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Maize straw application as an interlayer improves organic carbon and total nitrogen concentrations in the soil profile: A four-year experiment in a saline soil
CHANG Fang-di, WANG Xi-quan, SONG Jia-shen, ZHANG Hong-yuan, YU Ru, WANG Jing, LIU Jian, WANG Shang, JI Hong-jie, LI Yu-yi
2023, 22 (6): 1870-1882.   DOI: 10.1016/j.jia.2023.02.025
Abstract219)      PDF in ScienceDirect      

Soil salinization is a critical environmental issue restricting agricultural production.  Deep return of straw to the soil as an interlayer (at 40 cm depth) has been a popular practice to alleviate salt stress.  However, the legacy effects of straw added as an interlayer at different rates on soil organic carbon (SOC) and total nitrogen (TN) in saline soils still remain inconclusive.  Therefore, a four-year (2015–2018) field experiment was conducted with four levels (i.e., 0, 6, 12 and 18 Mg ha–1) of straw returned as an interlayer.  Compared with no straw interlayer (CK), straw addition increased SOC concentration by 14–32 and 11–57% in the 20–40 and 40–60 cm soil layers, respectively.  The increases in soil TN concentration (8–22 and 6–34% in the 20–40 and 40–60 cm soil layers, respectively) were lower than that for SOC concentration, which led to increased soil C:N ratio in the 20–60 cm soil depth.  Increases in SOC and TN concentrations in the 20–60 cm soil layer with straw addition led to a decrease in stratification ratios (0–20 cm:20–60 cm), which promoted uniform distributions of SOC and TN in the soil profile.  Increases in SOC and TN concentrations were associated with soil salinity and moisture regulation and improved sunflower yield.  Generally, compared with other treatments, the application of 12 Mg ha–1 straw had higher SOC, TN and C:N ratio, and lower soil stratification ratio in the 2015–2017 period.  The results highlighted that legacy effects of straw application as an interlayer were maintained for at least four years, and demonstrated that deep soil straw application had a great potential for improving subsoil fertility in salt-affected soils.

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TaSnRK2.4 is a vital regulator in control of thousand-kernel weight and response to abiotic stress in wheat
MIAO Li-li, LI Yu-ying, ZHANG Hong-juan, ZHANG Hong-ji, LIU Xiu-lin, WANG Jing-yi, CHANG Xiao-ping, MAO Xin-guo, JING Rui-lian
2021, 20 (1): 46-54.   DOI: 10.1016/S2095-3119(19)62830-3
Abstract173)      PDF in ScienceDirect      
Sucrose non-fermenting 1-related protein kinase 2 (SnRK2) is a plant-specific serine/threonine kinase involved in response to adverse environmental stimuli.  Previous studies showed that TaSnRK2.4 was involved in response to abiotic stresses and conferred enhanced tolerance to multiple stresses in Arabidopsis.  Further experiments were performed to decipher the underlying mechanisms and discover new functions.  The genomic sequences of TaSnRK2.4s locating on chromosome 3A, 3B and 3D were obtained.  Sequencing identified one and 13 variations of TaSnRK2.4-3A and TaSnRK2.4-3B, respectively, but no variation was detected in TaSnRK2.4-3D.  The markers 2.4AM1, 2.4BM1 and 2.4BM2 were developed based on three variations.  Association analysis showed that both TaSnRK2.4-3A and TaSnRK2.4-3B were significantly associated with thousand-kernel weight (TKW), and that SNP3A-T and SNP3B-C were favorable alleles for higher TKW.  Yeast two-hybrid and split luciferase assays showed that TaSnRK2.4 physically interacted with abiotic stress responsive protein TaLTP3, suggesting that TaSnRK2.4 enhanced abiotic stress tolerance by activating TaLTP3.  Our studies suggested that TaSnRK2.4 have potential in improving TKW and response to abiotic stress.
 
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Straw layer burial to alleviate salt stress in silty loam soils: Impacts of straw forms
ZHANG Hong-yuan, LU Chuang, PANG Huan-cheng, LIU Na, ZHANG Xiao-li, LI Yu-yi
2020, 19 (1): 265-276.   DOI: 10.1016/S2095-3119(19)62737-1
Abstract131)      PDF in ScienceDirect      
Salt stress can be alleviated by straw layer burial in the soil, but little is known of the appropriate form of the straw layer for optimal regulation of soil water and salinity because of the uncontrollability of field tests.  Here, the following four straw forms with compaction thickness of 5 cm buried 40–45 deep were studied: no straw layer (CK), segmented straw (SL, 5 cm in length), straw pellet (SK), and straw powder (SF).  The three straw forms (SL, SK and SF) significantly delayed the infiltration of irrigation water down the column profile by 71.20–134.3 h relative to CK and the migration velocity of the wetting front under SF was the slowest.  It took longer for the wetting front to transcend SK than SL but shorter for it to reach the bottom of soil column after water crossed the straw layer.  Compared with CK, the average volumetric water content in the 0–40 cm soil layer increased by 6.45% under SL, 1.77% under SK and 5.39% under SF.  The desalination rates at the 0–40 and 0–100 cm soil layers increased by 5.85 and 3.76% under SL, 6.64 and 1.47% under SK and 5.97 and 4.82% under SF.  However, there was no significant difference among straw forms in the 0–40 cm soil layer.  Furthermore, the salt leaching efficiency (SLE, g mm–1 h–1) above the 40 cm layer under SL was 0.0097, being significantly higher than that under SF (0.0071) by 37.23%.  Salt storage under SL, SK and SF in the 40–45 cm layer accounted for 4.50, 16.92 and 7.43% of total storage in the 1-m column profile.  Cumulative evaporation under SL and SF decreased significantly by 41.20 and 49.00%, with both treatments having the most significant inhibition of salt accumulation (resalinization rate being 36.06 and 47.15% lower than CK) in the 0–40 cm soil layer.  In conclusion, the different forms of straw layers have desalting effects under high irrigation level (446 mm).  In particular, SL and SF performed better than SK in promoting deep salt leaching and inhibiting salt accumulation on the soil surface.  However, SL was simpler to implement and its SLE was higher.  Therefore, the segmented 5 cm straw can be recommended as an optimum physical form for establishing a straw layer for managing saline soils for crop production.
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Buried straw layer and plastic mulching increase microflora diversity in salinized soil
LI Yu-yi, PANG Huan-cheng, HAN Xiu-fang, YAN Shou-wei, ZHAO Yong-gan, WANG Jing, ZHAI Zhen, ZHANG Jian-li
2016, 15 (7): 1602-1611.   DOI: 10.1016/S2095-3119(15)61242-4
Abstract1985)      PDF in ScienceDirect      
    Salt stress has been increasingly constraining crop productivity in arid lands of the world. In our recent study, salt stress was alleviated and crop productivity was improved remarkably by straw layer burial plus plastic film mulching in a saline soil. However, its impact on the microflora diversity is not well documented. Field micro-plot experiments were conducted from 2010 to 2011 using four tillage methods: (i) deep tillage with plastic film mulching (CK), (ii) straw layer burial at 40 cm (S), (iii) straw layer burial plus surface soil mulching with straw material (S+S), and (iv) plastic film mulching plus buried straw layer (P+S). Culturable microbes and predominant bacterial communities were studied; based on 16S rDNA, bacterial community structure and abundance were characterized using denaturing gradient gel electrophoresis (DGGE) and polymerase chain reaction (PCR). Results showed that P+S was the most favorable for culturable bacteria, actinomyces and fungi and induced the most diverse genera of bacteria compared to other tillage methods. Soil temperature had significant positive correlations with the number of bacteria, actinomyces and fungi (P<0.01). However, soil water was poorly correlated with any of the microbes. Salt content had a significant negative correlation with the number of microbers, especially for bacteria and fungi (P<0.01). DGGE analysis showed that the P+S exhibited the highest diversity of bacteria with 20 visible bands followed by S+S, S and CK. Moreover, P+S had the highest similarity (68%) of bacterial communities with CK. The major bacterial genera in all soil samples were Firmicutes, Proteobacteria and Actinobacteria. Given the considerable increase in microbial growth, the combined use of straw layer burial and plastic film mulching could be a practical option for alleviating salt stress effects on soil microbial community and thereby improving crop production in arid saline soils.
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