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Anaerobically mineralized nitrogen within macroaggregates as a soil health indicator
Catena ( IF 5.4 ) Pub Date : 2020-11-15 , DOI: 10.1016/j.catena.2020.105034
Gisela V. García , María E. Campos , Nicolás Wyngaard , Nahuel I. Reussi-Calvo , Silvina San Martino , Fernanda Covacevich , Guillermo A. Studdert

Anaerobically mineralized nitrogen (AN) in bulk soil (ANBS) has been described as a soil health indicator. Considering that large macroaggregates (2000–8000 μm, MA) are more sensitive to management practices than the bulk soil (i.e. whole soil), AN within MA (ANMA) would be a better soil health indicator than ANBS. The aim of this study was to evaluate if ANMA is a better indicator of: i) soil organic carbon (SOC) and particulate organic carbon (POC) in bulk soil (SOCBS and POCBS, respectively) and ii) aggregate stability (AS) than ANBS. Soil samples were taken at 0–5 and 5–20 cm from 46 continuously cultivated plots (CC) and a reference plot for each CC (pseudo-pristine, PRIS). These soils, located in the Argentinean Pampas, were classified as Mollisols with contrasting surface textural classes. The AS, SOCBS, POCBS, ANBS, SOC (SOCMA), and POC (POCMA) within MA and ANMA were determined separately at 0–5 and 5–20 cm soil depths and estimated at the 0–20 cm layer. The ANMA was a good indicator of SOCBS (R2 0.75, 0.48, and 0.61 at 0–5, 5–20 and 0–20 cm depths, respectively), POCBS (R2 0.66, 0.31, and 0.49, respectively), and AS (R2 0.80, 0.68, and 0.76, respectively). The ANMA performed similarly to predict SOCBS, POCBS, and AS as compared to ANBS, because ANMA was closely correlated to ANBS (r 0.90 at 0–20 cm). Since ANMA determination is more time-consuming than ANBS determination, its use as a soil health indicator would not be convenient. Therefore, the use of ANBS would be recommended over ANMA as a variable to monitor soil health.



中文翻译:

大骨料中厌氧矿化的氮作为土壤健康指标

散装土壤中厌氧矿化的氮(AN BS)已被描述为土壤健康指标。考虑到大型宏观聚集体(2000–8000μm,MA)比整块土壤(即整块土壤)对管理措施更敏感,因此,MA内的AN(AN MA)比AN BS是更好的土壤健康指标。这项研究的目的是评估AN MA是否可以更好地指示以下各项:i)散装土壤中的土壤有机碳(SOC)和颗粒有机碳(POC)(分别为SOC BS和POC BS),以及ii)集料稳定性( AS)比AN BS。从46个连续耕作的地块(CC)和每个CC的参考地块(假-原始,PRIS)分别在0-5和5-20 cm处获取土壤样品。这些位于阿根廷南美大草原上的土壤被归类为Mollisols,具有不同的表面质地类别。在MA和AN MA内分别在0-5和5-20 cm土深处确定AS,SOC BS,POC BS,AN BS,SOC(SOC MA)和POC(POC MA),并在0-20估算厘米层。的AN MA是SOC的良好指示器BS(R 2 0.75,0.48,和0.61在0-5,5-20和0-20厘米的深度,分别地),POC BS(R 2分别为0.66、0.31和0.49)和AS(R 2分别为0.80、0.68和0.76)。与AN BS相比,AN MA的性能与预测SOC BS,POC BS和AS相似,这是因为AN MA与AN BS紧密相关(在0-20 cm处r = 0.90)。由于AN MA测定比AN BS测定更耗时,因此将其用作土壤健康指标将不方便。因此,建议使用AN BS而不是AN MA作为变量来监测土壤健康。

更新日期:2020-11-15
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