含量达1.20±0.66 g kg-1,速效磷含量...根据90个样点表层(0~20cm)土壤磷素的化验数据,在ArcGIS8.1平台上运用地统计学方法研究了横断山北部土壤磷素的空间分布特征及其影响因素.结果表明,该区土壤全磷和速效磷含量均属中上水平,全磷含量达1.20±0.66 g kg-1,速效磷含量达13.7±12.6mg kg-1.土壤全磷空间分布总体上呈团状或块状,高值区(1.8~2.8g kg-1)主要分布于雅砻江流域西岸甘孜、新龙段和金沙江白玉、巴塘段之间的区域,并向西北和东南方向逐渐减少,低值区(<0.7g kg-1)则主要分布于稻城县南部以及莫拉山以南德格以北的一个狭长区域;速效磷空间分布总体上呈小团块状,高值区(28~55mg kg-1)主要分布于雅砻江中游的甘孜县东部和西部,并向西北和正南方向逐渐减少,低值区(<12mg kg-1)则主要分布于研究区东南部和南部边缘.成土母质本身含磷量和风化程度的不同使得磷素空间分布存在一定的水平、垂直分布特征.土地利用方式、海拔和坡度通过气候差异或土壤侵蚀程度来影响磷素含量.展开更多
The closed-jar incubation method is widely used to estimate the mineralization of soil organic C. There are two C pools (i.e., organic and inorganic C) in calcareous soil. To evaluate the effect of additional carbonat...The closed-jar incubation method is widely used to estimate the mineralization of soil organic C. There are two C pools (i.e., organic and inorganic C) in calcareous soil. To evaluate the effect of additional carbonates on CO2 emission from calcareous soil during closed-jar incubation, three incubation experiments were conducted by adding different types (CaCO3 and MgCO3 ) and amounts of carbonate to the soil. The addition of carbonates significantly increased CO2 emission from the soil; the increase ranged from 12.0% in the CaCO3 amended soil to 460% in the MgCO3 amended soil during a 100-d incubation. Cumulative CO2 production at the end of the incubation was three times greater in the MgCO3 amended soil compared to the CaCO3 amended one. The CO2 emission increased with the amount of CaCO3 added to the soil. In contrast, CO2 emission decreased as the amount of MgCO3 added to the soil increased. Our results confirmed that the closed-jar incubation method could lead to an overestimate of organic C mineralization in calcareous soils. Because of its effect on soil pH and the dissolution of carbonates, HgCl2 should not be used to sterilize calcareous soil if the experiment includes the measurement of soil CO2 production.展开更多
通过2年(2009-2011年)大田试验,研究不同耕作措施和秸秆还田及其交互效应对稻麦两熟制农田0~7、7~14和14~21 cm 3个土层土壤总有机碳和活性有机碳组分(易氧化有机碳、水溶性有机碳和微生物生物量碳)的影响.结果表明:秸秆还田处...通过2年(2009-2011年)大田试验,研究不同耕作措施和秸秆还田及其交互效应对稻麦两熟制农田0~7、7~14和14~21 cm 3个土层土壤总有机碳和活性有机碳组分(易氧化有机碳、水溶性有机碳和微生物生物量碳)的影响.结果表明:秸秆还田处理各土层土壤总有机碳和活性有机碳含量均显著高于无秸秆还田处理;0~7 cm土层,翻耕处理土壤微生物生物量碳含量显著高于旋耕处理,旋耕处理易氧化有机碳含量高于翻耕处理;7~14 cm土层,旋耕处理土壤总有机碳含量显著高于翻耕处理;14~21 cm土层,翻耕处理土壤总有机碳、水溶性有机碳和微生物生物量碳含量均显著高于旋耕处理;翻耕加稻麦两季秸秆均还田处理的总有机碳含量均高于其他各处理.展开更多
基金Supported by the National Natural Science Foundation of China (Nos. 40571087 and 40773057) and the National Key Technologies Research and Development Program of China during the llth Five-Year Plan Period (No. 2007BAD89B02).
文摘The closed-jar incubation method is widely used to estimate the mineralization of soil organic C. There are two C pools (i.e., organic and inorganic C) in calcareous soil. To evaluate the effect of additional carbonates on CO2 emission from calcareous soil during closed-jar incubation, three incubation experiments were conducted by adding different types (CaCO3 and MgCO3 ) and amounts of carbonate to the soil. The addition of carbonates significantly increased CO2 emission from the soil; the increase ranged from 12.0% in the CaCO3 amended soil to 460% in the MgCO3 amended soil during a 100-d incubation. Cumulative CO2 production at the end of the incubation was three times greater in the MgCO3 amended soil compared to the CaCO3 amended one. The CO2 emission increased with the amount of CaCO3 added to the soil. In contrast, CO2 emission decreased as the amount of MgCO3 added to the soil increased. Our results confirmed that the closed-jar incubation method could lead to an overestimate of organic C mineralization in calcareous soils. Because of its effect on soil pH and the dissolution of carbonates, HgCl2 should not be used to sterilize calcareous soil if the experiment includes the measurement of soil CO2 production.