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首页> 外文期刊>Frontiers in Ecology and Evolution >Soil Organic Carbon Pools as Early Indicators for Soil Organic Matter Stock Changes under Different Tillage Practices in Inland Pacific Northwest
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Soil Organic Carbon Pools as Early Indicators for Soil Organic Matter Stock Changes under Different Tillage Practices in Inland Pacific Northwest

机译:土壤有机碳池作为土壤有机物质早期指标在西北地区不同耕作实践下的土壤有机质库存变化

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摘要

Soil organic matter (SOM) is essential for sustaining soil health and crop productivity. However, changes in SOM stocks in response to agronomic practices are slow and show years later when it is too late for adjustments in management. Identifying early indicators of SOM dynamics will allow early management decisions and quick remedial action. The objectives of this study were to evaluate long-term effects of tillage intensity and timing on SOM pools and determine the most responsive SOM pools to tillage practice. Soil from a long-term (53 yrs) winter wheat (Triticum aestivum L.) - spring pea (Pisum sativum L.) rotation and undisturbed grass pasture (GP) in inland Pacific Northwest (iPNW) was sampled to evaluate the effect of four tillage systems [no-till (NT), disk/chisel (DT/CT), spring plow (SP), and fall plow (FP)] on soil organic carbon (SOC, proxy for SOM), total nitrogen (TN), particulate organic matter carbon (POM-C) and nitrogen (POM-N), permanganate oxidizable carbon (POXC), water extractable organic carbon (WEOC), total dissolved nitrogen (TDN), KCl-extractable nitrogen (KEN), microbial biomass carbon (MBC) and nitrogen (MBN), basal respiration (BR), carbon mineralization (Cmin), and metabolic quotient (qCO2). GP had higher levels of SOC pools than cultivated treatments. On average, tillage significantly decreased SOC and TN by 28% and 26%, respectively, compared to GP. Among the cultivated soils, tillage had no significant effect on SOC and TN, except for DT/CT that had slightly higher SOC than FP (P=0.08). On the contrary, NT and DT/CT significantly (P<0.05) increased levels of POM-C, POM-N, POXC, WEOC, MBC, BR, Cmin, and qCO2 over FP or SP. However, tillage did not affect TDN, MBN, and KEN. The C-pools (POM-C, POXC, MBC, WEOC, BR, and Cmin) were more strongly correlated with SOM than the N-pools (TDN, MBN, and KEN), with an exception to POM-N. Under wheat-pea rotation in the iPNW, reduced tillage systems (NT and DT/CT) have a potential to maintain or increase SOM, which can be assessed early through its physical (POM), chemical (POXC, WEOC), and microbiological (MBC, BR, Cmin) indicators. POXC and WEOC were the most sensitive indicators of tillage-induced changes in SOM dynamics.
机译:土壤有机物(SOM)对于维持土壤健康和作物生产率至关重要。然而,在农艺实践的回应时,SOM股票的变化缓慢而展示了在管理层调整时为时已晚。识别SOM动态的早期指标将允许早期管理决策和快速补救行动。本研究的目标是评估耕种强度和时序对SOM池的长期影响,并确定耕作实践中最敏感的SOM池。从长期(53岁)的土壤(53岁)冬小麦(Triticum aestivum L.) - 春天的豌豆(Pisum sativum L.)旋转和未受干扰的草地(GP)在南部的西北地区(IPNW)被取样,以评估四个效果耕种系统[No-Till(NT),磁盘/凿子(DT / CT),春耕(SP)和秋季犁(FP)]在土壤有机碳(SOM,SOM的SOC,Proxy),总氮(TN)上,颗粒状有机物质碳(POM-C)和氮气(POM-N),高锰酸盐可氧化碳(POXC),可溶解的有机碳(WEOC),总溶解氮(TDN),KCl-萃取物氮(KEN),微生物生物质碳(MBC)和氮气(MBN),基底呼吸(BR),碳矿化(CMIN)和代谢商(QCO2)。 GP具有比培养治疗更高的SoC游泳池。平均而言,与GP相比,耕作显着降低28%和26%,分别为28%和26%。在栽培的土壤中,耕作对SoC和Tn没有显着影响,除了SoC的SoC略高于Fp(P = 0.08)。相反,NT和DT / CT显着(P <0.05)POM-C,POM-N,POXC,WEOC,MBC,BR,CMIN和FP或SP的QCO2水平增加。然而,耕作不影响TDN,MBN和Ken。 C池(POM-C,POXC,MBC,WEOC,BR和CMIN)与SO池(TDN,MBN和KEN)更强烈地相关,POM-N异常。在IPNW中的小麦豌豆旋转下,减小的耕作系统(NT和DT / CT)具有维持或增加的潜力,可以通过其物理(POM),化学(POXC,WEOC)和微生物学( MBC,BR,CMIN)指标。 POXC和WEOC是耕种诱导的SOM动态变化最敏感的指标。

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