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首页> 外文期刊>Pedosphere: A Quarterly Journal of Soil Science >Water-extractable carbon pools and microbial biomass carbon in sodic water-irrigated soils amended with gypsum and organic manures.
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Water-extractable carbon pools and microbial biomass carbon in sodic water-irrigated soils amended with gypsum and organic manures.

机译:在用石膏和有机肥料改良的苏打水灌溉土壤中的水可提取碳库和微生物生物量碳。

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Microbial biomass carbon (MBC), a small fraction of soil organic matter, has a rapid turnover rate and is a reservoir of labile nutrients. The water-extractable carbon pools provide a fairly good estimate of labile C present in soil and can be easily quantified. Changes in soil MBC and water-extractable organic carbon pools were studied in a 14-year long-term experiment in plots of rice-wheat rotation irrigated with canal water (CW), sodic water (SW, 10-12.5 mmolc L-1 residual sodium carbonate), and SW amended with gypsum with or without application of organic amendments including farmyard manure (FYM), green manure (GM), and wheat straw (WS). Irrigation with SW increased soil exchangeable sodium percentage by more than 13 times compared to irrigation with CW. Sodic water irrigation significantly decreased hot water-extractable organic carbon (HWOC) from 330 to 286 mg kg-1 soil and cold water-extractable organic carbon (CWOC) from 53 to 22 mg kg-1 soil in the top 0-7.5 cm soil layer. In the lower soil layer (7.5-15 cm), reduction in HWOC was not significant. Application of gypsum alone resulted in a decrease in HWOC in the SW plots, whereas an increase was recorded in the SW plots with application of both gypsum and organic amendments in both the soil layers. Nevertheless, application of gypsum and organic amendments increased the mean CWOC as compared with application of gypsum alone. CWOC was significantly correlated with MBC but did not truly reflect the changes in MBC in the treatments with gypsum and organic amendments applied. For the treatments without organic amendments, HWOC was negatively correlated with MBC (r=-0.57*) in the 0-7.5 cm soil layer, whereas for the treatments with organic amendments, both were positively correlated. Irrigation with SW significantly reduced the rice yield by 3 t ha-1 and the yield of rice and wheat by 5 t ha-1 as compared to irrigation with canal water. Application of amendments significantly increased rice and wheat yields. Both the rice yield and the yield of rice and wheat were significantly correlated with MBC (r=0.49**-0.56**, n=60). HWOC did not exhibit any relation with the crop yields under the treatments without organic amendments; however, CWOC showed a positive but weak correlation with the crop yields. Therefore, we found that under sodic water irrigation, HWOC or CWOC in the soils was not related to MBC.
机译:微生物生物量碳(MBC)是土壤有机质的一小部分,具有快速的周转率,并且是不稳定养分的储存库。可水萃取的碳库可以很好地估算土壤中存在的不稳定碳,并且可以轻松量化。在一项为期14年的长期实验中,在用运河水(CW),苏打水(SW,10-12.5 mmol L -1 残留碳酸钠),并用石膏对SW进行修正,无论是否应用有机改良剂,包括农家肥(FYM),绿肥(GM)和麦秸(WS) 。与连续灌溉相比,西南灌溉增加了土壤可交换钠含量的13倍以上。苏打水灌溉使土壤中的可热水提取的有机碳(HWOC)从330降至286 mg kg -1 ,而可冷水提取的有机碳(CWOC)从53减少至22 mg kg - 1 土壤位于0-7.5厘米的最上层土壤中。在较低的土壤层(7.5-15厘米)中,HWOC的降低并不显着。单独施用石膏导致西南样地的HWOC降低,而在西南样地中,在两个土壤层中同时施用石膏和有机改良剂时,HWOC有所增加。然而,与单独施用石膏相比,施用石膏和有机改性剂增加了平均CWOC。 CWOC与MBC显着相关,但并未真正反映出在施用石膏和有机修饰剂的情况下MBC的变化。对于没有有机修饰的处理,HWOC与0-7.5 cm土壤层中的MBC呈负相关(r = -0.57 *),而对于具有有机修饰的处理,两者均呈正相关。与运河灌溉相比,SW灌溉显着降低了水稻产量3 t ha -1 ,水稻和小麦产量降低了5 t ha -1 。实施修正案大大提高了稻米和小麦的单产。水稻产量以及水稻和小麦的产量均与MBC显着相关(r = 0.49 **-0.56 **,n = 60)。在不进行有机改良的情况下,HWOC与作物产量没有任何关系。但是,CWOC与作物单产呈正相关但较弱。因此,我们发现在苏打水灌溉下,土壤中的HWOC或CWOC与MBC无关。

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